Ecological Research Series
GUIDELINES FOR  ZOOPLANKTON SAMPLING
                IN  QUANTITATIVE  BASELINE
              AND MONITORING PROGRAMS
                            Environmental Research Laboratory
                            Office of Research and Development
                           U.S. Environmental Protection Agency
                                  Corvallis, Oregon 97330

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                RESEARCH REPORTING SERIES

Research reports of the Office of Research and Development, U.S. Environmental
Protection Agency, have been grouped into nine series. These nine broad cate-
gories were established to facilitate further development and application of en-
vironmental technology.  Elimination of traditional grouping was  consciously
planned to foster technology transfer and a maximum interface in related fields.
The nine series are:

      1.  Environmental  Health Effects Research
      2.  Environmental  Protection Technology
      3.  Ecological Research
      4.  Environmental  Monitoring
      5.  Socioeconomic Environmental Studies
      6.  Scientific and Technical Assessment Reports (STAR)
      7.  Interagency Energy-Environment Research and Development
      8.  "Special" Reports
      9.  Miscellaneous Reports

This report has been assigned to the ECOLOGICAL RESEARCH series. This series
describes research on the effects of pollution on humans, plant and animal spe-
cies, and materials. Problems  are assessed for their long- and short-term influ-
ences. Investigations include formation, transport, and pathway studies to deter-
mine the fate of pollutants and their effects. This work provides the technical basis
for setting standards to minimize undesirable changes in living organisms in the
aquatic, terrestrial, and atmospheric environments.
 This document is available to the public through the National Technical Informa-
 tion Service, Springfield, Virginia 22161.

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                                                          EPA-600/3-78-'
                                                          February 1978
                GUIDELINES FOR ZOOPLANKTON SAMPLING IN
            QUANTITATIVE BASELINE AND MONITORING PROGRAMS1/
                                  by
                    Fred Jacobs and George C.  Grant
                 Virginia Institute of Marine  Science
                   Gloucester Point, Virginia   23062
                            Grant Number -
                            EPA-R804147010
                            Project  Officer

                           Richard C.  Swartz
                         Newport  Field Station
                Marine  and Freshwater Ecology  Branch
              Corvallis  Environmental  Research  Laboratory
                        Newport,  Oregon  97365
             CORVALLIS ENVIRONMENTAL RESEARCH LABORATORY
                 OFFICE OF RESEARCH AND DEVELOPMENT
                U. S. ENVIRONMENTAL PROTECTION AGENCY
                      CORVALLIS, OREGON. 27330
Special Scientific Report No. 83, Virginia Institute of Marine Science

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                                 DISCLAIMER
This report has been reviewed by the Corvallis Environmental Research Lab-
oratory, U.S. Environmental Protection Agency, and approved for publication.
Approval does not signify that the contents necessarily reflect the views
and policies of the U.S. Environmental Protection Agency, nor does mention
of trade names or commercial products constitute endorsement or recommen-
dation for use.
                                     ii

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                                  FOREWORD
Effective regulatory and enforcement actions by the Environmental Protection
Agency would be virtually impossible without sound scientific data on pollu-
tants and their impact on environmental stability and human health.  Respon-
sibility for building this data base has been assigned to EPA's Office of
Research and Development and its 15 major field installations, one of which
is the Corvallis Environmental Research Laboratory (CERL).

The primary mission of the Corvallis Laboratory is research on the effects
of environmental pollutants on terrestrial, freshwater, and marine ecosystems;
the behavior, effects and control of pollutants in lake systems; and the
development of predictive models on the movement of pollutants in the
biosphere.

This report presents a review of methods for sampling and analyzing marine
zooplankton communities.  These quantitative techniques can be used to
establish ecological baselines or to conduct surveys of the impact of
pollution on zooplankton dynamics.
                                      A. F. Bartsch
                                      Director, CERL
                                      111

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                                  ABSTRACT
Methods applicable to zooplankton sampling and analysis in quantitative
baseline and monitoring surveys are evaluated and summarized.  Specific
recommendations by managers must take into account characteristics of the
water mass under investigation, the abundance of contained zooplankton and
phytoplankton populations and the objectives of the study.  Realistic
planning and development must also consider available monetary and manpower
resources.

This report was submitted in fulfillment of Contract No. R804147010 by the
Virginia Institute of Marine Science under the sponsorship of the U. S.
Environmental Protection Agency.  This report covers a period from 24 Nov
75 to 31 May 77, and work was completed as of 25 Feb 77.
                                     iv

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                                  CONTENTS
Foreword

Abstract

Contents

Acknowledgments

Sections

1      Conclusions
       Introduction                                                      3
       2.1  Zooplankton                                                  3
       2.2  Spatial variations                                           3
       2.3  Temporal variations                                          4
       2.4  Introduction to bias and variation associated with           4
               sampling
            2.4.1  Introduction to sampling gear bias                    4
            2.4.2  Avoidance of samplers by zooplankton                  5

       Sampling                                                          6
       3.1  Sampling site selection and station selection                6
       3.2  Sampling gear                                                7
            3.2.1  Water bottles                                         7
            3.2.2  Pumping systems                                       7
            3.2.3  Introduction to net sampling                          8
            3.2.4  General considerations of net sampling                8
            3.2.5  Recommended nets for oceanic sampling                 10
            3.2.6  Care of nets                                          10

       Shipboard handling of samples                                     12
       4.1  Labelling and shipboard handling of samples                  12
       4.2  Preservation of samples                                      12
       4.3  Shipboard procedures for obtaining samples                   14
       4.4  Special cases                                    .            14
            4.4.1  Sampling for pollutants                               14
            4.4.2  Sampling gelatinous organisms                         15

       Sample processing                                                 16
       5.1  Subsampling by pipette method                                16

                                     v

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Sections
       Sample processing (cont.)
       5.2  Subsampling by splitting                                     16
       5.3  Biomass                                                      17
            5.3.1  Introduction                                          17
            5.3.2  Shipboard treatment                                    18
            5.3.3  Settling volume                                       18
            5.3.4  Displacement volume                                    18
            5.3.5  Wet  weight                                            19
            5.3.6  Dry  weight                                            20
            5.3.7  Ash-free dry weight                                    20
            5.3.8  Large gelatinous  forms                                 20

       Additional biochemical analyses                                    21
       6.1  Introduction                                                 21
       6.2  Total protein                                                21
            6.2.1  Biuret method                                          21
            6.2.2  Lowry (et al.)  method                                  21
       6.3  Total lipid analysis                                          22
       6.4  Carbohydrate                                                 22
       6.5  Ash                                                           22
       6.6  Chitin                                                       23
       6.7  Other analyses                                               23
            6.7.1  Amino acids                                            23
            6.7.2  Fatty acid analyses                                    23
       6.8  Biochemistry of marine zooplankton                            24

       Data  Analysis                                                      25
       7.1  Total numbers  and frequency of occurrence                     25
       7.2  Diversity indices                                            25
       7.3  Multivariate analysis                                         27

       Sectional  bibliography                                            28
                                    VI

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                               ACKNOWLEDGMENTS
The authors wish to thank Dr. Richard C. Swartz of the Environmental Protec-
tion Agency for his helpful suggestions in developing this report and for
critically reviewing the final draft.  We also thank Mrs. Shirley Sterling
for her very able secretarial assistance.
                                     vii

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                                  SECTION 1

                                 CONCLUSIONS
The zooplankton is a diverse assemblage of animal forms, and as a result,
exhibits wide spatial, diurnal and seasonal variations in abundance and
composition.  Accurate interpretation of quantitative and qualitative
relationships are further complicated by gear bias and the ability of
certain groups to avoid capture.  Methods to minimize error estimates
follow no standard procedure; only careful analysis of the problem under
study facilitates the proper approach.

Baseline studies are required to be broader in scope and more detailed in
their enactment than are monitoring studies.  Frequency of sampling, number
of stations, accumulation of hydrographic information, etc., should be
expansive for baseline studies.  Monitoring should be initiated when phe-
nomena are somewhat understood and/or patterns from previous baseline
studies have been developed.  As a result, stations in monitoring studies
are usually set further apart than in original baseline studies.  However,
characteristics of the water column being sampled are most important in
determining the location of sampling sites.  Sampling locations might be
further apart in homogeneous waters, such as certain offshore areas, than
in heterogeneous coastal waters.  In estuaries, where environmental para-
meters exhibit considerable variations over relatively short distances and
time periods, a closer spacing of sampling sites and an increased frequency
of sampling are recommended.  Sampling sites are often randomly selected
stratified stations chosen from a gridded pattern which has been overlaid
on the study area.  Transects may be utilized in situations where the study
area covers great distances and ship time is limited.  In pollution studies,
a series of transect lines radiating from a source point may be advisable.
Furthermore, stations along these transects should extend into unaffected
areas.  In studies concerned with small scale distribution of zooplankton,
a parachute drogue can be employed to maintain station locations for repeated
sampling from the same water parcel.

Pumping systems, although expensive, are most efficient for capturing micro-
zooplankton, but these systems should pump in excess of 150 1/min. to min-
imize avoidance.

Nets are recommended for sampling mesozooplankton.  There is no ideal
plankton net; appropriate gear selection is dictated by a clear understanding
of the problem being studied.  The mouth opening of the net should be as
large as possible, and still retain its ability to be handled efficiently
aboard ship.  Nets with mouth openings of 50 to 100 cm in diameter (or 0.2 m2
or greater)  are adequate for capturing most groups.  Tow speed should be

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 between 1 1/2 - 2 knots for low speed nets,  and the net should maintain a
 constant velocity while under tow.   Mesh size selection is critical in deter-
 mining quality and quantity of the  catch.   In relatively plankton rich,
 temperate coastal waters, 333 ym is the minimum mesh size that maintains a
 filtration efficiency of 85% or greater.  Although a 202 ym mesh  net has the
 advantage of retaining forms that pass through a 333 ym mesh net,  filtration
 efficiency drops after 5 minutes of tow in these waters.  In areas of low
 plankton biomass, where clogging is not likely to occur, the 202  ym net is
 recommended.  All nets should be properly  cared for, kept out of  direct sun-
 light,  and washed in fresh water at the conclusion of each cruise.

 Samples should be properly labelled and generally are best preserved in 4%
 buffered formaldehyde.   Sampling zooplankton for pollutants requires special
 methodology, largely designed to minimize  potential contamination.   Splitting
 of  samples is recommended for quantitative studies;  two types of  splitters
 are suggested,  the Folsom & the Burrell.  Zooplankton groups should be split
 to  workable numbers (usually 100-200 individuals within a group).

 Paired  nets provide a replicate sample that  can be utilized for biomass
 considerations.   The most popular techniques for presenting biomass are:
 (1)  Settling volume,  (2)  Displacement volumes,  (3)  Wet  weight,  (4)  Dry weight
 and (5)  Ash-free dry weight.   Volume measurements and wet weight  are non-
 destructive measurements.   Information on  the nutritional content  of the
 zooplankton is  provided by dry weight and  ash-free  dry  weight.  Dry weight
 is  best  determined by freeze-drying samples.

 The patchy distribution of zooplankton in  the marine environment  dictates
 care in  the application of appropriate statistical methods  of analysis.
 Observations made from ranking,  abundances of individual groups,  species
 and  biomass,  still form the bulk of the accumulated  data from baseline  and
 monitoring surveys.   Spatial  and seasonal  trends  can be interpreted  in  this
 manner.  Diversity indices can be used for zooplankton  community  comparisons
 and  pollution studies.  These  indices  may  have  added value when used  in
 conjunction  with  other  indices,  associated statistics and  observations.
With the widespread availability of computers,  multivariate  approaches  are
 receiving  greater  attention.   This  type  of analysis  draws  its  conclusions
by recognizing patterns among  variables  and by  condensing multidimensional
relationships.  By using clustering  techniques, samples may  be partitioned,
distinguished and  ranked,  according  to  similarities  of  species composition
and abundance.

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                                  SECTION 2

                                INTRODUCTION
2.1  Zooplankton

The  term zooplankton refers to individuals and communities of animals, whose
distribution and dispersal are influenced significantly by the movements of
the  waters.  Zooplankton are essential intermediary links in marine food
chains since they graze on phytoplankton, and provide a direct food source
for  more complex animal forms.  Furthermore, the zooplankton impart excretion
products and organic detritus to the marine environment, and planktonic
organisms constitute a considerable portion of the biomass of the world's
oceans.  Almost every animal phylum is represented, at least at some life
stage, in the plankton.

This great diversity of animal types makes the zooplankton a difficult com-
munity to work with.  Specialists are required for individual groups and
quantitative sampling is beset with problems.  In addition to errors asso-
ciated with present sampling methodology, a greater source of sampling
difficulty is the "aggregate" or "patchy" nature of the zooplankton itself.


2.2  Spatial variations

In the late 1800's and early 1900's opposing opinions concerning the distri-
bution of oceanic plankton were held.  Despite Haeckel's (1890) efforts to
persuade the scientific community that, "the composition of the plankton is
in qualitative as well as quantitative relations, very irregular," Victor
Hensen, working with Kiel planktologists, firmly advocated relatively even
distribution.  Hensen's theory implied that plankton data obtained from a
few hauls, could be used to estimate conditions over a much greater area of
the  ocean.  Haeckel's hypothesis implied that individual areas of the sea had
to be sampled before anything could be stated about plankton communities
within these areas.  The controversy was ended by results of A. C. Hardy's
(1936) "Discovery" and "William Scoresby" expeditions.  By utilizing a con-
tinuous plankton recorder, which sampled plankton densities and fluctuations
along continuous lines of observation, Hardy concluded that "there is no
doubt as to the patchy nature of the oceanic plankton."

Explanations offered for the existing patchy distribution of oceanic plankton
are numerous, ranging in physical, chemical and biological factors.  Selected
references dealing with this subject are presented in the bibliography on
this section.  These aggregates of zooplankton vary in size and shape, but
several researchers have indicated patch diameter to be hundreds of meters

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 or less.  Densities within patches are generally from 2 to 5 times greater
 than background densities.  Results from computer simulated models and actual
 field studies have indicated that the size and distribution of patches in a
 body of water greatly affect the accuracy and precision of estimates  of
 zooplankton abundance.


 2.3  Temporal variations

 Natural fluctuations associated with seasonal variations in sunlight  inten-
 sity, water temperature and transparency, oxygen and nutrient content of  the
 water etc.  exert direct and indirect effects on zooplankton survival  and
 community development.  As a result, wide ranges in zooplankton biomass and
 specific abundance occur.   At a single station in the Sargasso Sea, variations
 in  biomass  changed by a factor of 10, between certain seasons (Deevey 1971).
 In  Chesapeake Bay, biomass in summer months can be two orders of magnitude
 greater than in relatively sparse periods;  differences in actual numbers  of
 individuals within groups  can vary by as  much as 5 or 6 orders of magnitude
 between seasons (Jacobs and Grant MS.).   Furthermore the change of dominant
 species, over time,  results in distinctive  zooplankton communities during
 certain periods of the year.   The degree  to which naturally occurring seasonal
 phenomena affects  variability in zooplankton numbers and species must be
 considered  when designing  a zooplankton  study.

 Many  zooplanktonic organisms  perform diurnal vertical migrations,  the effects
 of  which are most  pronounced  in the upper 300 m.   An early model indicated
 that  upward migration begins  at noon, and organisms attain their highest  water
 column levels near midnight.   The effects of light and the physiology of  the
 organisms themselves appear to be the most  important controlling factors  in
 diurnal migration.   The likelihood of sampling error is further increased
 during darkness since migrating species  tend to be compressed into more
 discrete layers during night  hours,  than  are nonmigrating species.  An
 important consequence of vertical migration is  that no two samples from
 the same body of water,  unless taken at  the same  time of  day,  are  directly
 comparable.   In "Plankton  and Productivity  of the  Oceans",  Raymont (1963)
 devotes  a chapter  to vertical distribution  of zooplankton and reviews  the
 early  literature on  diurnal migration.

 There  appears  to be,  at  least in nearshore  waters,  a periodic fluctuation in
 zooplankton abundance and  composition that  is directly related  to  tidal con-
 dition.  This  is generally more prominent in species  that  do  not  undergo  diel
 vertical migrations  (Sameoto  1975).


 2.4  Introduction  to  bias  and variation associated  with  sampling

 2.4.1   Introduction  to sampling gear  bias
 In addition  to variations  related  to  the plankton  and  its  environment,  addi-
 tional error and bias  is introduced by the  choice  of  gear,  and  the manner  in
which  it is  used.  Proper  gear  selection is  essential  in  attempting to  max-
 imize  accuracy, but no "blanket"  recommendations for  the  "ideal" gear  types
 can be offered.  Only  careful  analysis of the problem under study will

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facilitate the correct choice(s).  Naturally, factors such as ship time and
capability, funds for study, and available manpower are, practically speaking,
as important as the questions under study, for selecting gear.  With many
samplers, variables such as the speed, depth and duration of tows can affect
resulting catches.  When nets are used, different mouth openings, mesh sizes,
netting material and net structure influence the biomass and constituency of
the captured organisms.  This report will present a variety of sampling sit-
uations and offer appropriate suggestions and recommendations to maximize
sampling efficiency.


2.4.2  Avoidance of samplers by zooplankton
Although discussed in greater detail later in this report, the subject of
avoidance deserves brief mention here.  Error and variation in estimating
zooplankton is increased by the ability of certain groups to avoid capture
while others cannot.  This results in selective sampling and in general
underestimation of zooplankton abundance and biomass.  Mechanisms of avoidance
are numerous:  responses to changes in water movements, size, swimming abil-
ity, etc. of the animals are all factors.  Certain age or physiologically
stronger groups within a species may exhibit a greater ability to avoid
capture than others.  Naturally, avoidance is greatly influenced by the
type(s) of gear utilized, and the manner in which it is used.  For further
information, a UNESCO report that summarizes the exhaustive literature on
avoidance, is recommended (Clutter and Anraku 1968).

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                                   SECTION 3

                                   SAMPLING


 3.1  Sampling site selection and station selection

 The problem under study, time, and available money, are essential consider-
 ations for sampling site selection.   The type of information required dictates
 the scientific approach.  For example,  baseline and monitoring studies,
 although related, have distinct differences in the scope of information  they
 seek, and therefore require different thought processes in their development.
 Subsequently, the location, frequency,  and number of stations sampled should
 be quite comprehensive for initial baseline studies.  Baseline studies should
 also include intensive sampling of a wide variety of related measurements,
 such as dissolved oxygen,  salinity,  temperature and other aspects of  water
 chemistry (i.e.  nutrients).  Selection  of sampling sites can be facilitated
 by dividing the  area into  a gridded  pattern or into transects.   Once  data
 and information  are analyzed, phenomena are better understood and trends
 established, scaled down monitoring  can be initiated.   Numbers of stations
 and samples can  be reduced, if it is feasible to do so without information
 loss.   Essentially, monitoring programs should be designed to provide maximum
 information for  minimum cost and effort.

 The design of the sampling program must consider both  the objectives  of  the
 investigations and the hydrographic  conditions in the  area of study.   Sampling
 locations might  be further apart in  offshore areas of  homogeneous  water  char-
 acteristics,  than in rather heterogeneous neritic areas,  where  close  sampling
 sites might be indicated.   In estuaries,  where environmental variables exhibit
 considerable variations over relatively short distances,  an  even  closer
 spacing of sampling sites  is recommended.

 In  oceanic studies,  the sampling patterns may consist  of  a series  of  transects
 across  different  current systems,  a  series from shore  to  deeper waters, or  a
 grid of nearly equidistant  stations  within an  oceanographic  area.  Although
 gridded mapping  of  a  study  area  is most desirable,  this is not always possible
 in  studies  that monitor large distances and  have  fixed  time  requirements.
When a  grid pattern  is  utilized,  it  is  usually  overlaid on a  study area that
has been  divided  into  subareas.   These  subareas  are  generally determined by
hydrographic  factors.   Within each subarea,  random stratified stations may  be
selected.   It  is  advisable  to draw up a cruise  track having  a clear indication
of  the  projected  ship  time,  both  available and  required,  to  complete  the
station program.   It is recommended  that  additional  alternate stations are
included  in the sampling program.  Furthermore, researchers  should pre-deter-
mine which stations are "least crucial" to the  study, in  the event that time
factors dictate elimination  of certain stations.

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Frequency of sampling is also dependent on the specific objectives to be
answered and available ship time.  Generally, ship requirements differ for
different studies; estuarine areas can, as a result, be more frequently
sampled than offshore waters.  It is desirable and feasible to conduct
surveys in estuarine waters monthly or biweekly, while offshore monitoring
is usually conducted bi-monthly, quarterly or semi-annually.  All available
published literature and hydrographic data accumulated for an area of poten-
tial study should be utilized to maximize efficiency of sampling design.

In cases of pollution related monitoring problems, it is preferable that a
series of samples should extend from affected to unaffected areas, the latter
samples then serving as controls.  If this is not possible, control data can
be provided from surveys in the same area, conducted previous to the time of
the introduction of a pollutant, or from other unpolluted areas of similar
hydrographic and environmental structure.  Sampling sites should be close
enough to show gradient effects when they exist.  Monitoring should continue
until recovery is complete.  In studies that monitor effects from a direct
environmental addition, stations can be established along a series of
transect lines, radiating from a source point.

For sampling a specific water parcel, the use of a parachute drogue, set below
the surface, provides a suitable reference point for navigation and station
location.  Relative positions of station sites are maintained, since modifi-
cations in the sampling locations are determined by movements of the drogue.
In this way the same parcel of water can be repeatedly sampled, regardless of
the influence of the currents.  This is particularly useful in field studies
that are concerned with small scale variations in zooplankton.
3.2  Sampling gear

Three general classes of sampling gear are used to sample zooplankton, namely
water bottles, pumps, and nets.  This section will devote a major emphasis on
net samplers, since they are most efficient for capturing organisms larger
than micro-zooplankton.

3.2.1  Water bottles
The use of water bottles provides samples and associated hydrographic data
from fixed locations within the water column.  For most purposes 10 liter
bottles are recommended.  These samplers can capture and return live organ-
isms; however, animals capable of only moderate locomotion can avoid capture.
Water bottles, widely used in phytoplankton sampling, are of value only in
sampling microzooplankton (animal plankters that pass through a 202 pm mesh
net) .

3.2.2  Pumping systems
This is probably the most favorable method for capturing microzooplankton.
These systems generally control filtering aboard ship, with water being run
through a single (or a nest of different sized) filter(s).  Samples are then
preserved and generally analyzed by direct counts with an inverted microscope.
Pumping systems can be towed from moving vessels and can provide integrated
samples over a range of depth.  The depth range capability is a function of

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 the amount of  hose attached to the pump.   To minimize  avoidance  these  systems
 should pump in excess  of 150 1/min.   If  the capture  of larger  forms  (i.e.
 copepods)  is desired,  pumping rate should  be in  excess of  200  1/min.   In
 certain cases,  pumping may cause partial or total  destruction  of soft  bodied
 forms.   Another disadvantage of pumping  systems  is that they tend  to be
 expensive  and  require  specific shipboard modifications.

 3.2.3   Introduction to net sampling
 Although this  is the best method for  capturing larger  forms, sampling  micro-
 zooplankton with nets  is not recommended.   To retain microzooplankton, net
 meshes  must be  small and as a result,  samplers tend  to clog rapidly.   A 103
 urn  mesh has been demonstrated to fall  below 85%  filtering  efficiency during
 the first  minute of tow (Smith et al.  1968).

 The grouping of zooplankton by size classes generally  follows  this scheme:
 (1)  microzooplankton  - defined as zooplankton that  pass through a mesh
     size  of 202 ym;

 (2)  small  mesozooplankton - defined as  zooplankton  retained by  a mesh size
     of 202 ym;

 (3)  large  mesozooplankton - defined as  zooplankton  retained by  1 mm mesh
     size;

 (4)  macrozooplankton  -  defined as large agile plankters and less agile
     nekton (captured  by such gear as  an Isaacs-Kidd Midwater  Trawl).

Although there  is no "ideal" zooplankton net available, attempts should be
made to limit choices  for  given situations.  This would improve  standard-
ization and  result  in  greater comparability of different studies.  Re-
searchers,   however  must  have a  clear definition of the problem under study;
this generally  facilitates  the  appropriate  choice of gear.   For  example,
Vannucci (1968) pointed  out  the differences in approach when sampling for
fish larvae  and mixed plankton.   "The  fisheries manager tries to select
certain size classes and or  species against the others, while the plank-
tologist tries  to obtain as  representative a sample  as possible  of the
mixed association living in  the  sea."  A 505 pm mesh net may be  adequate
for sampling fish larvae, but would be of limited scientific value for
sampling immature copepods and other smaller forms.

3.2.4  General considerations of net sampling
(1)   Mouth  opening - nets with  different sized  mouth openings have been shown
     to have selective  capabilities for the capture of zooplankton spe-
     cies.   The importance of mouth opening for the efficiency of capture has
     been examined in actual  field and computer simulated models.  It appears
     that 20 and 40 cm nets  introduce error by  underestimating abundance and
     diversity   (McGowan and Fraundorf 1966; Wiebe and Holland 1968).   Larger
     mouth  openings (100 cm or greater) yield more precise  data and capture
     larger forms.  However the larger the  net,  the more difficult it is to
     handle and retrieve.  Although larger  nets  are more desirable, nets with
     mouth  openings of  60 cm diameter (or 0.2 m^)  are considered adequate for
     ocean  sampling. When sampling for macrozooplankton,  little difference

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     was noted between 6 and 10 foot Isaacs-Kidd midwater trawls for most
     groups, excluding the fishes  (Friedl 1971).  The 10 ft trawl captured
     significantly more numbers and individual species of fish, than did the
     6 foot trawl.

 (2)  Tow speed - This can be an important factor, considering the avoidance
     capabilities of certain species.  Tested species of copepods were able
     to avoid nets towed at 30 cm/sec (0.6 knots).  It is therefore recom-
     mended that low speed nets be towed between 1 1/2 and 2 knots (75-100
     cm/sec).  Even at constant engine speeds (between 1 and 2 knots),
     variation in net speed through the water sometimes exists, and may
     introduce significant error in the interpretation of data.

     High speed samplers (>3 knots) have been developed for use from moving
     vessels.  Although records indicate that these samplers sometimes damage
     organisms, other reports found these samplers to capture and return
     intact organisms.  Reduction of mouth opening size avoids conditions
     of clogging in these nets.  At speeds of 1 1/2-2 knots most plankton
     are captured; high speed should be required only for sampling specific
     groups (primarily fishes) capable of considerable movement.

 (3)  Mesh size - In temperate, relatively plankton rich coastal waters, it
     has been demonstrated that 333 ym is the minimum net mesh size that
     maintains over 85% filtration efficiency for the duration of 15 minute
     tows   (Smith et al. 1968).  Smaller sizes tend to have reduced filtra-
     tion efficiency due to clogging.  Filtration efficiency is calculated by
     comparing results of two flow-meters, one mounted inside the net mouth
     opening, the other outside,


                            observed                      (from inside
Filtration Efficiency (%)   volume of water through net	flowmeter)	
                          = theoretical maximum volume of water (from outside
                                   through net                    flowmeter)
                            X 100

     Since the 202 pm mesh net delineates microzooplankton from small meso-
     zooplankton,  it would appear logical that this net receive wide usage,
     and it has.   A UNESCO (1968) report recommended using a 200 \im mesh net
     for sampling small mesozooplankton.  Unfortunately, this net tends to
     clog in plankton rich waters, filtration efficiency dropping below 85%
     in 5 minutes.   It does, however, have the advantage of retaining forms
     that pass through 333 um mesh net.   whether this would add significant
     information to a problem under study, must be considered by individual
     investigators.  In areas where clogging is not likely to occur, this
     mesh size (202 um)  is recommended.            '  -

(4)  All nets should be made of nylon material.

(5)  When nets are under tow, wire angle should be 30° or less.  Nets should
     not be raised faster than 45 meters/min during oblique or vertical tows.

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 (6)  Other factors such as filtration to mouth area ratios,  bridles,  color of
      nets, extrusion through meshes, etc. can all affect the net's efficiency.

 3.2.5  Recommended nets for oceanic sampling
 Of the dozens of samplers available (see Jossi, 1970)  only three types  are
 discussed below:
 (1)  Multiple opening-closing nets - These systems are now becoming popular
      at certain major oceanographic laboratories.  This system provides infor-
      mation on intermediate (100's to 1000's of meters) scale spatial patterns
      of zooplankton distribution and can be equipped with sensors that  monitor
      related environmental parameters.   The sampler contains several  nets,
      each of which is opened and closed sequentially by commands through
      conducting cable from the surface  (Wiebe et al. 1976).   This system
      provides the best technology developed to date for studying the  vertical
      distribution and profiles of marine zooplankton species.   This system
      is,  alas,  quite expensive and large; its use is limited to well  equipped,
      large ocean research vessels.

 (2)   Paired opening-closing Bongo system - This sampler consists of two
      mechanically operated opening-closing nets mounted side by side  (McGowan
      and  Brown,  1966).   These nets are  recommended over single net  samplers,
      in that  they provide two samples from the same environment.  One can be
      used for taxonomic purposes,  while biochemical analyses can be conducted
      on the other.   The mouth opening of each net should be  at least  50 cm  in
      diameter (60 cm is more desirable)  and have a mesh area to mouth opening
      area ratio  of  at least 5 to 1.  Used concomitantly with a pinger and/or
      a  Time-Depth Recorder, this system yields an integrated sample over a
      desired  depth  range.   Digital flowmeters should always  be used to  monitor
      water flow.  This  system is much less expensive than multiple  opening-
      closing  nets and is  easier to handle.   Although multiple  opening-closing
      nets  are preferable  for studying detailed vertical structure,  paired
      opening  closing  systems  are adequate when single  integrated  samples over
      a  depth  range  are  required.

 (3)   Longhurst-Hardy  Plankton Recorder  -  This  sampler  has been developed for
      studying small scale  patterns (10's  to  100's  of meters) of  spatial  zoo-
      plankton distribution.   This  net utilizes  the  Hardy  principle, of
      capturing plankton on gauze in  the  cod  end.   The  gauze  is  advanced  at
      periodic intervals, and  can be  changed  by  spooling.  This  sampler  ex-
     hibits a certain amount  of  bias, probably  in  part  due to  its relatively
      low mesh aperture  area to mouth opening area  ratio  (stalling and other
     residence time biasing of organisms  sometimes being significant).  Re-
     cently, Haury et al.  (1976) have conducted several experiments on  the
     sources and degree of bias  associated with Longhurst-Hardy Plankton
     Recorders.  Recommendations are made  for proper design and use of  this
     sampler.

3.2.6  Care of nets
(1)  After sample is removed from net, by  carefully hosing organisms into cod
     end,  net is rinsed without a  cod end.

(2)  If clogging is severe, nets should  be washed in detergent.


                                     10

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(3)   Net should never be left in direct sunlight for extended time periods.

(4)   Both net and flowmeter should be washed in fresh water,  after each
     cruise (flowmeters washed more often during cruise,  if possible).
                                      11

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                                  SECTION 4

                         SHIPBOARD HANDLING OF SAMPLES


 Most of the recommendations  from this section are taken directly from
 Griffiths et al.  (1976).   Samplers should always be handled carefully in
 a manner to minimize injury  to  zooplankters and scientists.


 4.1  Labelling and shipboard handling of samples

 Glass jars with screw on plastic lids are generally used for storing zoo-
 plankton.   Jars should be  labelled on the outside with pre-printed gummed
 labels,  this can  be done in  the  laboratory prior to ship time.   Labels should
 never be placed on jar caps.  A  sample label used by the Virginia Institute
 of Marine Science (VIMS) Planktology Department is presented below:


                       VIMS PLANKTOLOGY DEPT.

         SHIP	CRUISE NO	COLL.  NO	

         DATE	GEAR	MESH SIZE	

         STA. NO. or LOCATION —.	
In addition to outside labels, an internal label written  on water-resistant
paper should be placed in every jar.   Black India ink  is  preferred over pencil
marks because it provides a permanent, waterproof,  easy-to-read record.  In-
ternal labels should also be pre-printed.

Collecting information should be contained in« a  field  log as the samples are
being collected.  A sample page from a VIMS field log  is  presented on the
following page.   Generally, comments  on sea state,  hydrography and water
chemistry are kept on a separate form(s).


4.2  Preservation of samples

Formaldehyde is  commonly used as a fixative for  preserving zooplankton sam-
ples, a saturated solution containing 38-40% formaldehyde is known as,
"concentrated formalin".   One part formalin should  be  added to nine parts
sea water,  to provide a 4% formaldehyde solution.   Buffering of concentrated
formaldehyde should be conducted by adding 2 gms. of borax to 98 ml of


                                     12

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                            BLM Bongo Collections
Station No.                            Collection No.
Location  (start) 	 Depth

Location  (end) 	

Date                        Vessel
Time (EST) opened 	 Meter final rdg.

Time at depth 	   " initial rdg.

    Max fishing depth 	 No. revs. 	

Time closed                           Meter No.
Net size and mesh 	 Vessel speed

Type of tow (stepped or continuous oblique) 	
Depressor used 	Wire angle 	 Wire out
                                    (at max, fishing depth)	
Remarks:
                                     13

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 concentrated formalin, before dilution.  Periodically, the neutrality of the
 sample should be checked with pH paper.  Calcareous animals should be pre-
 served in formalin with a pH of 8.2, since calcium carbonate dissolves below
 that level.  The use of instruments that can dispense formalin is recommended.
 Furthermore, formaldehyde can be very harmful;  it should be washed off skin
 immediately.  Splashes in eyes should be followed by washing in cold water for
 10-15 minutes, and medical attention.
 4.3  Shipboard procedures for obtaining samples

 (1)  Secure flowmeter(s) propeller (use of TSK or GO type  meters are recom-
      mended) .   Read and record number of revolutions obtained  during tow.

 (2)  Wash net  from the outside, starting at the mouth and  working downward
      toward the cod end.  Use a sea water hose whenever possible.

 (3)  Remove the bucket or bag from the cod end; concentrate  sample through a
      concentrating device of mesh size equal to or smaller than the mesh of
      the net.   This must be done quickly to minimize damage.

 (4)  Plankton  should be washed into the labelled sample jar, filled 3/4 full
      with sea  water.   The volume of the plankton should not  exceed 10% of the
      jar.   If  catches are larger, plankton should be placed  in a larger jar
      or  divided into 2 jars.   If divided,  the jars should  indicate either,
      "1  of 2 samples" or "2 of 2 samples"  etc.

 (5)  Add formaldehyde, preferably from a dispenser.   Final concentration
      should be 4%.   Gently rotate jar.

 (6)   Place  inside  label in jar,  seal  cap tightly and invert  the  jar several
      times  periodically during the first hour of fixation.

 (7)   Before proceeding to next station,  check to see that  data have not been
      omitted from  field logs.

 (8)   Store  the jars  in a cool,  dark,  place.

 (9)   Upon return to  the  laboratory, the  state of the  sample preservation and
      sample  pH should  be periodically checked.

 (10)  Shipboard  procedures  for  obtaining  biomass  samples are discussed in
      section 5.3.
4.4  Special cases

4.4.1  Sampling for pollutants
Problems arise when sampling zooplankton for pollutants, such as trace metals,
pesticides or petroleum hydrocarbons.  Since these levels are extremely low
in the natural environment, and ocean-going vessels are a generous source of
these materials, the potential for obtaining contaminated specimens is great.


                                     14

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Certain precautions can, however, be taken to minimize contamination:
(1)  Specimens should never have any contact with the surface of the ship.
(2)  Contact between collecting gear and ship surfaces should be minimal.
(3)  Neither sample nor gear should be washed with the ship's salt water.

(4)  Hands, tools, sorting trays and storage containers should be liberally
     washed with 95% ethanol.

(5)  Handling and sorting gear must be of metal, glass or enamel.
(6)  Use metal cups for pesticide collections.

(7)  Use of opening-closing nets can be used to avoid contamination from the
     ship (i.e. paint chips).  Sampler is opened and closed below the surface.

4.4.2  Sampling gelatinous organisms
Sampling gelatinous zooplankton with nets may prove to be inadequate for
certain groups.  Many of these organisms are delicate and are lost or damaged
beyond recognition when strained through meshes.  Furthermore, many of these
groups do not preserve well in formaldehyde and require specialized methodol-
ogy for fixation and preservation.  Current information on biology and distri-
bution of these forms is being contributed from in situ observations made by
SCUBA divers.
Ctenophores

These organisms may appear in excessive numbers in plankton tows, especially
in temperate estuaries during certain times of the year.  Since they tend to
break apart and (when dominating samples) somewhat gum up formaldehyde pre-
served samples, ctenophores should be removed.  Their type, number and volume
should be recorded and they can be preserved separately.  A reference for
fixing and preserving ctenophores is listed in the bibliography (Adams et al.,
1976).
                                     15

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                                   SECTION 5

                               SAMPLE  PROCESSING
 Once  they are  returned  to  the  laboratory,  processing  of preserved  samples  can
 be  initiated.   Before proceeding  further,  large  organisms  (i.e. medusae, fish
 larvae,  etc.),  especially  when uncommon  to the sample, should be removed.
 These forms  are then counted and  identified.
 5.1   Subsampling by  pipette method

 A  summary  of  this method  is taken largely  from an  earlier U.  S. Environmental
 Protection Agency manual  (Weber, 1973)  and proceeds  as  follows:

 (1)   The sample is drained of  excess  formaldehyde; settled volume is read in
      a  graduated cylinder or Imhoff cone in  a  volume of water such that plank-
      ton makes up 1/5 of  the diluted  volume.

 (2)   Sample is stirred with a  Stempel pipette; 1 ml  of  the agitated mixture
      is withdrawn from the sample.

 (3)   The subsample is transferred to  a  gridded culture dish with 5 mm squares.

 (4)   Pipette  is rinsed with distilled water  into culture dish, to remove any
      adherent organisms.  Enumerate and identify subsample under a dissecting
     microscope.

After calculating the dilution factor,  the information derived from counting
together with estimates of water volume sampled, can be used to derive the
total abundance of individual groups  or of the total sample.  However, con-
sidering the relatively small aliquot studied, this method should be used
only when  rapid "ballpark" numbers are needed.  This method, and others
employing  similar methodology, are not recommended for precise, quantitative
analysis of samples.
5.2  Subsampling by splitting

This is the best method for quantitative analysis of zooplankton.  Two types
of splitters are recommended:  the classic Folsom splitter (McEwen et al.
1954) and the newer Burrell et_ al. (1974) device.  The Folsom splitter has
received some criticism, due to variations associated with individual han-
dling,  but certain simple modifications can alleviate this situation.
                                     16

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Samples should be sorted according to the following guidelines:
(1)  Remove excess  formaldehyde; place sample in culture dish with 5 mm
     square grid; place dish under dissecting microscope.

(2)  Remove any animals that are rare.  Look at numbers within groups that
     appear in the whole sample.  If less than 200 are in any group, remove
     all individuals within that group.  Keyed laboratory counters prove
     useful for recording individual counts.  Animals should be placed in
     labelled vials of 4% formaldehyde.

(3)  Place sample in splitter.  Split sample, wash and rinse splitter into
     sub-splits.  Remove and record all individuals of any groups that
     contain a "workable number" of organisms (100-200 individuals).

(4)  Continue splitting and sorting in this manner until an entire sample
     has been counted.

(5)  Splitter should be rinsed with fresh water.

Proper use of a splitter is best illustrated by example:
A 1/2 split contains decapod larvae plus numerous cladocerans and copepods.
Decapods are counted and removed until none are left, a total of 150 being
counted.  Sample is then split and it appears that cladoceran numbers are
workable.  175 individuals are counted, removed and recorded.  Sample is
split again to count copepods, and 156 individuals are counted.
                     Numbers in total sample:
                       Decapod larvae = 150 x 2 =  300
                       Cladocerans    = 175 x 4 =  700
                       Copepods       = 156 x 8 = 1248
In situations where certain groups require greater attention or study the
"workable number" may be increased.  Conversely, in situations where certain
groups will receive little study, or when monotypic groups are observed, the
"workable number" may be decreased.

Abundance estimates derived from splitting, and information derived from
flowmeters, facilitate the calculation of abundance/water volume.  Further-
more, fiducial limits can be placed on numbers within groups that have "been
counted.  After samples have been sorted into vials, specialists can deter-
mine the species compositions of individual groups.

Other methods for separating organisms by size groups, and density patterns
have shown promise for sorting certain individual groups.
5.3  Biomass

5.3.1  Introduction
Within the natural environment, every trophic level contains, at any given
time, a fixed amount of living material, composed of several kinds of
organisms.  This living material is referred to as the standing crop, the
biomass being a useful expression of it.  The most popular techniques for
presenting zooplankton biomass are:  (1) Settling volume, (2) Displacement

                                     17

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 volume, (3) Wet weight, (4)  Dry weight,  and (5)  Ash-free dry weight.   Dis-
 placement and settling volume, and wet weight are non-destructive measure-
 ments.   These methods leave  samples intact for further taxonomic and  other
 uses.   They are also less time demanding and require less equipment and  skill
 than other methods.   They do not, however, provide any insight  on the nutri-
 tional  content of the plankton.  If this information is desired, dry  weight
 and ash-free dry weight measurements should be conducted.  Ash-free dry  weight
 is considered the most desirable technique for reporting the chemical (organic
 carbon) composition.   Conversion factors between biomass techniques are  not
 always  applicable, due to variations in  interstitial water content between
 different sized samples (Wiebe et al.  1975).   Smaller samples appear  to  retain
 a larger percentage  of interstitial water than do larger samples.

 5.3.2   Shipboard Treatment
 In cases where biomass information is  being sought,  the use of  paired zoo-
 plankton samplers is  recommended.   In  this way,  a sampler required to undergo
 biomass analysis is derived  from a separate net  than is a taxonomic sample.
 If only a single net  is available, subsampling should be conducted rapidly,
 and with a minimum of damage resulting to the plankton.   In cases  where
 organic estimates are required, the sample should be washed and rinsed thor-
 oughly  in distilled water.   Triple glass distilled water is recommended
 whenever possible.  Samples  should be  placed  in  a freezer at -20°C, for
 storage.   If no shipboard freezer is available,  maintenance of  samples in
 a  well  insulated container,  filled with  dry ice, is adequate.

 Microzooplankton samples  obtained from water  bottles or pumping generally do
 not  provide  a great deal  of  material,  therefore  wet  weight  or volume  measure-
 ments are  not recommended.   Another problem associated with microzooplankton
 is  that  organisms  are generally concentrated  together with  phytoplankton and
 detrital material.  Direct counts  and  size measurements  using a microscope
 may  be  a better means for  obtaining biomass estimates for microzooplankton.

 5.3.3   Settling volume
 Settling volume is obtained  by  allowing  plankton  to  settle  in a graduated
 cylinder or  an  Imhoff cone.   This  method is not  recommended,  since it  exhibits
wide variations  in tests  that attempt  to reproduce results,  and  does  not
 compare well  with other biomass measures.   It  is  still  used  by  planktologists
because of its  simplicity and because  it  leaves material  undamaged.   This
method should be used only in situations  where rough  approximations of
biomass are desired.

5.3.4  Displacement volume
This method measures  an equivalent  volume  of  liquid  that  is  displaced by the
sample.   Displacement volume may be  read  by several methods  of varying com-
plexity.  A simple direct measurement proceeds as  follows:
 (1)  Sample is placed in sieve of mesh size equal  to  or smaller  than net used
     in  capture.

(2)  Sample is allowed to drain, and transferred  to a measured volume  of
     water in a graduated cylinder.

(3)  The new volume containing sample + known volume is read.

                                     18

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     The displacement volume = new volume minus original measured volume
     of water.

Another equally valid method reads the volume of water and the interstitial
fluid after it has been subtracted from the original (known) volume of sample
and fluid.

The more sophisticated Mercury Immersion method provides a better means for
removal of interstitial water but requires considerably more time and skill
than do direct measurements.  Nevertheless, this method has received consid-
erable use by plankton researchers, and several modifications of the original
method have been developed (see Beers, 1976).  Steps are outlined:
(1)  Sample is placed in a chamber with a sintered glass base.

(2)  Liquid and interstitial fluid is removed by applying air pressure.

(3)  The chamber containing the sample is placed in a dish of mercury,
     effectively sealing the underside of the glass base.

(4)  The chamber is filled to a certain known level by adding water from a
     burette.  The volume of water utilized is read.

(5)  After the sample has been removed, the chamber is filled with only water.
     This volume is read.

     Displacement volume = step (5) - step (4), which represents the
     difference in the volume of water required to fill the chamber,
     with and without plankton.  It is usually expressed in ml/m  of
     water volume sampled.

5.3.5  Wet weight
Wet weight is used to determine the actual weight of the "raw" plankton, once
interstitial water has been removed.  However, care must be taken to avoid
loss of body fluids from the organisms.  A disadvantage of wet-weight is the
existing degree of variation associated with individual technique.  Further-
more in mixed zooplankton samples, individual taxa retain different amounts
of water relative to their organic and inorganic constituency.  In deter-
mining wet weight, the following steps should be followed:
(1)  Pre-weigh glass jar.

(2)  Strain plankton through plankton gauze of a smaller mesh size than used
     for capture.  Rinse thoroughly with fresh water.

(3)  Allow water to drain.

(4)  Blot sample on absorbent paper towels until water is no  longer absorbed
     onto the towels.

(5)  Transfer sample to glass jar and weigh.
                                      19

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     The wet weight is the difference between the weight of the sample + the
     jar, less the weight of the jar (step 5-1).  Wet weight is usually
     expressed in milligrams (or grams)/m3 of water volume sampled.

5.3.6  Dry weight
Dry weight is a measure of the total plankton weight, after the water content
has been removed.  To obtain maximum accuracy, drying should be conducted
without the loss of any volatile organic material.  Freeze-drying (lyophili-
zation) is the best method for extracting water and providing an accurate dry
weight value, with minimal biochemical alteration of the sample.

If freeze-drying is not possible, oven-drying at 60°C is recommended.  This
temperature provides rapid drying and is still low enough to insure a minimum
of organic loss.  The time required for drying may vary, according to the
size of the sample; drying is considered complete when a sample attains a
constant weight (two successive readings are not significantly different).
Dry weight is usually expressed in milligrams (or gms)/m^ of water volume
sampled.

5.3.7  Ash-free dry weight
Ash content (weight), in samples that were freeze-or oven-dried to constant
weight is determined by ashing the sample in a muffle furnace at 500°C.
Weights are taken after sample has been allowed to cool.  Ash-free dry weight
is the measure of organic material in the sample, exclusive of all water and
inert organic material.  It is calculated as follows:
     Ash-free dry weight = dry weight - ash weight.  Ash-free weight is
     usually expressed in milligrams (or gms)/m3 of water volume sampled.

5.3.8  Large gelatinous forms
Remove from sample and measure separately.
                                     20

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                                   SECTION  6

                       ADDITIONAL  BIOCHEMICAL ANALYSES
 6.1   Introduction

 In recent years  there has been a marked increase in the accumulation of data
 on the biochemical  constituency of marine zooplankton.  Procedures for
 obtaining total  protein, lipid, carbohydrate, ash and chitin values were
 summarized by Raymont et al.  (1964), and are outlined below.

 Values for the individual components are usually expressed as a percentage of
 dry weight, obtained from freeze or oven dried samples.  Other more detailed
 types of analyses are mentioned and references to guide potential investi-
 gators are offered.


 6.2  Total protein

 The largest single  fraction of most oceanic plankton is usually the protein.
 The most widely  accepted method for determining protein from zooplankton is
 the colorimetric biuret method.

 6.2.1  Biuret method - Procedure:
 (1)  Homogenize  a known dry weight (0-5 mgm) with 1 ml distilled water and
     4 ml biuret reagent in a Potter-Elvehjem homogenizer until all purple
     particles are  dissolved.

 (2)  Filter homogenate through glass paper.  Repeat this step until a clear
     filtrate is obtained.

 (3)  Transfer to a  cuvette and read in a spectrophotometer at 540 mu.  The
     instrument should be zeroed by a blank consisting of 1 ml distilled
     water and 4 ml biuret reagent.

The optical density (OD) of the sample should be read against a standard curve
for bovine albumen.  The standard curve should be made up by dissolving a
series of known weights (from 0-10 mg) of the albumen in 1 ml distilled water
and 4 ml biuret reagent.

6.2.2  Lowry (et^jal.) method
This is another colorimetric indicator of total protein, and although more
sensitive than the biuret method, it is generally considered a micro-method.
Its use is recommended in situations where only very small amounts of material
are available.

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 6.3  Total lipid analysis

 The lipid is generally the most variable fraction of the marine zooplankton.
 Constituent classes of this fraction are important as energy reserves and are
 essential for reproductive and structural components.  A common procedure used
 for calculating total lipid employs extractive and gravimetric methodology.

 (1)  Lipid is extracted from about 10 mg of dry weight with a 2:1 chloroform-
      methanol (V/V) mixture in a Potter-Elvehjem homogenizer.

 (2)  After filtering, the filtrate is washed with a 0.05 N potassium chloride
      solution.   Volume of wash solution added should be approx. 20% of the
      homogenate volume .

 (3)  Allow phases to separate by standing (or centrifugation) .

 (4)  Siphon off upper phase.

 (5)  Transfer lower phase to pre-weighed container and evaporate solvent in
      a stream of nitrogen.

 (6)  Only lipid should remain.   Record weight and express as a  percentage of
      the initial dry weight.

 Modifications of this method  using benzene  instead of chloroform,  and heating
 samples in a boiling water  bath,  have been  reported to yield accurate results
 for lipids of individual  species.   Furthermore,  colorimetric procedures  also
 appear  adequate.


 6.4 Carbohydrate

 Carbohydrate has been shown to  appear in relatively small amounts  in  most
 marine  zooplankton.   Values are. almost  always  less than  4%  of the  dry weight.
 Colorimetric methodology  for determination  of  carbohydrates  is  recommended.
 Procedure :

 (1)  Place a constant  dry weight  (1-5 mg) in a boiling tube,  with  1 ml
     distilled water,  1 ml  5% phenol  solution  and  5 ml cone.
(2)  After allowing to cool for 20 minutes, read optical density  (OD) in a
     spectrophotometer at 490 m y.

(3)  Compare CD's with standard curve for glucose.
6.5  Ash

Obtained from ash-free dry weight analysis (Sec. 5.3.7).  Value is material
that remains in muffle furnace after sample has been ashed at 500°C.
                                     22

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6.6  Chitin

Crustacean exoskeletons are  chitinous, making this material an important
fraction  to  quantify.  Procedure is as follows:

(1)  A known wet weight (250 mg) is boiled for two hours in 50% NaOH.

(2)  Sample  is left in solution overnight.

(3)  Exoskeletons are removed and washed in dilute HC1.

(4)  Exoskeletons are washed in water.

(5)  Dry  and weigh.  This material is ash plus chitin.

(6)  Ash  in  a muffle furnace to burn off any organic material.  Only ash
     should  remain.

The chitin value is the difference between the weight of the exoskeleton plus
the ash,  and only the ash (step 5 - step 6), and can be expressed as a per-
centage of dry weight.  It must be emphasized that the above described pro-
cedure is effective only with "wet" or "raw" samples.  It does not apply to
dried material, since a viscous, gummy solution is produced when the alkaline
solution  is  added.  Bamstedt (1974) suggested a modified methodology for
estimating total chitin that can be used on dried material.  The procedure
calls for treatments with IN HC1 in a bath of boiling water, and with 4N
NaOH for  20 minutes, also in a water bath.  The material is then washed in
a succession of fluids.  Attempts to reproduce Bamstedt's procedure on dried
material  in  this laboratory  (VIMS), proved unsuccessful.


6.7  Other analyses

Amino acid and fatty acid analyses are mentioned briefly but detailed pro-
cedures are not presented.  References on respective sections should be
consulted.

6.7.1  Amino acids
Methodology has been developed for quantification of free amino acids and
protein hydrolyzates of certain zooplanktonic crustaceans.  Free amino acids
are extracted from lipid-free material with hot distilled water.  Proteins
are precipitated with hot trichloroacetic acid and hydrolyzates are prepared
by refluxing with 6N HC1.   A column chromatograph and technicon autoanalyzer
yield chromatograms for amino acids and protein hydrolyzates.

6.7.2  Fatty acid analysis
Lipid is extracted from the plankton with chloroform-methanol (see Sec. 5.3).
Thin layer and column chromatography can be used to separate lipid into
principle classes, such as phospholipids, triglycerides, hydrocarbons, wax
esters, etc.   Gravimetric analysis has, in certain cases, provided relative
percentages of the various lipid fractions and studies have assessed the
overall significance of these fractions to the organism(s) under examination.


                                     23

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Preparation, hydrogenations and gas liquid chromatography of the methyl
esters of constituent fatty acids has provided insight into the fatty acid
composition of several species of marine and brackish water plankton.
6.8  Biochemistry of marine zooplankton

A bibliography on this rapidly expanding area of investigation is provided,
                                     24

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                                   SECTION  7

                                DATA ANALYSIS
 After  samples have been  sorted  and  other  appropriate analyses completed, a
 cohesive  interpretation  of  data must be developed.  Since planktonic organisms
 are  distributed  in patches,  classical  statistical techniques are of limited
 value.  Most zooplankton studies  to date, have drawn conclusions from obser-
 vations of  raw data, by  ranking abundances of individual species.  With
 expanding computer usage in  recent  years, techniques such as diversity
 indices and multivariate analyses,  have been developed as tools that deter-
 mine quantitative relationships among  and between zooplankton communities,
 and  between community  and environmental parameters.
 7.1  Total numbers and  frequency of occurrence

 Historically  this has been  the most popular method of presenting zooplankton
 data.  Abundances of individual species  (or groups) are listed and ranked.
 Data on  frequency of and periods of occurrence are also calculated.  Abundance
 data are usually expressed  in units of individuals per volume of water (m3,
 100 m^,  etc.) sampled.  Mean total numbers of individual species (or groups)/
 up and percentages of individual species' contribution to the entire sample
 can also be determined.  Confidence limits may be placed on mean numbers of
 individuals but, unfortunately, due to avoidance and the patchy nature of the
 plankton, these limits  generally cover an extremely wide range.  Seasonal
 trends are usually developed by plotting abundances (no. of ind./m3) VS.
 months (or other sampling time period).  In addition to baseline and monitor-
 ing surveys,  studies concerned with day-night differences, spatial variations
 and ecological zonation of  zooplankton communities have employed this type
 of data  interpretation.  It is still the most popular, and in many cases,
 the most meaningful interpretation of data.
7.2  Diversity indices

Diversity indices can be used to establish species diversity gradients in
geographical areas.  These indices allow for comparisons between community
diversity in different areas, with respect to parameters selected (i.e.
effects of seasonality, coastal vs. offshore populations of copepods).
Diversity indices can also be used as a baseline statistic, in areas where
natural or man made changes are anticipated, and can be useful in determining
effects of pollutants on changing zooplankton community structure.

These indices are applicable only after the number of species, and the total

                                      25

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 number of individuals within a species, have been tabulated.  Diversity
 indices can then offer a statement on the "information content" of each
 individual in a sample.  The Shannon-Wiener H', has been a most widely
 used diversity statistic and is calculated as follows:
                               H1 =  -  Zp

              where p. =  number of individuals in the ith species
                          total number of individuals

 The index weighs both numbers of species and evenness of species distri-
 butions.  In systems of low diversity, each successive individual drawn
 from a sample would, since it is likely to be the same species  as a previously
 drawn individual, contribute rather little to the information of the system;
 adequate knowledge could be obtained after relatively few drawings.  This
 would result in a low H' value, since individual information input is low.
 In diverse systems, each successive individual is likely to be  different
 from one previously drawn,  and makes a significant contribution to the
 knowledge of the system.  Many drawings would be required to understand
 the system,  and the diversity statistic H'  would be high.

 Criticisms and modifications in the application of diversity indices have been
 widespread in the literature.   One method claims that the value of H1  can be
 improved by  scaling all measurements down to a common sampling  size.   Other
 investigators question the  value and validity of these indices  for ecological
 research.

 Very often,  pollution in present day ecosystems results  in an overall reduc-
 tion of  certain species and the elimination of others;  a few species are,
 however,  capable of exploiting these conditions.   Diversity indices may
 prove useful in pollution-related studies.   However,  diversity  measurements
 as  indicated by H'  reflect  changes  in overall information content rather
 than enumerate  upon an individual species composition changes.   In a sit-
 uation where one species is completely replaced by another,  the diversity
 value would  remain  constant, yet the change of the species (or  several spe-
 cies)  may  be indicative of  significant environment modifications.   In cases
 like this, use  of an  index  of  faunal overlap  may prove helpful.   Of the
 numerous overlap indices available,  a commonly used measurement is the
 percentage similarity statistic,  which ranges  from 0  when two samples
 contain no species  in common,  to 100  when two  samples are identical in
 both species  and abundances.

                       PS =   100  (1 -  0.5  E|pia -  pib|)

where p.  =  total number of  individuals in  the  ith  species  in sample
            a f  total number of  individuals in  sample a.
      p.,  = the  same  for sample b.

Thus, diversity  indices  used in conjunction with  either  other indices  and
statistics, or associated observations can, in  certain cases, provide  an

                                      26

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effective tool in analyzing aspects of zooplankton community structure.


7.3  Multivariate analysis

This type of analysis draws its conclusions by recognizing patterns between
variables.  As data sets increase in size, the individual's ability to detect
trends or patterns naturally declines.  The increase in availability and
usage of computers has made these analyses feasible and desirable.  These
techniques condense multidimensional relationships by projecting data onto
a reduced number of planes.  Thus the multivariate approach tests the reality
of a variable, by expressing its variability in terms of an additional coord-
inate and seeing whether the variable displays a systematic and logical
pattern.

Cluster analysis is a multivariate approach that orders sets of taxa on the
basis of pre-determined criteria.  For example, data from zooplankton surveys
may cluster and distinguish groups of samples based upon similarities in
composition.  The inverse analysis clusters the species according to simi-
larities in their distribution and abundances.  Other multivariate approaches,
referred to as ordination, make no assumptions in grouping the entities or
in drawing boundaries between classes.  Recently, principal component anal-
ysis has been used to describe and quantify the major elements responsible
for fluctuations in zooplankton abundances (Colebrook 1977).
                                     27

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                                   SECTION 8

                            SECTIONAL BIBLIOGRAPHY
 2.2  Spatial variations

 Anraku, M.  1956.   Some experiments on the variability of  horizontal plankton
 hauls and the horizontal distribution of plankton in a limited area.   Bull.
 Fac.  Fish. Haddaido Univ.  7(1):1-16.

 Anraku, M.  1975.   Microdistribution  of marine copepods in a small inlet.
 Mar.  Biol. 30:79-87.

 Barnes, H.  1949a.   On the volume measurement  of  water filtered by a plankton
 pump, with some  observations on the distribution  of  planktonic animals.  J.
 nar.  biol. Ass.  U.K. 28:651-661.

 Barnes, H.  1949b.   A statistical study of the variation in vertical plankton
 hauls,  with special reference to  the  loss of the  catch with divided hauls.
 J.  mar. biol.  Ass.  U.K.  28(2):429-446.

 Barnes, H. and S. M. Marshall.   1951.   On the  variability  of replicate
 plankton samples and some  applications  of contagious  series to the statistical
 distribution of  catches  over restricted periods.   J.  mar.  biol.  Ass.  U.K.
 30:233-263.

 Boyd,  C.  M.   1973.   Small  scale spatial patterns  of marine zooplankton
 examined by an electronic  in situ zooplankton  detecting device.  Neth. J.
 Sea Res.  7:103-111.

 Cassie,  R.  M.  1960.   Factors influencing the  distribution of  plankton in the
 mixing  zone between oceanic  and harbour waters.   N.Z.  J. Sci.  3:26-50.

 Cassie,  R.  M.  1963.   Microdistribution of plankton.   Oceanog. Mar. Biol.
Ann.  Rev.  1:223-252.

 Gushing,  D.  H.  1962.  Patchiness.  Rappt. Proces-Verbaux Reunions,  Conseil
perm. int.  Explor.  Mer.  15:152-163.

Fasham,  J.  J.  R., M. V. Angel & H.  S. J.  Roe.  1974.   An investigation of the
spatial  pattern of  zooplankton  using the  Longhurst-Hardy plankton  recorder.
J. exp. mar. Biol.  Ecol. 16:93-112.

Haeckel, E.  1890.   Plankton studies [transl. by  G. W.  Field].  Rep. U.S.
Comm. Fish.  1889-1891, p. 565-641.

                                     28

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 Harder,  W.   1968.   Reactions  of plankton organisms  to water  stratification.
 Limnol.  Oceanogr.  13:156-168.

 Hardy,  A.  C.   1936.   Observations  on  the uneven  distribution of  the  oceanic
 plankton.   Discovery Rep.  11:511-538.

 Hardy,  A.  C.   1956.   The  open sea,  Pt.  1.   Houghton Mifflin.   335 p.

 Haury,  L.  R.   1976.   Small-scale patterns  of  a California Current zooplankton
 assemblage.   Mar.  Biol. 37:137-157.

 Longhurst,  A.  R.   1967.   Diversity  and  trophic structure of  zooplankton  com-
 munities in the  California Current.   Deep-Sea Res.  14:393-407.

 Smith,  L.  R.,  C. B.  Miller &  R.  L.  Holton.  1976.   Small-scale horizontal
 distribution  of  coastal copepods.   J. exp.  mar.  Biol. Ecol.  23:241-253.

 Wiebe,  P.  H.   1970.   Small-scale spatial distribution in oceanic zooplankton.
 Limnol.  Oceanogr.  15:205-217.

 Wiebe,  P.  H.   1971.   A computer model of zooplankton patchiness and  its
 effects  on sampling  error.  Limnol. Oceanogr. 16:29-38.

 Wiebe,  P.  H.  and W.  R. Holland.  1968.   Plankton patchiness:  effects on
 repeated net  tows.   Limnol. Oceanogr. 13:315-320.


 2.3  Temporal  variations

 Backus,  R. H., J.  E.  Craddock,  R. L. Haedrich and D. L. Shores.  1970.  The
 distribution  of mesopelagic fishes  in the  equatorial and western North
 Atlantic Ocean.  J.  Mar. Res.  28(2):179-201.

 Badcock, J.   1970.   The vertical distribution of mesopelagic  fishes  collected
 on the Sond cruise.   J. mar. biol. Ass.  U.K.  50:1001-1044.

 Barham,  E. G.  1970.  Deep-sea  fishes:  lethargy  and vertical  orientation.
 In Biological  sound  scattering  in the ocean,  pp. 100-118.  Ed. G. B. Farquhar.
 Maury Center for Ocean Science  Rep. 005.   U.S. Government Printing Office.

 Brinton, E.  1962.   Variable factors affecting the apparent range and esti-
 mated concentration  of euphausiids in the North Pacific.  Pacif. Sci. 16(4):
 374-408.

 Clarke,  T.  A., and P. J. Wagner.  1976.  Vertical distribution and other
 aspects  of the ecology of  certain mesopelagic fishes -taken near Hawaii.
 Fish. Bull. 74(3):635-645.

Deevey,  G.  B.  1971.  The annual cycle  in quantity and composition of the
zooplankton of the Sargasso Sea  off Bermuda.  I.  The upper 500 M.   Limnol.
Oceanogr. 18:219-240.
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 Fager, E. W. and J. A. McGowan.  1963.  Zooplankton species groups in the
 North Pacific.  Science 40:453-460.

 Hardy, A. C.  1935.  The plankton community, the whole fisheries and the
 hypothesis of animal exclusion.  Discovery Rep. 11:273-370.

 Haury, L. R.  1976.  Small-scale patterns of a California Current zooplankton
 assemblage.  Mar. Biol. 37:137-157.

 Jacobs, F. & G.  C.  Grant.   MS.  Seasonal composition and biomass of zooplank-
 ton in the lower Chesapeake Bay.  In prep.

 Maynard,  S. D.,  F.  V. Riggs and J.  F. Walters.   1975.  Mesopelagic micronekton
 in Hawaiian waters:  faunal composition, standing stock, and diel migration.
 Fish.  Bull. 73:726-736.

 Miller, C. B.   1970.   Some environmental consequences of vertical migration
 in marine zooplankton.   Limnol. Oceanogr.  15:727-741.

 Pearcy, W. G.   1964.   Some distributional  features of mesopelagic fishes off
 Oregon.  J. Mar.  Res. 22:83-102.

 Platt,  T.  and  R.  J. Conover.   1971.   Variability and its effect  on 24 h
 chlorophyll budget  of a small marine basin.   Mar.  Biol.  10:52-65.

 Raymont,  J. E. G.   1963.   Plankton  and productivity in the  oceans.   Pergamon
 Press.  660 p.

 Russell,  F.  S.   1927.  The vertical distribution of plankton in  the sea.
 Biol. Rev.  2:213-256.

 Russell,  F.  S.   1928.  The vertical  distribution of marine  macroplankton.
 VII.  Observations  on the  behaviour  of Calanus  finmarchicus.  J.  mar. biol.
 Ass. U.K.  15:429-454.

 Russell,  F.  S.   1931.   The vertical  distribution of marine  macroplankton.   X.
 Notes on  the behaviour  of  Sagitta in the Plymouth  area.   J.  mar.  biol. Ass.
 U.K. 17:391-414.

 Russell, F.  S.  1934.   The  vertical  distribution of marine  macroplankton.
 XII.  Some  observations on  the  vertical distribution of  Calanus  finmarchicus
 in relation  to light  intensity.  J.  mar. biol. Ass.  U.K.  19:569-584.

 Sameoto, D. D.  1975.  Tidal  and diurnal effects on zooplankton  sample vari-
ability in a nearshore marine environment.  J. Fish.  Res. Bd. Can.  32:347-366.

Youngbluth, M. J.   1975.  The vertical distribution and  diel migration of
euphausiids in the  central waters of  the eastern South Pacific.  Deep-Sea
Res. 22:519-536.
                                     30

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 2.4   Introduction  to  bias  and  variation associated with sampling

 Biological Methods Panel Committee on Oceanography.  1969.  Recommended pro-
 cedures  for measuring the  productivity of plankton standing stock and related
 oceanic  properties.   National  Acad. of Sciences, Washington, D. C.  59 pp.

 Clutter,  R. I.  and M.  Anraku.   1968.  Avoidance of samplers.  pp. 57-76.  In;
 D. J.  Tranter  [Ed.] Zooplankton sampling.  UNESCO.  Monographs on oceano-
 graphic  methodology.   No.  2.   174 p.

 Laval, P. H.   1974.   Un modele mathematique de 1'evitement d'un filet a
 plancton, son  application  pratique, et sa verification indirected en
 recourant an parasitisme de 1'amphipode hyperide Vebilia armata Bouvallius.
 J. exp.  mar. Biol.  Ecol. 14:57-87.

 Singarajah, K.  V.   1969.   Escape reactions of zooplankton:  the avoidance of
 a pursuing siphon  tube.  J. exp. mar. Biol. Ecol. 3:171-178.
3.1  Sampling location and station selection

Biological Methods Panel Committee on Oceanography (E. Ahlstrom, Chairman).
1969.  Recommended procedures for measuring the productivity of plankton
standing stock and related oceanic properties.  National Acad. of Sciences,
Washington, D. C.  59 pp.

Dicks, B.  1976.  Offshore biological monitoring.  Pp. 325-359.  In J. M.
Baker  (Ed.). Marine ecology and oil pollution.  Proceedings of a meeting in
Aviemore, Scotland, Apr. 1975, Halstead  (Wiley) N. Y.  566 pp.

Volkman, G., J. Krauss and A. Vine.  1956.  The use of parachute drogue in
the measurement of subsurface ocean currents.  Trans. Am. Geophys. Union
37:573-577.
3.2.1  Water bottles

Biological Methods Panel Committee on Oceanography (E. Ahlstrom, Chairman).
1969.  Recommended procedures for measuring the productivity of plankton
standing stock and related oceanic properties.  National Acad. of Sciences,
Washington, D. C.  59 pp.

UNESCO.  1968.  Microzooplankton.  Report of working party No. 1.  pp. 150-
152.  In: D. J. Tranter (Ed.) Zooplankton sampling.  Monographs on oceano-
graphic methodology, No. 2.  174 p.
3.2.2  Pumping systems

Beers, J. R. and G. L. Stewart.  1967.  Micro-zooplankton in the euphotic
zone at five locations across the California Current.  J. Fish. Res. Bd.
Can. 24:2053-2068.

                                     31

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 Beers, J. R. and G. L. Stewart.  1969.  The vertical distribution of micro-
 zooplankton and some ecological observations.  J. Cons.  perm. int. Explor.
 Mer. 33:30-44.

 Beers, J. R.,  G. L. Stewart and J. D. H. Strickland.  1967.   A pumping system
 for sampling small plankton.  J. Fish. Res. Bd.  Can. 24:1811-1818.

 Cassie,  R.  M.   1958.  Apparatus for investigating spatial distribution of
 plankton.  N.Z. J. Sci.,  1:436-448.

 Leong, R.  1969.  Evaluation of a pump and reeled hose system for studying
 the vertical distribution of small plankton.   Spec.  Scient.  Rep.  U.S.  Fish.
 Wild.  Serv.  Fish,  No.  545,  9 p.

 O'Connell,  C.  P. and R. J.  H.  Leong.   1963.  A towed pump and shipboard
 filtering system for sampling small zooplankters.  Spec.  Scient.  Rep.  U.S.
 Fish.  Wild.  Serv., Fish., No.  452, 19 pp.


 3.2.3   Introduction to net  sampling

 Biological Methods Panel  Committee on Oceanography.   1969.   Recommended
 procedures  for measuring  the productivity  of  plankton standing stock and
 related  oceanic properties.   National Acad. of Sciences,  Washington, D.C.
 59  pp.

 Smith, P. E.,  R. C.  Counts  and R.  I.  Clutter.   1968.   Changes in  filtering
 efficiency of  plankton nets  under  tow due  to  clogging.  J. Cons.  perm.  int.
 Explor. Mer. 32:1-13.

 Vannucci, M.   1968.  Loss of organisms through the meshes,   pp. 77-86.  In
 D.  J.  Tranter  (Ed.). UNESCO  Monographs on  Oceanographic Methodology.   No. 2.
 174  p.
3.2.4  General considerations of net sampling

Aron, W. and S. Collard.  1969.  A study on the influence of net speed on
catch.  Limnol. Oceanogr. 14:242-249.

Barkley, R. A.  1964.  The theoretical effectiveness of towed-net samplers as
related to sampler size and to swimming speed of organisms.  J. Cons. perm.
int. Explor. Mer. 29:146-157.

Clutter, R. I. and M. Anraku.  1968.  Avoidance of samplers,  pp. 57-76.
In: D. J. Tranter (Ed.) Zooplankton sampling.  UNESCO Monographs on
oceanographic methodology.  No. 2.  174 p.

Fleminger,  A. and R.  I. Clutter.  1965.  Avoidance of towed nets by zooplank-
ton.  Limnol. Oceanogr. 11:456-469.
                                      32

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Friedl, W. A.   1971.  The relative sampling performance of 6- and 10-foot
Isaacs-Kidd midwater  trawls.   Fish. Bull. 69:427-432.

Gehringer, J. W.  and  W. Aron.  1968.  Field techniques, pp. 87-104.  In
D. J. Tranter  [Ed.] UNESCO Monographs on oceanographic methodology.  No. 2.
174 p.

Laval, P. H.  1974.   Un modele mathematique de 1'evitement d'in filet a
plancton, son application pratique, et sa verification indirecte en
recourrant an parasitime de 1'amphipode hyperide Vibilia armata Bouvallius.
J. exp. mar. Biol. Ecol. 14:57-87.

Le Fevre, J.  1973.   Clogging  and filtration coefficient in a light-speed
plankton sampler.  Mar. Biol.  21:29-33.

McGowan, J. A.  and V. J. Fraundorf.  1966.  The relationship between size of
net used and estimates of zooplankton diversity.  Limnol. Oceanogr. 11:456-
469.

Noble, R. L.  1970.   Evaluation of the Miller high-speed sampler for sampling
yellow perch and  walleye fry.  J. Fish. Res. Bd. Can. 27:1033-1044.

Sameoto, D. D.  1975.  Tidal and diurnal effects on zooplankton sample vari-
ability in a nearshore marine  environment.  J. Fish. Res. Bd. Can. 32:347-366.

Smith, P. E., R.  C. Counts and R. I. Clutter.  1968.  Changes in filtering
efficiency of plankton nets due to clogging under tow.  J. Cons. perm. int.
Explor. Mer. 32:232-248.

Tranter, D. J.  and P. E. Smith.  1968.  Filtration performance,  pp. 27-56.
In D. J. Tranter  (Ed.) UNESCO Monographs on Oceanic Methodology.  No. 2.
174 p.

Vannucci, M.  1968.   Loss of organisms through the meshes,  pp. 77-86.  In
D. J. Tranter (Ed.) UNESCO Monographs on Oceanographic Methodology.  No. 2.
174 p.

Wiebe, P. H.  1972.  A field investigation of the relationship between length
of tow, size of net and sampling error.  J. Cons. perm. int.  Explor. Mer.
34(2):268-275.

Wiebe, P. H. and  W. R. Holland.  1968.  Plankton patchiness:   effects on
repeated net tows.  Limnol. Oceanogr. 13:315-321.
3.2.5  Recommended nets for ocean sampling

Baker, A de C., M. R. Clarke and M. J. Harris.  1973.  The N.I.O. combination
net (RMT 1+8) and further developments of rectangular midwater trawls.  J.
mar. biol. Ass. U.K. 53:167-184.
                                     33

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 Brown, N. L.  1974.  A precision CTD microprofiler.  Proceedings of the
 International Conference on Engineering in the Ocean Environment.  Halifax,
 Nova Scotia, Vol. 2, 270-278.

 Bruce, R. H. and J. Aiken.  1975.  The undulating oceanographic recorder - a
 new instrument system for sampling plankton and recording physical variable
 in the euphotic zone from a ship underway.  Mar.  Biol. 32:85-97.

 Fasham, M. J. R., M. V. Angel and H. S. J. Roe.  1974.  An investigation of
 the spatial pattern of zooplankton using the Longhurst-Hardy Plankton Re-
 corder.  J. exp. mar. Biol. Ecol. 16:93-112.

 Frost, B. W. and L. E. McCrone.  1974.   Vertical  distribution of zooplankton
 and myctophid fish at Canadian weather station P, with description of a new
 multiple net trawl.  Proceedings of the International Conf.  on Engineering
 in the Ocean Environment.  Halifax, Nova Scotia,  vol. 1, 159-165.

 Haury, L. R.  1973.  Sampling bias of a Longhurst-Hardy Plankton Recorder.
 Limnol. Oceanogr.  18:500-506.

 Haury, L. R.,  P.  H. Wiebe and S. H. Boyd.   1976.   Longhurst-Hardy Plankton
 Recorder:  their design and use to minimize bias.  Deep-Sea  Res. 23:1217-1229.

 Jossi,  J. W.  1970.  Annotated bibliography of zooplankton sampling devices.
 U.S.  Dept.  Interior, U.S. Fish and Wildlife Serv. No. 609.

 Longhurst,  A.  R.,  A. D.  Reith, R.  E.  Bower and L. D.  R.  Siebert.  1966.   A
 new system for the collection  of multiple  serial  plankton  samples.   Deep-Sea
 Res.  13:213-222.

 McGowan,  J.  A.  and D.  M.  Brown.   1966.   A  new opening-closing paired zoo-
 plankton  net.   Univ.  Calif.  Scripps Inst.  Oceanogr.   (Ref. 66-23).

 Tucker, G. H.   1951.   Relation of  fishes and  other  organisms  to  the  scattering
 of  underwater  sound.   J.  Mar.  Res.  10:215-238.

Wiebe,  P. H.,  K. H.  Burt,  S. H.  Boyd  and A. W.  Morton.   1976.  A multiple
 opening/closing net  and  environmental sensing system  for sampling zooplankton.
J. Mar. Res. 34(3):313-326.
3.2.6  Care of nets

UNESCO.  1968.  Smaller mesozooplankton.  Report of working party No. 2.
pp. 153-159.  In; D. J. Tranter (Ed.) Zooplankton sampling.  Monographs on
oceanographic methodology.  No. 2.  174 p.
4.  Shipboard handling of samples
                                     34

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 Griffiths,  F. B., A.  Fleminger, B. Kimor and M. Vannucci.  1976.  Shipboard
 and  curating  techniques,  pp.  17-33.  ^n H. F. Steedman  [Ed.] UNESCO.
 Monographs  on oceanographic methodology.  No. 4.  350 p.

 UNESCO.   1968.   Smaller mesozooplankton.  Report of working party No. 2, pp.
 153-159.  In: D. J. Tranter (Ed.) Monographs on oceanographic methodology.
 No.  2.   174 p.
4.4   Special cases

Adams, H. R., A. P. Flerchinger and H. F.  Steedman.  1976.  Ctenophora
fixation and preservation,  pp. 270-271.   In: H. F. Steedman (Ed.) UNESCO.
Monographs on oceanographic methodology.   No. 4.  350 p.

Grice, G. D., G. R. Harvey, V. T. Bowen and R. H. Backus.  1972.  The col-
lection and preservation of open ocean marine organisms for pollutant
analysis.  Bull. Environmental Contamination and Toxicology 7:125-132.

Hamner, W. M., L. P. Madin, A. L. Alldredge, R. W. Gilmer, and P. P. Hamner.
1975.  Underwater observations of gelatinous zooplankton:  Sampling problems,
feeding biology and behavior.  Limnol. Oceanogr. 20:907-917.

UNESCO.  1976.  Part VIII.  Fixation and preservation of various marine taxa.
In H. F. Steedman (Ed.), Monographs in oceanographic methodology, No. 4.
350 p.
5.1  Subsampling by pipette method

Frolander, H. F.  1968.  Statistical variation in zooplankton numbers from
subsampling with a Stempel pipette.  J. Wat. Pollut. Control Fed. 40, R82-
R88.

Weber, C.  1973.  Biological field and laboratory method for measuring the
quality of surface waters and effluents.  Nat. Environmental Res. Center
Office of Res. Development.  U.S. Environmental Protection Agency.  20 p.
5.2  Subsampling by splitting

Be', A. W. H.  1959.  A method for rapid sorting of Foraminifera from marine
plankton samples.  J. Paleontol. 33:846-848.

Bowen, R. A., J. M. St. Onge, J. B. Colton and C. A. Price.  1972.  Density-
gradient centrifugation as an aid to sorting planktonic organisms.  I.
Gradient materials.  Mar. Biol. 14:242-247.

Burrell, V. G., W. A. Van Engel, and S. G. Hummel.  1974.  A new device for
subsampling plankton samples.  J. Cons. perm. int. Explor. Mer. 35:364-366.
                                      35

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 Furnass, T. I. and W. C. Findley.  1975.  An improved sorting device for
 zooplankton.  Limnol. Oceanogr. 20:295-297.

 Horwood, J. W. and R. M. Driver.  1976.  A note on a theoretical subsampling
 distribution of macroplankton.  J. Cons. perm. int. Explor.  Mer. 36(3):274-
 276.

 Kirkerud, L. A.  1974.  A method for the rapid sorting of plankton into a
 number of size groups.  J. Cons. perm.  int. Explor. Mer.  35:367-369.

 Longhurst, A.  R.  and D.  L. R. Siebert.   1967.   Skill in the  use of Folsom's
 plankton sample splitter.  Limnol. Oceanogr.  12:334-335.

 McEwen, G. F., M.  W. Johnson and T.  R.  Folsom.  1954.   A statistical analysis
 of the performance of the Folsom plankton sample splitter based upon test
 observations.   Arch. Meteorol. Geophys. Bioklimatol.,  Ser. A Meleorol.
 Geophys.  7:502-527.

 McGowan,  J.  A.  and V. J. Fraundorf.   1964.   A modified heavy fraction zoo-
 plankton sorter.   Limnol. Oceanogr.  9:152-154.

 Nival,  S.  and  P. Nival.   1971.  A simple device for the sorting of living
 planktonic copepods.  Limnol. Oceanogr. 16:977-980.

 Venrick,  E.  L.   1971. The statistics of subsampling.   Limnol.  Oceanogr.  16:
 811-818.
 5.3  Biomass

 Ahlstrom,  E. H. and  J. R.  Thrailkill.   1963.  Plankton volume  loss with  time
 of preservation.   Calif. Coop.  Oceanic  Fish.  Invest. Rep. 9:57-73.

 Beers, J.  R.  1976.  Determination of zooplankton biomass.  Pp.  35-84.   In
 H. F. Steedman  [Ed.] Zooplankton  fixation  and preservation.  UNESCO.  Mon-
 ographs on oceanographic methodology.   No.  4.   350 p.

 Curl, H.,  Jr.  1962.  Analyses  of carbon in marine plankton organisms.   J.
 Mar. Res.  20:181-188.

 Fudge, H.  1968.   Biochemical analysis  of  preserved zooplankton.  Nature
 219:380-381.

Harris, R. H.  1976.  Freeze drying,  pp.  97-99.  In: H. F. Steedman  [Ed.],
Zooplankton fixation and preservation.  UNESCO.  Monographs on oceanographic
methodology.  No.  4.  350 p.

Howey,  T.  W.  1976.  Zooplankton of the Gulf of Mexico.  Distribution of
displacement volume, occurrence of systematic groups, abundance and diversity
among copepods.   Dissertation L.S.U.  93 p.
                                     36

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Lovegrove, T.   1962.  The effect of various factors on dry weight values.
Rapp.  Cons. Explor. Her. 153:86-91.

Lovegrove, T.   1966.  The determination of the dry weight of plankton and
the  effects of  various  factors  on the values obtained,  pp. 429-467.  In:
H. Barnes  (Ed.).   Some  contemporary studies in marine science.  London,
Allen  and  Univinn  Ltd.  716 p.

Nakai,  Z.  1955.   The chemical  composition, volume, weight and size of the
important  marine plankton.  Spec. Publs Tokai Fish. Res. Lab. 5:12-24.

Nakai,  Z.  and K. Honjo.  1962.  Comparative studies on measurements of the
weight and the  volume of plankton samples.  A preliminary account.  Indo-Pac.
Fish Counc. Proc., 9th  Sess., Sec. II, p. 9-16.

Platt,  T., M. Brown and B. Irvin.  1969.  Caloric and carbon equivalents of
zooplankton biomass.  J. Fish.  Res. Bd. Can. 26:2345-2349.

Platt,  T.  and B. Irvin.  1973.  Caloric content of phytoplankton.  Limnol.
Oceanogr.  18:306-310.

Smith,  R.  L.  1966.  Ecology and field biology.  Harper and Rowe.  New York.
686  p.

Steedman,  H. F.  1974.  Laboratory methods in the study of marine zooplankton.
J. Cons. perm.  int. Explor. Mer., 35:351-358.

Utermohl,  H.  1958.  Zur Vervollkommuny der quantitativen Phytoplankton.
Methodik.  Mitt. d. Int. Vereinig f. Limnologie, no. 9, 39 p.

van  Heusden, G. P. H.   1972.  Estimation of the biomass of plankton.
Hydrobiologia 39:165-208.

Wiebe,  P.  H., K. H. Burt, S. H. Boyd and J. L. Cox.  1975.  Relationships
between zooplankton displacement volume, wet weight, dry weight, and carbon.
Fish.  Bull. 73(4):777-786.

Yentsch, C. S., and J.  E. Hebard.  1957.  A gauge for determining plankton
volume  by  the mercury immersion method.  J. Cons. perm. int. Explor. Mer.,
22:184-190.
6.2  Total protein analysis

Lowry, 0. H., N. J. Rosebrough, A. L. Farr, and R. J. Randall.  1951.
Protein measurement by the Folin-phenol reagent.  J._ Biol. Chem. 196:
265-275.

Parvin, R., S. V. Parde and T. A. Venkitasubramanian.  1965.  On the color-
imetric biuret method of protein determination.  Analyt. Biochem. 12:219-229.
                                     37

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 Raymont, J.  E.  G.,  J. Austin  and  E. Linford.  1964.  Biochemical studies on
 marine  zooplankton.  I.  The  biochemical composition of Neomysis integer.
 J. Cons. perm.  int.  Explor. Her.  28:354-363.


 6.3  Total lipid analysis

 Armenta, J.  S.  1964.  A rapid chemical method for quantification of lipids
 separated by thin-layer chromatography.  J. Lipid Res. 5:270-272.

 Bligh, E. G. and W. J. Dyer.  1959.  A rapid method of total lipid extraction
 and purification.  Chr. J. Biochem. Physiol. 37:911-917.

 Donaldson, H. A.  1976.  Chemical composition of sergestid shrimps (Decapoda:
 Natantia) collected near Bermuda.  Mar. Biol. 38:51-58.

 Fisher, L. R.  1962.  The total lipid material in some species of marine
 zooplankton.  Rapp. Cons. Explor. Her. 153:129-136.

 Folch, J., M. Lees and G. H. Sloane Stanley.  1957.  A simple method for the
 isolation and purification of total lipids from animal tissues.  J.  biol.
 Chem.  226:646-648.

 Metcalfe, L.  D.  and A.  A. Schmitz.  1961.   The rapid preparation of  fatty
 acid  esters for gas chromatographic analysis.  Anal.  Chem.  33:363-364.

 Raymont, J.  E.  G.,  J. Austin and E.  Linford.  1964.  Biochemical studies on
 marine zooplankton.   I.   The biochemical composition of Neomysis integer.
 J.  Cons. perm.  int.  Explor.  Mer.  28:354-363.

 Zb'llner, N.  and  K.  Kirsch.   1962.   Uber die quantitative Bestimmuny  von
 Lipoider (Mikromethode)  mittels  den vielen naturllchen Lipoiden (Allen
 bekannten Plasmalipoiden)  gemeinsamen  Sulfophosphovanillen  -  Reaktion.
 Zectschrift  fur  die  gesamte  exper. Med.  135:545-561.
 6.4   Carbohydrate  analysis

 Dubois, M.,  K. A.  Gills,  J.  K.  Hamilton,  P. A. Reebers,  and  F.  Smith.   1956.
 Colorimetric method  for determination  of  sugars  and  related  substances.
 Anal. Chem.  28:350-356.

 Krey, J.   1950.  Eine neue Methode  Zur quantitativen Bestimmuny des Plankton.
 Kieler Meeresforsch  7:58-75.

Mendel, B.,  A. Kemp  and D. K. Myers.   1954.  A colorimetric  micromethod for
 the determination  of glucose.   J. Biochem. 56:639-46.

Raymont, J.  E. G., J. Austin and E. Linford.  1964.  Biochemical studies on
marine zooplankton.  I.  The biochemical  composition of Neomysis integer.
J. Cons. perm. int.  Explor. Mer. 28:354-363.
                                     38

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6.5  Ash analysis  (See also Sec. 5.3.7)

Raymont, J. E. G., J. Austin and E. Linford.  1964.  Biochemical studies on
marine zooplankton.  I.  The biochemical composition of Neomysis integer.
J. Cons. perm. int. Explor. Her. 28:354-363.


6.6  Chitin analysis

Baumstedt, V.  1974.  Biochemical studies on the deep-water pelagic community
of Korsfjorden, Western Norway.  Methodology and sample design.  Sarsia 56:
71-86.

Raymont, J. E. G., J. Austin and E. Linford.  1964.  Biochemical studies on
marine zooplankton.  I.  The biochemical composition of Neomysis integer.
J. Cons. perm. int. Explor. Her. 28:354-363.
6.7  Other analyses

American Oil Chemists' Society.  1965.  Official and tentative methods.
Chicago, 111.

Culkin, F. and R. J. Morris.  1969.  The fatty acids of some marine crus-
taceans.  Deep. Sea. Res. 16:109-116.

Culkin, F. and R. J. Morris.  1970.  The fatty acids of some cephalopods.
Deep-Sea Res. 17:171-174.

Folch, J., M. Lees and G. H. Sloane Stanley.  1957.  A simple method for the
isolation and purification of total lipids from animal tissues.  J. biol.
Chem. 226:497-509.

Klein, F. K. and H. Rapoport.  1970.  A two-dimensional pipette for sample
application in preparative thin-layer chromatography.  J. Chromatography
47:505-506.

Morrison, W. R. and L. M. Smith.  1964.  Preparation of fatty acid methyl
esters and dimethylacetates from lipids with boron fluoride-methanol.  J.
Lipid Res. 5:600-608.

Raymont, J. E. G., J. Austin and E. Linford.  1968.  Biochemical studies on
marine zooplankton.  V.  The composition of the major biochemical fractions
in Neomysis integer.  J. mar. biol. Ass. U.K. 48:735-760.

Srinivasagam, R. T., J. E. G. Raymont, C. F. Woodie,_and J. K. B. Raymont.
1971.  Biochemical studies on marine zooplankton.  X.  The amino acid
composition of Euphausia superba, Meganyctiphanes norvegica and Neomysis
integer.  J. mar. biol. Ass. U.K. 51:917-925.
                                     39

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 6.8  The biochemistry of zooplankton

 Ackman, R. G. and C. A. Eaton.  1966.  Lipids of the fin whale (Balaenoptera
 physalus) from North Atlantic waters.  III.  Occurrence of eicosenoic and
 docosenoic fatty acids in the zooplankter Meganyctiphanes norveigca (M.  Sears)
 and their effect on whale oil composition.  Can. J.  Biochem.  44:1561-1566.

 Ackamn, R. G. and C. A. Eaton.  1967.  Fatty acid composition of the decapod
 shrimp Pandalus borealis in relation to that of the  euphausid Meganyctiphanes
 norvegica.  J. Fish. Res. Bd. Can. 24:467-471.

 Ackman, R. G., C. S. Tocher and J. McLachlan.  1968.  Marine  phytoplankter
 fatty acids.   J.  Fish. Res. Bd. Can.  25:1603-1620.

 Ackman, R. G., C. A. Eaton, J. C.  Sipos,  S. N.  Hooper and J.  D.  Castell.
 1970.   Lipids and fatty acids of two species of North Atlantic krill
 (Meganyctiphanes  norvegica and Thysanoessa inermis)  and their role  in the
 aquatic food  web.  J.  Fish. Res.  Bd.  Can.  27:513-533.

 Armenta,  J. S.  1964.   A rapid chemical method  for quantification of lipids
 separate  by thin-layer chromatography.  J. Lipid Res.  5:270-272.

 Barnes, H. , M. Barnes, and D.  M.  Finlayson.  1963.   The seasonal  changes  in
 body weight,  biochemical composition, and  oxygen uptake of two common boreo-
 arctic cirripedes,  Balanus balanoides and  B.  balanus.   J.  mar. biol.  Ass.
 U.K. 43:185-211.

 Barnes, H. and R.  Evens.   1967.   Studies in the biochemistry  of  cirripede
 eggs.   III.   Changes in the amino-acid  composition during  development of
 Balanus balanoides  and B_.  balanus.   J.  mar. biol. Ass.  U.K. 47:171-180.

 Bartley,  W.,  L. M.  Birt and P.  Banks.   1968.  The biochemistry of tissues.
 John Wiley.   375  pp.

 Beers,  J.  R.   1966.  Studies on the  chemical  composition of the major zoo-
 plankton  groups in  the Sargasso Sea off Bermuda.  Limnol.  Oceanogr.  11:
 520-528.

 Benson, A. A.  and R. F.  Lee.   1975.   The role of wax in oceanic food  chains.
 Sci. Am.  232:77-86.

 Beyer,  F.  1962.  Absorbtion of water in crustaceans, and  the  standing crop
 of zooplankton.   Rapp.  Cons.  Explor. Mer.  153:79-85.

 Bligh,  E.  G.  and W.  J.  Dyer.   1959.   A  rapid method  of  total  lipid extraction
 and purification.  Can. J.  Biochem. Physiol.  37:911-917.

 Blumer, M., M. M. Mullin and R. R. L. Guillard.  1970.  A  polyunsaturated
hydrocarbon (3, 6, 9,  12,  15,  18 - hereicosahexaene  in  the marine food web.
Mar. Biol. 6:226-235.
                                     40

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Blumer, M. , M. M. Mullin  and D. W. Thomas.  1963.  Pristane in zooplankton.
Science, N. Y.   140:974.

Blumer, M., M. M. Mullin  and D. W. Thomas.  1964.  Pristane in the marine
environment.  Helgolander wiss.  Meeresunters. 10:187-201.

Bogorov, B. G.   1934.   Seasonal changes  in biomass of Calanus finmarchicus
in  the Plymouth  area in 1930.  J. mar. biol. Ass. U.K. 19:585-611.

Bottino, N. R.   1974.   The  fatty acids of Antarctic phytoplankton and
euphausiids:  fatty acid  exchange among  trophic levels of the Ross Sea.
Mar. Biol. 27:197-204.

Bottino, N. R.,  L. M. Jeffrey and R. Reiser.  1967a.  Metabolism of long-
chain polyunsaturated fatty acids in Antarctic euphausia.  Fed. Proc. 26:
795.

Bottino, N. R.,  L. M. Jeffrey and R. Reiser.  1967b.  The lipids of Antarctic
fish.  Antarctic J. U.S.  2:194-195.

Brant, K.  1898.  Beitrage  zur Kenntniss der chemischen zusammensetzung der
Planktons.  Wiss. Merresuntersuch., Abt. Kiel, N.F. 3:43-90.

Brant, K. and E. Raben.   1919.  Zur Kenntnis der Cehmischen zusammensetung
des Planktons und einiger Bodenorganismen.  Wiss. Merresuntersuch., Abt.
Kiel, N.F. 19:175-210.

Brockerhoff, H., M. Yurkowski, R. J. Hoyle, and R. G. Ackman.  1964.  Fatty
acid distribution in lipids of marine plankton.  J. Fish. Res. Bed. Can.
21:1379-1384.

Burkholder, P. K. , E. F.  Mandelli and P. Centeno.  1967.  Some chemical
properties of Munida gregaria and Euphausia superba.  J. Agric. Fd. Chem.
15:718-720.

Camien, M. M., H. Sanlet, G. Duchateau and M. Florkin.  1951.  Non-protein
amino acids in muscle and blood of marine and freshwater Crustacea.  J. biol.
Chem. 193:881-885.

Christomanos, A. A., A. Dimitriadis and V. Gardiki.  1962.  Contribution to
plankton chemistry.  I.   Chim. Chron. 27(A):23-26.

Clarke, G. L. and S. S. Gellis.  1935.  The nutrition of copepods in relation
to the food cycle of the  sea.  Biol. Bull. Woods Hole.  68(2):231-246.

Collier, A.  1967.  Fatty acids in certain planktonic. organisms.  In
Estuaries (Ed. G. H. Lauff), pp. 353-360.  Publ. No. 83, AAAS, Wash. D.C.

Conover, R. J.   1959.   Regional and seasonal variation in the respiratory
rate of marine copepods.  Limnol. Oceanogr. 4:259-268.
                                     41

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 Corner, E. D. S. and C. B. Cowey.  1964.  Some nitrogenous constituents of
 the plankton.  Ann. Rev. Oceanogr. mar. Biol. (Ed. H. Barne), George Allen
 and Unwin Ltd. London. 2:146-167.

 Corner, E. D. S. and C. B. Cowey.  1968.  Biochemical studies on the produc-
 tion of marine zooplankton.  Biol. Rev. 43:393-426.

 Corner, E. D. S. and B. S. Newell.  1967.  On the nutrition and metabolism
 of zooplankton.  IV.  The forms of nitrogen excreted by Calanus.  J. mar*
 biol. Ass. U.K. 47:113-120.

 Cowey, C. B. and E. D. S. Corner.  1962.  The amino acid compositions of
 Calanus helgolandicus (Glaus) in relation to that of its food.  Rapp. Cons.
 Explor. Her. 153:124-128.

 Cowey, C. B. and E. D. S. Corner.  1963a.  Amino acids and some other
 nitrogenous compounds in Calanus finmarchicus.   J. mar.  biol.  Ass.  U.K.
 43:485-493.

 Cowey, C.  B.  and E. D.  S. Corner.  1963b.  On the nutrition and metabolism
 of zooplankton.   II.  The relationship between  the marine copepod Calanus
 heloglandlcus and particulate material in Plymouth sea water,  in terms of
 amino-acid composition.   J.  mar. biol. Ass.  U.K.  43:495-511.

 Cowey, C.  B.  and E. D.  S.  Corner.  1966.  The amino-acid composition of
 certain unicellular algae,  and of the  faecal pellets produced by Calanus
 finmarchicus  when feeding on them.   In Some  Contemporary Studies in Marine
 Science,  (ed.  H.  Barnes),  pp.  225-231, George Allen and  Unwin  Ltd.  London.

 Culkin,  F. and R.  J.  Morris.   1969.  The fatty acids of  some  marine crus-
 taceans.   Deep-Sea Res.  16:109-116.

 Culkin,  F. and R.  J.  Morris.   1970.  The fatty acids of  some  cephalopoda.
 Deep-Sea Res.  17:171-174.

 Curl,  H.   1962a.   Standing  crops of  carbon,  nitrogen,  and phosphorus and
 transfer between  trophies  levels,  in continental  shelf waters  south of
 New York.  Rapp.  Cons. Explor. Her.  153:183-189.

 Curl, H.   1962b.  Analyses of  carbon in  marine plankton  organisms.   J.  Mar.
 Res. 20:181-188.

 Davis, C.  C.   1944.  On four species of  Copepoda  new to  Chesapeake  Bay,  with
 a description  of  a  new variety of Paracalanus crassirostris.   Dahl.  Publ.
 Chesapeake Biol. Lab. No.  (61):1-11.

Dawson, R. M. C. and H. Barnes.   1966.   Studies in  the biochemistry  of
cirripede eggs.  II.  Changes in  lipid composition  during development  of
Balanus balanoides  and _B. balanus.  J. mar. biol. Ass. U.K. 46:249-261.

Donaldson, H. A.  1976.  Chemical composition of  sergestid  shrimps  (Decapoda:
Natantia) collected near Bermuda.  Mar.  Biol. 38:51-58.


                                     42

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 Dubois,  M., K. A.  Gills, J. K. Hamilton, P. A. Reebers and F. Smith.  1956,
 Colorimetric method  for determination of sugars and related substances.
 Anal.  Chem. 28:350-356.

 Farkas,  T. and S.  Herodek.  1964.  The effect of environmental temperature on
 the  fatty  acid composition of  crustacean plankton.  J. Lipid Res. 5:369-373.

 Ferguson,  C. F.  and  J. K. B. Raymont.  1974.  Biochemical studies in marine
 zooplankton.  XII.   Further investigations  on Euphausia superba Dana.  J.
 mar. biol. Ass.  U.K.  54:719-725.

 Fisher,  L. R.  1962.  The total  lipid material in some species of marine
 zooplankton.  Rapp.  Cons. Explor. Mer. 153:129-136.

 Florkin, M. and  E. Schoffeniels.  1965.  Euryhalinity and the concept of
 physiological radiation.  In Studies in Comparative Biochemistry (K. A.
 Munday,  Ed.), p. 6-40.  Pergamon, Oxford.

 Folch, J., M. Lees and G. H. Sloane Stanley.  1956.  A simple method for  the
 isolation  and purification of  total lipids  from animal tissues.  J. biol.
 Chem.  226(a):497-509.

 Harris,  E.  1959.  The nitrogen  cycle in Long Island Sound.  Bull. Bingham
 Oceanogr.  Coll.  17:31-65.

 Harris,  E. and G.  A.  Riley.  1956.  Oceanography of Long Island Sound, 1952-
 1954.  VIII.  Chemical composition of the plankton.  Bull. Bingham Oceanogr.
 Coll.  15:315-323.

 Harris,  R. R.  1969.  Free amino acid and haemolymph concentration in
 Sphaeroma  rugicarida  (Isopoda) during adaptation to a dilute salinity.
 J. exp.  Biol. 50:319-326.

 Hinchcliffe, P.  R. and J. P. Riley.  1972.  The effect of diet on the
 component  fatty-acid  composition of Artemia salina.  J. mar. biol. Ass.
 U.K. 52:203-211.

 Holm-Hansen, 0.  1968.  Determination of particulate organic nitrogen.
 Limnol.  Oceanogr.  13:175-178.

 Hopkins, T. L.   1968.  Carbon  and nitrogen  content of fresh and preserved
 Nematoscelis difficilis, a euphausid crustacean.  J. Cons. perm. int. Explor.
 Mer 31(3):300-304.

 Ikeda, T.  1971.   Changes in respiration rate and in composition of organic
 matter in  Calanus  cristatus (Crustacea, Copepoda) -under starvation.  Bull.
 Fac. Fish. Hakkaido Univ. 21:280-298.

 Jawed, M.  1969.  Body nitrogen and nitrogenous excretion in Neomysis rayii
Murdoch and Euphausea pacifica Hansen.  Limnol. Oceanogr. 14:748-754.
                                     43

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 Jeffries, H. P.  1970.  Seasonal composition of temperate plankton commun-
 ities:  fatty acids.  Limnol. Oceanogr. 5(3):419-425.

 Jeffrey, L. M., N. R. Bottino and R. Reiser.  1966.  The distribution of
 fatty acid classes in lipids of antarctic euphausids.  Antarctic J. U.S.
 1:209.

 Jezyk, P. F. and A. J. Penicnak.  1966.  Fatty acid relationships in an
 aquatic food chain.  Lipids 1:427-429.

 Johannes, R. E., S. J. Coward and K. L. Webb.   1969.   Are dissolved amino
 acids an energy source for marine invertebrates?  Comp. Biochem.  Physiol.
 29:283-288.

 Johannes, R. E.  and K. L.  Webb.   1965.  Release of dissolved amino acids by
 marine zooplankton.  Science 150:76-77.

 Johannes, R. E.  and K. L.  Webb.   1970.  Release of dissolved organic compounds
 of marine and freshwater invertebrates.  In (D. Hood, ed.).  Organic Matter in
 Natural Waters.   Univ. of  Alaska Press, College,  Alaska,  p.  257-273.

 Kayama,  M., Y.  Tsuchiya and J.  T.  Mead.  1963.   A model experiment of aquatic
 food  chain with special significance in fatty   acid  conversion.   Bull.  Jap.
 Soc.  Fish.  29:452-458.

 Kelly,  P.  B.,  R.  Reiser and D.  W.  Hood.  1959.   The origin of marine poly-
 unsaturated fatty acids.   Composition of some  marine  plankton.   J.  Amer.
 Oil Chem.  Soc.  36:104-106.

 Klem,  A.   1932.   Contributions  to  the study of  the oils of marine Crustacea.
 I.  The  oils of  Meganyctiphanes  norvegica,  M.  Sara and Calanus  finmarchicus
 Gunn.  Hvalradets  Skr.  6:24  p.

 Krey,  J.   1950.   Eine neue Methode  Zur quantitativen  Bestimmung  des
 Planktons.   Kieler  Meeresforsch  7:58-75.

 Krishnaswamy, S., J.  Tundisi and J.  E.  G. Raymont.  1966.  The measurement
 of succinic  dehydrogenase activity  in ascidians.   Naturwiss.  17,  441, 1-2.

 Krishnaswamy, S., J.  Tundisi and J.  E.  G. Raymont.  1967.  Succinic
 dehydrogenase activity  in marine animals.   Int. Revue  ges. Hydrobiol. 52:
 447-451.

 Kryuchkova, M. I.,  and 0. E.  Makarov.   1969.  Technochemical  characteristics
 of krill.  Trudy vues nachno-issled.   Inst. morsk.  ryb. Khoz. Okeanogr.
 Vol. 66, pp. 295-298.   (Translation  RE  55-94, Nat. Lend. Lib. Sci.  Tech).

Lasker, R.  1966.  Feeding,  growth,  respiration and carbon utilization of  a
 euphausid crustacean.  J. Fish.  Res.  Bd. Can. 23:1291-1317.
                                     44

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 Lee,  R.  F.,  and J.  Hirota.   1973.  Wax  esters  in  tropical  zooplankton and
 nekton and  the  geographical  distribution  of wax esters  in  marine  copepods.
 Limnol.  Oceanogr.  18:227-239.

 Lee,  R.  F.,  J.  Hirota and A. M.  Barnett.   1971.   Distribution and importance
 of  wax esters in marine  copepods and  other zooplankton.  Deep-Sea Res.  18:
 1147-1165.

 Lee,  R.  F.,  J.  C.  Kevenzel and  G. A.  Paffenhdfer.   1970.   Wax esters in marine
 copepods.   Science 167:1510-1511.

 Lee,  R.  F.,  J.  C.  Nevenzel,  and G. A. Paffenhofer.   1971.  Importance of wax
 esters and  other lipids  in the  marine food chain:   phytoplankton  and copepods.
 Mar.  Biol.  9:99-108.

 Lee,  R.  F.  J. Nevenzel,  G. A. Paffenhofer and  A.  A.  Benson.  1970.  The
 metabolism  of wax  esters and other lipids by the  marine copepod,  Calanus
 helgolandicus.   J.  Lipid Res. 11:237-240.

 Lewis,  R. W.  1967.   Fatty acid composition of some  marine animals  from
 various  depths.  J. Fish. Res.  Bd. Can. 24:1101-1115.

 Lewis,  R. W.  1969.   The fatty  acid composition of  Arctic  marine  phyto-
 plankton and zooplankton with special reference to  minor acids.   Limnol.
 Oceanogr. 14:35-40.

 Linford, E.  1965.  Biochemical studies on marine zooplankton.  II.  Vari-
 ations  in the lipid content  of  some Mysidacea.  J.  Cons. perm.  int. Explor.
 Mer 30:16-27.

 Littlepage, J.  L.   1964.  Seasonal variation in lipid content of  two
 Antarctic marine crustaces.  Biol. Antarctique, Actual.  Scient. Ind.
 1312:463-470.

 Lockwood, A. P. M.  1968.  Aspects of the Physiology of Crustacea.  Oliver
 and Boyd, Edinburg  and London;  328 pp.

 Lovegrove, T.   1962.  The effect of various factors  on  dry weight values.
 Rapp. Cons. Explor. Mer  153:86-91.

 Lovegrove, T.   1966.  The determination of the dry  weight  of plankton and
 the effect of various factors on the  values obtained.   In: Some Contemporary
 Studies  in Marine  Science (ed.  H. Barnes), George Allen and Unwin,  London,
 716 pp.

 Lovern, J. A.   1935.  Fat metabolism  in fishes.  VI. _The  fats  of some
 plankton Crustacea.  Biochem. J. 29:847-849.

 Lovern, J. A.   1964.  The lipids of marine organisms.   Ann. Rev.  Oceanogr.
Mar. Biol. 2:169-191.
                                     45

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 Lowry, 0. H., N. J. Rosebrough, A. L. Farr and R. J. Randall.  1951.  Protein
 measurement by the Folin-Phenol Reagent.  J. Biol. Chem. 196:265-275.

 Manwell, C., C. M. Baker, P. Ashton and E. 0. Corner.  1967.  Biochemical
 differences between Calanus finmarchicus and _C. helgolandicus.  Esterases,
 malate, and triosephosphate, dehydrogenase, aldolase, 'peptidases' and other
 enzymes.  J. mar. biol. Ass. U.K. 47:145-169.

 Marshall, S. M. and A. P. Orr.  1955.  On the biology of Calanus finmarchicus.
 J. mar. biol. Ass. U.K. 34:495-529.

 Marshall, S. M. and A. P. Orr.  1962.  Feeding and digestion in marine
 copepods.  UNESCO Conference on Radiosotopes in Scientific Research.
 UNESCO/NS/RIC/137  6 pp.

 Mayzaud, P.   1973.  Respiration and nitrogen excretion of zooplankton.  II.
 Studies of the metabolic characteristics of starved animals.  Mar. Biol.  21:
 19-28.

 Mendel, B.,  A.  Kemp and D.  K.  Myers.   1954.   A colorimetric micro-method  for
 the determination of glucose.   J.  Biochem.  56:639-646.

 Metcalfe, L.  D.  and A. A. Schmitz.  1961.   The rapid preparation of fatty
 acid esters  for gas chromatographic analysis.   Anal.  Chem.  33:363-364.

 Morris, R. J.   1971.   Seasonal and environmental  effects on the lipid compo-
 sition of Neomysis integer.   J. mar.  biol.  Ass. U.K.  51(1):21-32.

 Morris, R. J.   1973a.   Relationships  between the  sex and degree of maturity
 of marine crustaceans  and their lipid compositions.   J.  mar. biol.  Ass. U.K.
 53:27-37.

 Morris, R. J.   1973b.   Changes  in  the lipid  composition  of  Acantephyra
 purpurea  Milne  Edwards (Crustacea:Decapoda)  during its diurnal  migration:
 a  preliminary investigation.   J. exp.  mar. Biol.  Ecol. 13:550-61.

 Morris, R. J., C.  F. Ferguson  and  J.  E.  G. Raymont.   1973.   Preliminary
 studies on the lipid metabolism of Neomysis  integer,  involving  labelled
 feeding experiments.   J.  mar.  biol. Ass. U.K.  53:657-664.

 Morris, R. J. and J. R.  Sargent.   1973.  Studies  on  the  lipid metabolism  of
 some oceanic crustaceans.  Mar.  Biol.  22:77-83.

 Nakai,  Z.  1955.  The  chemical  composition, volume, weight  and  size  of the
 important marine plankton.  Spec.  PubIs. Tokai Fish.  Res. Lab.  5:12-24.

Nevenzel, J.  C.  1970.  Occurrence, function and biosynthesis of wax esters
 in marine organisms.  Lipids 5:308-319.

Omori, M.  1969.  Weight and chemical composition of  some important  oceanic
zooplankton in the North Pacific Ocean.  Mar. Biol. 3:4-10.
                                     46

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 Orr,  A.  P.   1934a.   The weight  and  chemical composition of Euchaeta norvegica
 Boeck.   Proc. Roy  Soc. Edinb. B, 54:51-55.

 Orr,  A.  P.   1934b.   On the biology  of Calanus finmarchicus.  Part IV.  Sea-
 sonal changes in the weight  and chemical composition in Loch Fyne.  J. mar.
 biol.  Ass.  U.K. 19:613-632.

 Parvin,  R. ,  S. V.  Fade and T. A. Venkitasubramanian.  1965.  On the color-
 imetric  biuret method of protein determination.  Analyt. Biochem. 12:219-229.

 Petipa,  T.  S.  1966.  Oxygen consumption and food requirement in copepods
 Acartia  clausi Giesbricht and A_. lalisetosa Kritoz.  Zool. Zhurnal 45:363-70.

 Petipa,  T.  S., E.  V. Pavlova and G. N. Mironov.  1970.  The food web struc-
 ture,  utilization  and transport of  energy by trophic levels in the planktonic
 communities.  In:  Marine Food  Chains (ed. J. H. Steele), pp. 142-167.

 Raymont, J.  E. G., J. Austin and E. Linford.  1964.  Biochemical studies on
 marine zooplankton.  I.  The biochemical composition of Neomysis integer.
 J. Cons. perm. int.  Explor.  Her 28:354-363.

 Raymont, J.  E. G., J. Austin and E. Linford.  1966.  Biochemical studies on
 marine zooplankton.  III.  Seasonal variation in the biochemical composition
 of Neomysis  integer.  In Some Contemporary Studies in Marine Science, ed. H.
 Barnes,  pp.  597-605.  London.

 Raymont, J.  E. G., J. Austin and E. Linford.  1967.  Biochemical composition
 of certain oceanic zooplanktonic decapods.  Deep-Sea Res. 14:113-115.

 Raymont, J.  E. G., J. Austin and E. Linford.  1968.  Biochemical studies on
 marine zooplankton.  V.  The composition of the major biochemical fractions
 in Neomysis  integer.  J. mar. biol. Ass. U.K. 48:735-760.

 Raymont, J.  E. G.  and R. J.  Conover.  1961.  Further investigations on the
 carbohydrate content of marine  zooplankton.  Limnol. Oceanogr. 6:154-164.

 Raymont, J.  E. G.  and S. Krishnaswamy.  1960.  Carbohydrate in some marine
 planktonic animals.  J. mar. biol. Ass. U.K. 39:239-248.

 Raymont, J. E. G., S. Krishnaswamy and J. Tundisi.  1967.  Biochemical
 studies  on marine  zooplankton.  IV.  Investigations on succinic dehydrogenase
 activity in zooplankton with special reference to Neomysis integer.  J. cons.
 perm. int. Explor.  Mer. 31:164-169.

 Raymont, J. E. G. and E. Linford.  1966.  A note on the biochemical compo-
 sition of some Mediterranean zooplankton.  Int. Revue_ges. Hydrobiol. 51:
 485-488.

 Raymont, J. E. G.,  R. J. Morris, C. F. Ferguson and J. K. D. Raymont.  1975.
Variation in the amino-acid  composition of lipid-free residues of marine
animals  from the northeast Atlantic.  J. exp. mar. Biol. Ecol. 17:261-267.
                                     47

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 Raymont, J. E. G., R. T. Srinlvasagam, and J. K. B. Raymont.  1969a.
 Biochemical studies on marine zooplankton.  VI.  Investigations on
 Meganyctiphanes norvegica (M. Sars).   Deep-Sea Res. 16:141-156.

 Raymont, J. E. G. , R. T. Srinivasagam, and J. K. B. Raymont.  1969b.
 Biochemical studies on marine zooplankton.  VII.  Observations on certain
 deep sea zooplankton.  Int.  Revue ges. Hydrobiol. 54:357-365.

 Raymont, J. E. G., R. T. Srinivasagam and J. K. B. Raymont.   1971a.
 Biochemical studies on marine zooplankton.  VIII.  Further investigations
 on Meganyctiphanes norvegica (M. Sars).   Deep-Sea Res.  18:1167-1178.

 Raymont, J. E. G.,  R. T. Srinivasagam and J. K. B. Raymont.   1971b.
 Biochemical studies on marine zooplankton.  IX.  The biochemical composition
 of Euphausla superba.  J.  mar.  biol.  Ass. U.K.  51:581-588.

 Reeve,  M.  R.,  J.  E. G. Raymont  and J. K.  B.  Raymont.  1970.   Seasonal
 biochemical composition and  energy sources of Sagitta hispida-  Mar. Biol.
 6(4):357-364.

 Saiki,  M.,  S.  Fang and T.  Mori.   1959.  Studies on the  lipid of plankton.
 II.   Fatty acid composition  of  lipids from Euphausiacea collected in the
 Antarctic  and  northern Pacific  Ocean.  Bull. Jap.  Soc.  Sci.  Fish.  24:837-839.

 Sequin,  G.   1968.  Contribution a 1'etude biochimique de Praunus flexuosus
 (Muller).   Deep-Sea Res.  15:491-492.

 Shewbart,  K. L.,  W.  L.  Mies  and  P.  D.  Ludwig.   1972.   Identification and
 quantitative analysis of the amino  acids  present in protein  of the brown
 shrimp  Penaeus aztecus.  Mar. Biol. 16:64-67.

 Sidhu,  G.  S.,  W.  A.  Montgomery,  G.  L.  Holloway,  A.  R. Johnson  and  D.  M.
 Walker.  1970.  Biochemical  composition and  nutritive value  of krill
 (Euphausia  superba  Dana).  J. Sci.  Fd. Agric. 21:293-296.

 Simpson, J.  W., K.  Allen and J.  Awapara.   1959.   Free amino  acids  in some
 aquatic  invertebrates.   Biol. Bull.   Woods Hole  117:371-381.

 Sipos, J. C. and  R.  G. Ackman.   1968.  Jellyfish (Cyanea capillata)  lipids;
 fatty acid  composition.  J.  Fish. Res. Bd.,  Can.  25:1561-1569.

 Srinivasagam,  R. T.,  J. E.  G. Raymont, C. F. Moodie  and J.  K.  B.  Raymont.
 1971.  Biochemical  studies on marine  zooplankton.   X.   The amino acid compo-
 sition of Euphausia  superba, Meganyctiphanes norvegica  and Neomysis  integer.
J. mar. biol. Ass. U.K. 51:917-925.

Suyama, M., K. Nakajima and  J. Nonaka.  1965.  Studies  on the  protein and
non-protein nitrogenous constituents  of Euphausia.  Bull. Jap.  Soc.  Scient.
Fish. 31:302-306.

Vinogradov, A.  P.  1953.  The elementary  chemical composition  of marine
 )rganisms.  Mem. Sears Found. Mar. Res. 2:1-647.

                                      48

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 Vinogradova,  Z.  A.   I960.   Study of  the biochemical  composition of Antarctic
 krill (Euphausia superba Dana).   Dokl. Akad.  Nauk  SSSR  133:68-682.   (N.L.L.
 Translation.)

 Vinogradova,  Z.  A.   1964.   Some  biochemical aspects  of  a comparative study
 of plankton from the Black Sea,  the  Sea of Azov and  the Caspian Sea.
 Okeanologiya 4(2):232-242.

 Webb,  K.  L.  and  R.  E.  Johannes.   1967.  Studies of the  release of dissolved
 free  amino acids by marine zooplankton.   Limnol. Oceanogr.  12:376-382.

 Webb,  K.  L.,  R.  E.  Johannes and  S. J. Coward.  1971.  Effects of salinity and
 starvation on release of dissolved free amino acids  by  Dugesia dorotocephala
 and Bdelloura Candida (Platyhelminth.es, Turbellaria).   Biol. Bull. 141:364-
 371.

 Yamada, M.   1961.   Studies on  the lipid of plankton.  I.  The lipid of
 Neomysis  nakazawaii.   J. Japan Oil Chem.  Soc.  10:236-239.

 Yamada, M.   1964.   The lipid of  plankton.  Bull. Jap. Soc.  Sci., Fish.  30:
 673-681.

 Zollner,  N.  and  K.  Kirsch.   1962.  Uber die quantitative bestimmung von
 lipoiden  (mikromethode)  mittels  der  vie len natur  lichen lipoiden (alien
 bekannten plasmalipoiden)  gemeinsamen sulfo phosphovantillin-reaction.
 Zeitschrift  fur  gesanite exper Medizine 135:545-561.
7.1  Total numbers  and  frequency of occurrence.

Anraku, M.  1975.   Microdistribution of marine copepods in a small inlet.
Mar. Biol. 30:79-87.

Brinton, E.  1962.  Variable factors affecting the apparent range and esti-
mated concentration of  euphausiids in the North Pacific.  Pacific Sci. 16:
374-408.

Deevey, G. B.  1956.  Oceanography of Long Island Sound, 1952-1954.  5.
Zooplankton.  Bull. Bingham Oceanogr. Collect. 15:113-155.

Deevey, G. B.  1971.  The annual cycle in quantity and composition of the
zooplankton of the  Sargasso Sea off Bermuda.  I.  The upper 500 m.  Limnol.
Oceanogr. 18:219-240.

Egan, W. G. and J.  E. Conrad.  1975.  Summer abundance and ecology of zoo-
plankton in the Gulf Stream.  Biol. Bull. 149:492-505.

Grice, G. A. and A. D. Hart.  1962.  The abundance, seasonal occurrence, and
distribution of the epizooplankton between New York and Bermuda.  Ecol.
Monogr. 32:287-309.
                                     49

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 7.2  Diversity indices

 Goodman, D.  1975.  The theory of diversity - stability relationships in
 ecology.  Quart. Rev. Biol. 50:237-266.

 Haedrich, R. L.  1975.  Diversity and overlap as measures of environmental
 quality.  Water Res. 9:945-952.

 Hurlbert, S. H.  1971.  The nonconcept of species diversity:  a critique and
 alternative parameters.  Ecology 52:577-586.

 Lloyd, M. and R. J. Gherlardi.  1964.  A table for calculating the "equitabil-
 ity" component of species diversity.  J. Anim. Ecol.  33:217-225.

 Lloyd, M. J., J. H. Zar and J. R. Karr.  1968.  On the calucation of infor-
 mation-theoretical measures of diversity.  Amer.  Midland Naturalist 79:257-
 272.

 Margalef, R.  1968.  Perspectives in ecological theory.   University of Chicago
 Press.   Chicago, 111.   Ill p.

 Peet,  R. K.   1975.   Relative diversity indices.   Ecology 56:496-498.

 Sager,  P. and A.  D. Easier.   1969.   Species diversity in lacustrine phyto-
 plankton.  I.  The  components  of the index of diversity  from Shannon's
 formula.  Amer.  Natur.  103:51-59.

 Sanders, H.  L.   1968.   Marine  benthic diversity:   a comparative study.   Am.
 Natur.  102:243-282.

 Shannon, C.  E.  and  W. Weaver.   1963.   The mathematical theory of  communica-
 tion.   Univ.  of  Illinois Press.   Urbanna, 117 pp.

 Simpson, G.  G.   1960.   Notes on the  measurement of  faunal  resemblance.   Am.
 J. Sci.  258-A:300-311.

 Whittaker, R. H. and C. W. Fairbanks.   1958.   A study of plankton  copepod
 communities  in the  Columbia  Basin, Southeastern Washington.   Ecology  39:46-65.

 Wilhm, J. L.  1968.  Use of  biomass  units in  Shannon's formula.  Ecology 49:
 153-156.
7.3  Multivariate analysis

Boesch, D. F.  1976.  Application of numerical classification in ecological
investigations of water pollution.  Virginia Inst. of Marine Science, Spec.
Sci. Rept. No. 77, 114 p.

Clifford, H. T. and W. Stephenson.  1975.  An introduction to numerical
classification.  Academic Press.  New York.  229 p.
                                     50

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Colebrook, J. M.  1969.  Variability in the plankton.  Progress in Ocean-
ography.  Ed. Mary Sears. 5:115-125.

Colebrook, J. M.  1977.  Annual fluctuations in biomass of taxonomic group of
zooplankton in the California Current, 1955-59.  Fish. Bull. 75:357-368.

Fager, E. W.  1957.  Determination and analysis of recurrent groups.  Ecology
38:586-595.

Fager, E. W. and J. A. McGowan.  1963.  Zooplankton species groups in the
North Pacific.  Science 140:453-460.

Pielou, E. C.  1969.  An introduction to mathematical ecology.

Williams, W. T.  1971.  Principles of clustering.  Ann. Rev. Ecol. Syst. 2:
303-326.
                                     51

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                                     TECHNICAL REPORT DATA
                             (Please read Instructions on the reverse before completing)
 1. REPORT NO.
   EPA-600/3-78-026
                                                             3. RECIPIENT'S ACCESSION NO.
 4. TITLE AND SUBTITLE
   GUIDELINES  FOR ZOOPLANKTON  SAMPLING IN QUANTITATIVE
   BASELINE AND MONITORING PROGRAMS
                                                             5. REPORT DATE
                                                              February 1978
              6. PERFORMING ORGANIZATION CODE
 7. AUTHOR(S)
   Fred Jacobs  and George C. Grant
              8. PERFORMING ORGANIZATION REPORT NO
                Special Scientific  Report
                  No.  83
 9. PERFORMING ORGANIZATION NAME AND ADDRESS

   Department  of  Planktology
   Virginia  Institute of Marine Science
   Gloucester  Point,  VA  23062
              10. PROGRAM ELEMENT NO.

                 1 BA 025
              11. CONTRACT/GRANT NO.
                                                                EPA-R-804147010
 12. SPONSORING AGENCY NAME AND ADDRESS
   Corvallis Environmental Research Laboratory
   Office of Research  and Development
   U.S. Environmental  Protection Agency
   Corvallis, Oregon   97330
              13. TYPE OF REPORT AND PERIOD COVERED
                Final Report	
              14. SPONSORING AGENCY CODE
                 EPA/600/02
 15. SUPPLEMENTARY NOTES
 16. ABSTRACT

    Methods applicable  to zooplankton  sampling and analysis  in  quantitative baseline
    and monitoring surveys are evaluated  and summarized.  Specific recommendations  by
    managers must take  into account characteristics of the water  mass under investi-
    gation, the abundance of contained zooplankton and phytoplankton populations  and
    the objectives of the study.  Realistic  planning and development must also consider
    available monetary  and manpower resources.

    This report was submitted in fulfillment of Contract No. R804147010 by the Virginia
    Institute of Marine Science under  the sponsorship of the U.S. Environmental Pro-
    tection Agency.  This report covers a period from 24 Nov 75,  to 31 May 77, and
   work was completed  as of 25 Feb 77.
                                KEY WORDS AND DOCUMENT ANALYSIS
                  DESCRIPTORS
                                               b.IDENTIFIERS/OPEN ENDED TERMS
                           c.  COSATl F-'ield/Group
            Marine biology
            Sampling
            Water pollution
            Zooplankton
                             08/A
 8. DISTRIBUTION STATEMENT

    Release to  public
19. SECURITY CLASS (This Report I
  unclassified
21. NO. OF PAGES
 60
                                               20. SECURITY CLASS (Thispage)
                                                 unclassified
                                                                          22. PRICE
EPA Form 2220-1 (Rev. 4-77)   PREVIOUS EDITION is OBSOLETE
                                              52
    U.S. GOVERNMENT PRINTING OFflCEi 1978—799-946/86 REGION 10

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