The Southern Ocean benthic fauna and climate change: a historical perspective

Environmental change is the norm and it is likely that, particularly on the geological timescale, the temperature regime experienced by marine organisms has never been stable. These temperature changes vary in timescale from daily, through seasonal variations, to long-term environmental change over...

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Published in:Philosophical Transactions of the Royal Society of London. Series B: Biological Sciences
Format: Article in Journal/Newspaper
Language:English
Published: The Royal Society 1992
Subjects:
Online Access:http://dx.doi.org/10.1098/rstb.1992.0150
https://royalsocietypublishing.org/doi/pdf/10.1098/rstb.1992.0150
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spelling crroyalsociety:10.1098/rstb.1992.0150 2024-06-23T07:45:48+00:00 The Southern Ocean benthic fauna and climate change: a historical perspective 1992 http://dx.doi.org/10.1098/rstb.1992.0150 https://royalsocietypublishing.org/doi/pdf/10.1098/rstb.1992.0150 en eng The Royal Society https://royalsociety.org/journals/ethics-policies/data-sharing-mining/ Philosophical Transactions of the Royal Society of London. Series B: Biological Sciences volume 338, issue 1285, page 299-309 ISSN 0962-8436 1471-2970 journal-article 1992 crroyalsociety https://doi.org/10.1098/rstb.1992.0150 2024-06-10T04:15:14Z Environmental change is the norm and it is likely that, particularly on the geological timescale, the temperature regime experienced by marine organisms has never been stable. These temperature changes vary in timescale from daily, through seasonal variations, to long-term environmental change over tens of millions of years. Whereas physiological work can give information on how individual organisms may react phenotypically to short-term change, the way benthic communities react to long-term change can only be studied from the fossil record. The present benthic marine fauna of the Southern Ocean is rich and diverse, consisting of a mixture of taxa with differing evolutionary histories and biogeographical affinities, suggesting that at no time in the Cenozoic did continental ice sheets extend sufficiently to eradicate all shallow-water faunas around Antarctica at the same time. Nevertheless, certain features do suggest the operation of vicariant processes, and climatic cycles affecting distributional ranges and ice-sheet extension may both have enhanced speciation processes. The overall cooling of southern high-latitude seas since the mid-Eocene has been neither smooth nor steady. Intermittent periods of global warming and the influence of Milankovitch cyclicity is likely to have led to regular pulses of migration in and out of Antarctica. The resultant diversity pump may explain in part the high species richness of some marine taxa in the Southern Ocean. It is difficult to suggest how the existing fauna will react to present global warming. Although it is certain the fauna will change, as all faunas have done throughout evolutionary time, we cannot predict with confidence how it will do so. Article in Journal/Newspaper Antarc* Antarctica Ice Sheet Southern Ocean The Royal Society Southern Ocean Philosophical Transactions of the Royal Society of London. Series B: Biological Sciences 338 1285 299 309
institution Open Polar
collection The Royal Society
op_collection_id crroyalsociety
language English
description Environmental change is the norm and it is likely that, particularly on the geological timescale, the temperature regime experienced by marine organisms has never been stable. These temperature changes vary in timescale from daily, through seasonal variations, to long-term environmental change over tens of millions of years. Whereas physiological work can give information on how individual organisms may react phenotypically to short-term change, the way benthic communities react to long-term change can only be studied from the fossil record. The present benthic marine fauna of the Southern Ocean is rich and diverse, consisting of a mixture of taxa with differing evolutionary histories and biogeographical affinities, suggesting that at no time in the Cenozoic did continental ice sheets extend sufficiently to eradicate all shallow-water faunas around Antarctica at the same time. Nevertheless, certain features do suggest the operation of vicariant processes, and climatic cycles affecting distributional ranges and ice-sheet extension may both have enhanced speciation processes. The overall cooling of southern high-latitude seas since the mid-Eocene has been neither smooth nor steady. Intermittent periods of global warming and the influence of Milankovitch cyclicity is likely to have led to regular pulses of migration in and out of Antarctica. The resultant diversity pump may explain in part the high species richness of some marine taxa in the Southern Ocean. It is difficult to suggest how the existing fauna will react to present global warming. Although it is certain the fauna will change, as all faunas have done throughout evolutionary time, we cannot predict with confidence how it will do so.
format Article in Journal/Newspaper
title The Southern Ocean benthic fauna and climate change: a historical perspective
spellingShingle The Southern Ocean benthic fauna and climate change: a historical perspective
title_short The Southern Ocean benthic fauna and climate change: a historical perspective
title_full The Southern Ocean benthic fauna and climate change: a historical perspective
title_fullStr The Southern Ocean benthic fauna and climate change: a historical perspective
title_full_unstemmed The Southern Ocean benthic fauna and climate change: a historical perspective
title_sort southern ocean benthic fauna and climate change: a historical perspective
publisher The Royal Society
publishDate 1992
url http://dx.doi.org/10.1098/rstb.1992.0150
https://royalsocietypublishing.org/doi/pdf/10.1098/rstb.1992.0150
geographic Southern Ocean
geographic_facet Southern Ocean
genre Antarc*
Antarctica
Ice Sheet
Southern Ocean
genre_facet Antarc*
Antarctica
Ice Sheet
Southern Ocean
op_source Philosophical Transactions of the Royal Society of London. Series B: Biological Sciences
volume 338, issue 1285, page 299-309
ISSN 0962-8436 1471-2970
op_rights https://royalsociety.org/journals/ethics-policies/data-sharing-mining/
op_doi https://doi.org/10.1098/rstb.1992.0150
container_title Philosophical Transactions of the Royal Society of London. Series B: Biological Sciences
container_volume 338
container_issue 1285
container_start_page 299
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