Chapter 2 - SOUTHERN OCEAN FIELD STUDY: SUMMARY & RECOMMENDATIONS
In this section we summarize the recommendations of the GLOBEC meeting
on Marine Animal Populations and Climate Change in the Southern Ocean,
distilled from the Working Group Reports which are presented in their
entirety in Section 7. These recommendations are intended to serve as
guidelines for specific GLOBEC studies.
For each taxonomic group - zooplankton, benthos and top predators
- the recommendations are organized according to Site Selection
criteria, with the exception that criteria relating to climate change
are first discussed in general as applicable to all populations
considered, and aspects of international, inter-program and
inter-agency activity are discussed in a separate section following
this one (Section 3). An outline of the suggested logistics of the
field study is presented in Section 4.
2.1 Relation to Climate Change
The Southern Ocean is in many respects an ideal region in which to
study marine animal populations in the context of global climate
change. Meteorological dynamics are likely to impact coastal zones,
areas covered by sea ice, and may affect the large-scale
circulation. Present ocean-atmosphere models of the earth suggest that
the Southern Ocean may be the last part of the ocean to experience
warming, but other effects of global atmospheric warming could take
precedence.
Coastal ocean regions are believed to be the places
in which climate change would most influence marine animal
populations, primarily through changes in meltwater input and solar
radiation. Meltwater input would be induced by melting of the polar
icecap, and solar radiation is expected to decrease over the
ocean. Either of these processes will affect water column stability,
leading to changes in vertical mixing and the primary productivity
which fuels higher trophic levels. Animal populations are most
concentrated in coastal regions.
Sea ice covers roughly half of the Southern Ocean during winter and
approximately 10% during the summer. The annual cycle of accretion and
melting contributes significantly to primary production, again by
altering water column stability. Furthermore, the ice edge is a region
where marine animals congregate in large numbers. Long term effects of
global warming are expected to reduce the seasonality of sea ice and
could result in the eventual absence of summer ice. These effects are
likely to greatly reduce the productivity and habitat for marine
animal populations.
Changes in the flow intensity of circumpolar current may also be
anticipated, brought on by a reduced temperature contrast between the
equator and the poles which would reduce the strength of prevailing
circumcontinental westerly winds. It is clear that circumpolar current
interacts with ocean bathymetry to yield areas of high primary
production, but it is not clear how global climate change would impact
overall production in the circumpolar region.
The key recommendations identified with respect to climate change are:
- To organize and analyze existing historical data to compensate for
the lack of long term observations;
- To make consistent and synoptic observations of sea ice and
currents in the Southern Ocean, to optimize the ability to detect the
effects of a climate change;
- To improve the understanding of how meteorological conditions
drive variability in sea ice extent; and
- To improve observations of coastal circulation, which determines
the distribution of marine animal populations.
2.1.1 Approach
The general approach is to undertake studies which will address the
role that climate plays in determining local and regional episodic
events, mass transport, and total energy of the marine system. Such
studies should employ satellites, moored instruments, and
drifters. Coupled with a better understanding of how physical
mechanisms affect marine populations, this approach will lead to the
basis for predicting how climate change will affect population
dynamics.
2.2 Zooplankton, Including Krill
2.2.1 Target species
Krill (Euphausia superba) has clear economic and ecological
importance, and is suggested as the primary target species. Other
species of primary interest include Salpa thompsoni, which can
be especially dominant but about which little is known, Euphausia
crystallorophias, a coastal and high Antarctic species, and two
abundant copepod species, Calanoides acutus and Calanus
propinquus. These species together represent the spectrum of
different life strategies and the bulk of the zooplankton biomass in
the Southern Ocean. Other species of interest would include
Themisto gaudichaudi, Metridia gerlachei, Rhincalanus
gigas, Thysanoessa macrura, and Sagitta gazellae.
2.2.2 Definable populations
The Bellingshausen Sea is a region where relatively discrete
populations of krill and other holozooplankton might be maintained, by
virtue of a regional gyral circulation, which may restrict
communication with adjacent seas. An area directly west of the Ross
Sea, bounded by the continent to the south, 65 deg S, and 140 to
160 deg E, has supported a consistent krill fishery for some time, and
may also possess populations definable in space and time. The details
of regional circulation in both areas are poorly known, and will
require study. However, geostrophic circulation patterns presented in
Stein (in press) suggest the presence of two gyres in this region that
partly overlay the continental shelf (Figure 1). These features may be
persistent Key objectives of a field study would include:
- Sampling surveys of sufficient frequency to define the temporal
and spatial extent of discrete populations, and developmental cohorts;
- The use of biochemical and genetic marker techniques to clearly
identify populations.
Figure 1. Geopotential anomalies from the recent work of Stein (in press) suggest the presence of two gyres
in the coastal and slope regions of the Bellingshausen Sea.
2.2.3 Population dynamics
The primary goal of population dynamics studies on krill and other zooplankton is to better define demographic parameters, particularly in the context of regional circulation. Such studies will require year-round sampling, with particular emphasis on the role of sea ice in structuring the community. The following particular studies are indicated:
- Much more data are required on populations in the winter,
especially on the role of demographic parameters of populations in
determining the size of populations during the productive summer
season;
- Identification and study of those demographic parameters which may
be especially sensitive to climate change, and to temperature
increases in particular.
2.2.4 Focus on process and mechanisms
Process studies would be carried out on cruises designed specifically
for that purpose, as well as at the numerous shore-based laboratories
in the Antarctic Peninsula region. Particular attention should be paid
to measuring rates of metabolism, egg production, feeding, growth and
development, as well as investigating the diapause
phenomenon. Research might include the following studies:
- Determination of the environmental triggers for metabolic and
behavioral events, noting that very small changes (i.e., 0.5 deg C) may
trigger change;
- Comparison of metabolic responses between extremes in environment
(e.g. summer vs. winter);
- Measurement of physiological responses to conditions outside the
normal environmental range;
- Determination of the relative sensitivity of various developmental
stages to environmental variables, to understand which stages are most
vulnerable.
2.2.5 Historical database
Relatively little information exists on plankton distributions in the
Bellingshausen Sea, although the nearby waters of the Antarctic
Peninsula region are perhaps the best studied in all the Southern
Ocean. This is particularly important because waters from the
Bellingshausen Sea provide some of the flow through the northern
reaches of the Antarctic Peninsula coastal region, and thus the fauna
of the Bellingshausen are already reasonably well known. The BIOMASS
data base, centered at the British Antarctic Survey in Cambridge UK,
may prove a valuable resource.
2.2.6 Modeling
Specific modeling studies recommended include:
- Design of models to investigate life cycles of zooplankton, with
particular emphasis on determining the results of different
life-history strategies (e.g. seasonally migrating vs. non-migrating
species);
- Development of coupled biological-physical numerical models for
krill and other zooplankton populations at the study site, with
particular emphasis on interactions with regional scale circulation,
and with finer-scale resolution, especially in the vertical;
- Development of models regarding the formation, maintenance and
dissolution of patches, with particular emphasis on krill.
2.2.7 Technology
Certain developments in technology will be applicable to all taxonomic
categories of interest, particularly in the case of field sampling
instruments. Those of special interest to zooplankton and krill
studies would include:
- Improvement of instrumentation needed to sample the upper 10 rn of
the water column as well as under sea ice, where current
instrumentation is inadequate;
- Improvement of large volume sampling techniques to determine the
abundance, biomass and distribution of salps with minimal disturbance
to aggregates;
- Development of non-invasive techniques to observe distributions of
krill and other zooplankton in both ice-covered and ice-free areas.
2.2.8 References
Stein, M. 1991. Variability of local upwelling off the Antarctic
Peninsula, 19861990. Archiv far Fischwiss. (In Press)
2.3 Benthos
2.3.1 Target species
Five characteristics were considered as criteria for the selection of
benthie species, primarily that the species: (1) have measurable
growth parameters, (2) be abundant, (3) have either a wide or
restricted distribution, (4) have a known life history, and (5) be
amenable to reproductive studies. Given these constraints, the
following species are particularly recommended (p and b
denote pelagic and benthie larval forms, respectively):
- Bivalves: Adamussium (p), Laternula (p), Mysella (b), Gamardia (b)
- Echinoderms: Odontaster (p), Sterechinus (p), Ophionotus (p), Diplasteria (b)
- Crustaceans: Notocrangon (p), Chorismus (p), Glyptonotus (p)
2.3.2 Definable populations
Populations that would be definable in time and space would be likely
to occur in the following areas, distributed from high to low
Antarctic:
High Antarctic:
- Ross Sea/McMurdo Sound
- Southeast Weddell Sea Davis Sea
Low Antarctic:
- South Orkney/South Shetland Islands
- Antarctic Peninsula/Bellingshausen Sea
In particular, genetic studies would be desirable for distinguishing
between populations.
2.3.3 Population dynamics
Measurements relative to the population dynamics of benthic species
(e.g. recruitment, life history strategies) should be done in
conjunction with measurements on physical processes. Particular
studies recommended include:
- Colonization processes in areas exposed by recent calving of major
portions of ice shelf;
- Species succession in areas with high iceberg grounding frequency;
- Studies that emphasize observations during winter, a period for
which little is known.
2.3.4 Focus on process and mechanisms
Studies should be conducted to understand how fundamental parameters
of population dynamics, such as growth, reproduction, larval
dispersal, behavior, settlement and survival vary directly and
indirectly as a function of physical and biological
forcing. Particular processes or parameters which should be studied
with reference to potential global change include:
- Processes delivering carbon to the benthos via vertical flux of
particulate matter;
- Ice conditions in the overlying water,
- Flow of local currents;
- Temperature and salinity;
- Light regimes; and
- Redox profiles in sediments.
Measurements of the response of individuals and populations should be
assessed with particular regard to:
- Energy flow;
- Physiological response, which would provide information on rates
and processes;
- Population dynamics;
- Community structure, which would assess the effects of
environmental change on species composition, abundance and biomass.
2.3.5 Historical database
A large body of data exists on benthic communities near a number of
Antarctic field stations. Some effort should be made to gather these
data and make them available at an accessible central location.
2.3.6 Modeling
Modeling studies are encouraged which
- Evaluate the processes of aggregation, dispersal and settlement of
meroplanktonic larvae;
- Assess the role of large-scale climatic changes on physiology and
population dynamics of discrete populations.
2.3.7 Technology
Developments in technology are particularly required in the following areas:
- Quantitative assessment of distribution and abundance using
video and camera technology;
- Methods for determining the age of individuals.
2.4 Top Predators
2.4.1 Target species
Target species are recommended among fishes, birds and mammals. For
fish, these include
- Commercially harvested species
Champsocephalus gunnari
Notothenia larseni
Electrona carlsbergi
- Non-harvested holopelagic species
Pleuragramma antarctica
Electrona antarctica
- Non-harvested nearshore species
Notothenia neglecta
Trematomus hansoni
Harpagifer sp.
Species in the first group occur primarily in the Atlantic sector and
are already included in CCAMLR monitoring studies. The second group
are species abundant in food webs of the high Antarctic and represent
contrasting ecological and life history patterns. The third group
contains species which are conveniently collected from shore stations.
Among the birds, key species of interest include Adelie, chinstrap,
macaroni and gentoo penguins, cape and Antarctic petrels, Black-broWed
albatross, grey headed albatross and South Polar skua. It is noted
that roughly 2/3 of the Southern Ocean bird biomass is comprised of
Adelie penguins; other species are recommended for a variety of
specialized reasons.
Target species recommended among the mammals are the crabeater
seal and the Antarctic fur seal. Both are largely dependent on krill
as a food resource, and occupy habitats analogous to those of Ade1ie
and chinstrap penguins.
2.4.2 Definable populations
In the Atlantic sector of the Southern Ocean, which is generally
recommended as a primary study region, it is generally felt that
CCAMLR subareas represent reasonable approximations of the
distribution of fish populations. Distributions of bird and seal
populations may represent distinct populations, but studies are
required to verify this assumption. Specific studies should include:
(1) Better assessment of species distributions in time and space; and
(2) Molecular techniques (e.g. mitochondrial DNA) applied to distinguish
popuations.
2.4.3 Population dynamics
Some of the important demographic parameters for target populations
can be acquired directly from the CCAMLR monitoring program. These
would include data on spawning stock biomass, growth and reproduction
of commercially taken fishes, and the growth rate, breeding success
and cohort survival of birds and seals. Studies particttlarly
encouraged under GLOBEC would include:
- Assessment of growth and developmental rates of larval fishes as
related to biotic and physical environments;
- Foraging dynamics of birds and seals, with special emphasis on
winter; and
- Marking and tracking studies on birds and seals which assist in
identifying populations and observing behavior.
2.4.4 Focus on process and mechanisms
Certain key processes are expected to reveal the response of top
predator populations to global change. This calls for studies focused
on:
- Effects of temperature on growth and development of different
ontogenetic stages of fishes;
- Overwintering studies of top predators to determine critical
mortality periods;
- Potential effects of UV radiation on near-surface fish eggs and
larvae;
- Effects of physical circulation on dispersal of early life stages
of fishes;
- The importance of food availability on physiological condition and
reproductive behavior, and
- Foraging dynamics of top predators in relation to prey abundance
and aggregation behavior.
2.4.5 Historical database
Relatively sound historical databases have been collected through the
CCAMLR and BIOMASS programs, as well as through various national
programs in the US, UK, Germany, France, Australia, New Zealand and
South Africa. Access to these should be made readily to principal
investigators conducting studies in the GLOBEC framework.
2.4.6 Modeling
Specific studies recommended for modeling exercises include:
- Effects of the physical environment and fluid dynamics on food
supply, growth and development rates, survivorship and dispersal of
the early life history stages of fish;
- Development of a standard population dynamics model for seabirds,
integrating physiological data with environmental variables;
- Models of movement and dispersal of foraging predators to
determine how seabirds and seals locate food patches;
- Effects of climate and fishing pressure on harvested species;
- Trophodynamic models of multispecies interactions between fish,
higher predators, and their prey.
2.4.7 Technology
Special technological advances which could greatly aid studies of top
predators in the Southern Ocean include:
- Improved acoustical hardware and Software for locating,
identifying and quantifying the abundance of fish;
- Underwater visual systems for assessing the distributions of prey
items (e.g. krill and pelagic fishes);
- Improved satellite tracking and time-depth recording devices for
predators;
- Improved techniques for remote sensing of sea ice, either by
satellite or aircraft, which yield higher resolution and which better
differentiate sea-ice conditions;
- Biochemical methods for evaluating fish condition factors;
- Genetic markers for determining stock identity; and
- Increased use of Lagrangian drifters to observe current transport
and advective processes.
2.5 General Modeling Issues
Many of the issues relevant to modeling marine populations in the
Antarctic have already been considered as part of the discussions for
each taxonomic group. However, there are additional issues that are
relevant to a GLOBEC program in the Southern Ocean.
First, it is now apparent that many of the components of the
Antarctic food web are dependent on sea ice during some or all of
their life history. The time scales of this dependence range from days
(for phytoplankton) to years (for seals and marine birds) and extend
over space scales of a few meters to 100s of kilometers. Thermodynamic
models of sea ice, that describe the annual growth and melting of an
uniform ice field, are reasonably well developed. Schemes for
incorporating thermodynamic sea ice models into general circulation
models exist. However, the existing sea-ice models are simple and do
not include processes such as rafting of sea-ice, and the existing
coupled ocean-ice models do not consider flow underneath the ice,
which can be important for biological populations. Assuming that
climate change effects in the Antarctic will be reflected in the
variability and extent of sea-ice cover, then the development of
realistic sea-ice models that can be interfaced with circulation and
biological models is a critical area of research. Also models that
incorporate the feedbacks between sea-ice cover and higher predators,
that are decoupled from the flow field (e.g. penguins) need
development.
Second, any GLOBEC initiative planned for the Southern Ocean will
likely have a regional focus, i.e., Bellingshausen Sea. However, the
circulation models developed for regional studies will need to include
the effects of the larger scale circulation of the Southern
Ocean. Thus, techniques for combining the results of large-scale
circulation models (e.g. FRAM) with results from regional circulation
models need development. A related problem is that the space and time
scales resolved in physical models are often inappropriate for
biological processes. In particular, the vertical resolution of
circulation models is frequently not consistent with that needed to
adequately model biological processes. Thus, methods for scaling
between circulation and biological models need development.
Third, there is a need for the development of models that can
simulate the aggregation behavior of animals such as
krill. Considerable theory on modeling animal aggregation and swarming
behavior has been developed for terrestrial systems. Efforts need to
be made to transfer and adapt this theory for marine populations.