Ecology of Southern Ocean pack ice
Around Antartica the annual five-fold growth and decay of sea ice is the most prominent physical process and has a profound impact on marine life there. In winter the pack ice canopy extends to cover almost 20 million square kilometres — some 8% of the southern hemisphere and an area larger than the...
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ftunstandrewcris:oai:risweb.st-andrews.ac.uk:publications/03835026-afd2-4ccb-bffd-f3a07356549f 2023-05-15T13:45:52+02:00 Ecology of Southern Ocean pack ice Brierley, Andrew Stuart Thomas, DN 2002 https://risweb.st-andrews.ac.uk/portal/en/researchoutput/ecology-of-southern-ocean-pack-ice(03835026-afd2-4ccb-bffd-f3a07356549f).html https://doi.org/10.1016/S0065-2881(02)43005-2 http://www.scopus.com/inward/record.url?scp=0036322973&partnerID=8YFLogxK eng eng info:eu-repo/semantics/restrictedAccess Brierley , A S & Thomas , DN 2002 , ' Ecology of Southern Ocean pack ice ' , Advances in Marine Biology , vol. 43 , pp. 171-276 . https://doi.org/10.1016/S0065-2881(02)43005-2 ANTARCTIC SEA-ICE KRILL EUPHAUSIA-SUPERBA DISSOLVED ORGANIC-MATTER WESTERN WEDDELL SEA FORAMINIFER NEOGLOBOQUADRINA-PACHYDERMA COPEPOD PARALABIDOCERA-ANTARCTICA TRANSPARENT EXOPOLYMER PARTICLES SOLAR ULTRAVIOLET-RADIATION CALANOIDES-ACUTUS COPEPODA MARINE PRIMARY PRODUCTION article 2002 ftunstandrewcris https://doi.org/10.1016/S0065-2881(02)43005-2 2021-12-26T14:10:56Z Around Antartica the annual five-fold growth and decay of sea ice is the most prominent physical process and has a profound impact on marine life there. In winter the pack ice canopy extends to cover almost 20 million square kilometres — some 8% of the southern hemisphere and an area larger than the Antarctic continent itself (13.2 million square kilometres) — and is one of the largest, most dynamic ecosystems on earth. Biological activity is associated with all physical components of the sea-ice system: the sea-ice surface; the internal sea-ice matrix and brine channel system; the underside of sea ice and the waters in the vicinity of sea ice that are modified by the presence of sea ice. Microbial and microalgal communities proliferate on and within sea ice and are grazed by a wide range of proto- and macrozooplankton that inhabit the sea ice in large concentrations. Grazing organisms also exploit biogenic material released from the sea ice at ice break-up or melt. Although rates of primary production in the underlying water column are often low because of shading by sea-ice cover, sea ice itself forms a substratum that provides standing stocks of bacteria, algae and grazers significantly higher than those in ice free areas. Decay of sea ice in summer releases particulate and dissolved organic matter to the water column, playing a major role in biogeochemical cycling as well as seeding water column phytoplankton blooms. Numerous zooplankton species graze sea-ice algae, benefiting additionally because the overlying sea-ice ceiling provides a refuge from surface predators. Sea ice is an important nursery habitat for Antarctic krill, the pivotal species in the Southern Ocean marine ecosystem. Some deep-water fish migrate to shallow depths beneath sea ice to exploit the elevated concentrations of some zooplankton there. The increased secondary production associated with pack ice and the sea-ice edge is exploited by many higher predators, with seals, seabirds and whales aggregating there. As a result, much of the ... Article in Journal/Newspaper Antarc* Antarctic Antarctic Krill Antarctica antartic* Euphausia superba ice algae Neogloboquadrina pachyderma Sea ice Southern Ocean Weddell Sea University of St Andrews: Research Portal Antarctic Southern Ocean The Antarctic Weddell Sea Weddell 171 IN4 |
institution |
Open Polar |
collection |
University of St Andrews: Research Portal |
op_collection_id |
ftunstandrewcris |
language |
English |
topic |
ANTARCTIC SEA-ICE KRILL EUPHAUSIA-SUPERBA DISSOLVED ORGANIC-MATTER WESTERN WEDDELL SEA FORAMINIFER NEOGLOBOQUADRINA-PACHYDERMA COPEPOD PARALABIDOCERA-ANTARCTICA TRANSPARENT EXOPOLYMER PARTICLES SOLAR ULTRAVIOLET-RADIATION CALANOIDES-ACUTUS COPEPODA MARINE PRIMARY PRODUCTION |
spellingShingle |
ANTARCTIC SEA-ICE KRILL EUPHAUSIA-SUPERBA DISSOLVED ORGANIC-MATTER WESTERN WEDDELL SEA FORAMINIFER NEOGLOBOQUADRINA-PACHYDERMA COPEPOD PARALABIDOCERA-ANTARCTICA TRANSPARENT EXOPOLYMER PARTICLES SOLAR ULTRAVIOLET-RADIATION CALANOIDES-ACUTUS COPEPODA MARINE PRIMARY PRODUCTION Brierley, Andrew Stuart Thomas, DN Ecology of Southern Ocean pack ice |
topic_facet |
ANTARCTIC SEA-ICE KRILL EUPHAUSIA-SUPERBA DISSOLVED ORGANIC-MATTER WESTERN WEDDELL SEA FORAMINIFER NEOGLOBOQUADRINA-PACHYDERMA COPEPOD PARALABIDOCERA-ANTARCTICA TRANSPARENT EXOPOLYMER PARTICLES SOLAR ULTRAVIOLET-RADIATION CALANOIDES-ACUTUS COPEPODA MARINE PRIMARY PRODUCTION |
description |
Around Antartica the annual five-fold growth and decay of sea ice is the most prominent physical process and has a profound impact on marine life there. In winter the pack ice canopy extends to cover almost 20 million square kilometres — some 8% of the southern hemisphere and an area larger than the Antarctic continent itself (13.2 million square kilometres) — and is one of the largest, most dynamic ecosystems on earth. Biological activity is associated with all physical components of the sea-ice system: the sea-ice surface; the internal sea-ice matrix and brine channel system; the underside of sea ice and the waters in the vicinity of sea ice that are modified by the presence of sea ice. Microbial and microalgal communities proliferate on and within sea ice and are grazed by a wide range of proto- and macrozooplankton that inhabit the sea ice in large concentrations. Grazing organisms also exploit biogenic material released from the sea ice at ice break-up or melt. Although rates of primary production in the underlying water column are often low because of shading by sea-ice cover, sea ice itself forms a substratum that provides standing stocks of bacteria, algae and grazers significantly higher than those in ice free areas. Decay of sea ice in summer releases particulate and dissolved organic matter to the water column, playing a major role in biogeochemical cycling as well as seeding water column phytoplankton blooms. Numerous zooplankton species graze sea-ice algae, benefiting additionally because the overlying sea-ice ceiling provides a refuge from surface predators. Sea ice is an important nursery habitat for Antarctic krill, the pivotal species in the Southern Ocean marine ecosystem. Some deep-water fish migrate to shallow depths beneath sea ice to exploit the elevated concentrations of some zooplankton there. The increased secondary production associated with pack ice and the sea-ice edge is exploited by many higher predators, with seals, seabirds and whales aggregating there. As a result, much of the ... |
format |
Article in Journal/Newspaper |
author |
Brierley, Andrew Stuart Thomas, DN |
author_facet |
Brierley, Andrew Stuart Thomas, DN |
author_sort |
Brierley, Andrew Stuart |
title |
Ecology of Southern Ocean pack ice |
title_short |
Ecology of Southern Ocean pack ice |
title_full |
Ecology of Southern Ocean pack ice |
title_fullStr |
Ecology of Southern Ocean pack ice |
title_full_unstemmed |
Ecology of Southern Ocean pack ice |
title_sort |
ecology of southern ocean pack ice |
publishDate |
2002 |
url |
https://risweb.st-andrews.ac.uk/portal/en/researchoutput/ecology-of-southern-ocean-pack-ice(03835026-afd2-4ccb-bffd-f3a07356549f).html https://doi.org/10.1016/S0065-2881(02)43005-2 http://www.scopus.com/inward/record.url?scp=0036322973&partnerID=8YFLogxK |
geographic |
Antarctic Southern Ocean The Antarctic Weddell Sea Weddell |
geographic_facet |
Antarctic Southern Ocean The Antarctic Weddell Sea Weddell |
genre |
Antarc* Antarctic Antarctic Krill Antarctica antartic* Euphausia superba ice algae Neogloboquadrina pachyderma Sea ice Southern Ocean Weddell Sea |
genre_facet |
Antarc* Antarctic Antarctic Krill Antarctica antartic* Euphausia superba ice algae Neogloboquadrina pachyderma Sea ice Southern Ocean Weddell Sea |
op_source |
Brierley , A S & Thomas , DN 2002 , ' Ecology of Southern Ocean pack ice ' , Advances in Marine Biology , vol. 43 , pp. 171-276 . https://doi.org/10.1016/S0065-2881(02)43005-2 |
op_rights |
info:eu-repo/semantics/restrictedAccess |
op_doi |
https://doi.org/10.1016/S0065-2881(02)43005-2 |
container_start_page |
171 |
op_container_end_page |
IN4 |
_version_ |
1766231813633605632 |