Crustacea in Arctic and Antarctic Sea Ice: Distribution, Diet and Life History Strategies
This review concerns crustaceans that associate with sea ice. Particular emphasis is placed on comparing and contrasting the Arctic and Antarctic sea ice habitats, and the subsequent influence of these environments on the life history strategies of the crustacean fauna. Sea ice is the dominant featu...
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ftunivtasmania:oai:eprints.utas.edu.au:2164 2023-05-15T13:36:46+02:00 Crustacea in Arctic and Antarctic Sea Ice: Distribution, Diet and Life History Strategies Arndt, CE Swadling, KM Southward, A.J. Sims, D.W. 2006 application/pdf https://eprints.utas.edu.au/2164/ https://eprints.utas.edu.au/2164/1/ArndtSwadling_AMB2006.pdf https://doi.org/10.1016/S0065-2881(06)51004-1 en eng Elsevier https://eprints.utas.edu.au/2164/1/ArndtSwadling_AMB2006.pdf Arndt, CE and Swadling, KM 2006 , 'Crustacea in Arctic and Antarctic Sea Ice: Distribution, Diet and Life History Strategies', in A.J. Southward and D.W. Sims (eds.), Advances in Marine Biology , Elsevier, pp. 197-315. cc_utas 270702 Marine and Estuarine Ecology (incl. Marine Ichthyology) Book Section PeerReviewed 2006 ftunivtasmania https://doi.org/10.1016/S0065-2881(06)51004-1 2020-05-30T07:15:54Z This review concerns crustaceans that associate with sea ice. Particular emphasis is placed on comparing and contrasting the Arctic and Antarctic sea ice habitats, and the subsequent influence of these environments on the life history strategies of the crustacean fauna. Sea ice is the dominant feature of both polar marine ecosystems, playing a central role in physical processes and providing an essential habitat for organisms ranging in size from viruses to whales. Similarities between the Arctic and Antarctic marine ecosystems include variable cover of sea ice over an annual cycle, a light regimen that can extend from months of total darkness to months of continuous light and a pronounced seasonality in primary production. Although there are many similarities, there are also major diVerences between the two regions: The Antarctic experiences greater seasonal change in its sea ice extent, much of the ice is over very deep water and more than 80% breaks out each year. In contrast, Arctic sea ice often covers comparatively shallow water, doubles in its extent on an annual cycle and the ice may persist for several decades. Crustaceans, particularly copepods and amphipods, are abundant in the sea ice zone at both poles, either living within the brine channel system of the ice-crystal matrix or inhabiting the ice–water interface. Many species associate with ice for only a part of their life cycle, while others appear entirely dependent upon it for reproduction and development. Although similarities exist between the two faunas, many diVerences are emerging. Most notable are the much higher abundance and biomass of Antarctic copepods, the dominance of the Antarctic sea ice copepod fauna by calanoids, the high euphausiid biomass in Southern Ocean waters and the lack of any species that appear fully dependent on the ice. In the Arctic, the ice-associated fauna is dominated by amphipods. Calanoid copepods are not tightly associated with the ice, while harpacticoids and cyclopoids are abundant. Euphausiids are nearly absent from the high Arctic. Life history strategies are variable, although reproductive cycles and life spans are generally longer than those for temperate congeners. Species at both poles tend to be opportunistic feeders and periods of diapause or other reductions in metabolic expenditure are not uncommon. Book Part Antarc* Antarctic Arctic Arctic Sea ice Southern Ocean Copepods University of Tasmania: UTas ePrints Antarctic Arctic Southern Ocean The Antarctic 197 315 |
institution |
Open Polar |
collection |
University of Tasmania: UTas ePrints |
op_collection_id |
ftunivtasmania |
language |
English |
topic |
270702 Marine and Estuarine Ecology (incl. Marine Ichthyology) |
spellingShingle |
270702 Marine and Estuarine Ecology (incl. Marine Ichthyology) Arndt, CE Swadling, KM Crustacea in Arctic and Antarctic Sea Ice: Distribution, Diet and Life History Strategies |
topic_facet |
270702 Marine and Estuarine Ecology (incl. Marine Ichthyology) |
description |
This review concerns crustaceans that associate with sea ice. Particular emphasis is placed on comparing and contrasting the Arctic and Antarctic sea ice habitats, and the subsequent influence of these environments on the life history strategies of the crustacean fauna. Sea ice is the dominant feature of both polar marine ecosystems, playing a central role in physical processes and providing an essential habitat for organisms ranging in size from viruses to whales. Similarities between the Arctic and Antarctic marine ecosystems include variable cover of sea ice over an annual cycle, a light regimen that can extend from months of total darkness to months of continuous light and a pronounced seasonality in primary production. Although there are many similarities, there are also major diVerences between the two regions: The Antarctic experiences greater seasonal change in its sea ice extent, much of the ice is over very deep water and more than 80% breaks out each year. In contrast, Arctic sea ice often covers comparatively shallow water, doubles in its extent on an annual cycle and the ice may persist for several decades. Crustaceans, particularly copepods and amphipods, are abundant in the sea ice zone at both poles, either living within the brine channel system of the ice-crystal matrix or inhabiting the ice–water interface. Many species associate with ice for only a part of their life cycle, while others appear entirely dependent upon it for reproduction and development. Although similarities exist between the two faunas, many diVerences are emerging. Most notable are the much higher abundance and biomass of Antarctic copepods, the dominance of the Antarctic sea ice copepod fauna by calanoids, the high euphausiid biomass in Southern Ocean waters and the lack of any species that appear fully dependent on the ice. In the Arctic, the ice-associated fauna is dominated by amphipods. Calanoid copepods are not tightly associated with the ice, while harpacticoids and cyclopoids are abundant. Euphausiids are nearly absent from the high Arctic. Life history strategies are variable, although reproductive cycles and life spans are generally longer than those for temperate congeners. Species at both poles tend to be opportunistic feeders and periods of diapause or other reductions in metabolic expenditure are not uncommon. |
author2 |
Southward, A.J. Sims, D.W. |
format |
Book Part |
author |
Arndt, CE Swadling, KM |
author_facet |
Arndt, CE Swadling, KM |
author_sort |
Arndt, CE |
title |
Crustacea in Arctic and Antarctic Sea Ice: Distribution, Diet and Life History Strategies |
title_short |
Crustacea in Arctic and Antarctic Sea Ice: Distribution, Diet and Life History Strategies |
title_full |
Crustacea in Arctic and Antarctic Sea Ice: Distribution, Diet and Life History Strategies |
title_fullStr |
Crustacea in Arctic and Antarctic Sea Ice: Distribution, Diet and Life History Strategies |
title_full_unstemmed |
Crustacea in Arctic and Antarctic Sea Ice: Distribution, Diet and Life History Strategies |
title_sort |
crustacea in arctic and antarctic sea ice: distribution, diet and life history strategies |
publisher |
Elsevier |
publishDate |
2006 |
url |
https://eprints.utas.edu.au/2164/ https://eprints.utas.edu.au/2164/1/ArndtSwadling_AMB2006.pdf https://doi.org/10.1016/S0065-2881(06)51004-1 |
geographic |
Antarctic Arctic Southern Ocean The Antarctic |
geographic_facet |
Antarctic Arctic Southern Ocean The Antarctic |
genre |
Antarc* Antarctic Arctic Arctic Sea ice Southern Ocean Copepods |
genre_facet |
Antarc* Antarctic Arctic Arctic Sea ice Southern Ocean Copepods |
op_relation |
https://eprints.utas.edu.au/2164/1/ArndtSwadling_AMB2006.pdf Arndt, CE and Swadling, KM 2006 , 'Crustacea in Arctic and Antarctic Sea Ice: Distribution, Diet and Life History Strategies', in A.J. Southward and D.W. Sims (eds.), Advances in Marine Biology , Elsevier, pp. 197-315. |
op_rights |
cc_utas |
op_doi |
https://doi.org/10.1016/S0065-2881(06)51004-1 |
container_start_page |
197 |
op_container_end_page |
315 |
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