Aquatic primary production in the Antarctic

A review is presented of studies, including recent work by members of the British Antarctic Survey, on the primary productivity of plankton, ice-flora and benthos in both marine and freshwater habitats in the Antarctic. Those members of the flora so far studied have low compensation points enabling...

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Published in:Philosophical Transactions of the Royal Society of London. B, Biological Sciences
Format: Article in Journal/Newspaper
Language:English
Published: The Royal Society 1977
Subjects:
Online Access:http://dx.doi.org/10.1098/rstb.1977.0069
https://royalsocietypublishing.org/doi/pdf/10.1098/rstb.1977.0069
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spelling crroyalsociety:10.1098/rstb.1977.0069 2024-06-02T07:57:55+00:00 Aquatic primary production in the Antarctic 1977 http://dx.doi.org/10.1098/rstb.1977.0069 https://royalsocietypublishing.org/doi/pdf/10.1098/rstb.1977.0069 en eng The Royal Society https://royalsociety.org/journals/ethics-policies/data-sharing-mining/ Philosophical Transactions of the Royal Society of London. B, Biological Sciences volume 279, issue 963, page 27-38 ISSN 0080-4622 2054-0280 journal-article 1977 crroyalsociety https://doi.org/10.1098/rstb.1977.0069 2024-05-07T14:16:42Z A review is presented of studies, including recent work by members of the British Antarctic Survey, on the primary productivity of plankton, ice-flora and benthos in both marine and freshwater habitats in the Antarctic. Those members of the flora so far studied have low compensation points enabling slow growth in low light intensities but otherwise show no apparent adaptation to temperatures around freezing point. Certain sea areas, mostly inshore, have dense standing crops with daily and annual productivities as high as those of productive areas elsewhere in the oceans but in the open Southern Ocean productivity seems generally low even although nutrient concentrations are high, probably because of excessive turbulence carrying plankton out of the photic zone. There is as yet insufficient data to show whether, as a whole, the photosynthetic efficiency of the Southern Ocean is greater or less than that of other sea areas. Antarctic algae liberate extracellular products of photosynthesis but there is no definite evidence that these are reassimilated to support growth when light intensities are low and it may be that this material, carried by currents, supports heterotrophic production in other parts of the ocean. Comparison of data for adjacent marine and freshwater systems shows that their rates of primary production are much the same but the marine phytoplankton shows characteristics of shade-adapted cells consistent with the greater turbulence to which it is exposed. Article in Journal/Newspaper Antarc* Antarctic British Antarctic Survey Southern Ocean The Royal Society Antarctic Southern Ocean The Antarctic Philosophical Transactions of the Royal Society of London. B, Biological Sciences 279 963 27 38
institution Open Polar
collection The Royal Society
op_collection_id crroyalsociety
language English
description A review is presented of studies, including recent work by members of the British Antarctic Survey, on the primary productivity of plankton, ice-flora and benthos in both marine and freshwater habitats in the Antarctic. Those members of the flora so far studied have low compensation points enabling slow growth in low light intensities but otherwise show no apparent adaptation to temperatures around freezing point. Certain sea areas, mostly inshore, have dense standing crops with daily and annual productivities as high as those of productive areas elsewhere in the oceans but in the open Southern Ocean productivity seems generally low even although nutrient concentrations are high, probably because of excessive turbulence carrying plankton out of the photic zone. There is as yet insufficient data to show whether, as a whole, the photosynthetic efficiency of the Southern Ocean is greater or less than that of other sea areas. Antarctic algae liberate extracellular products of photosynthesis but there is no definite evidence that these are reassimilated to support growth when light intensities are low and it may be that this material, carried by currents, supports heterotrophic production in other parts of the ocean. Comparison of data for adjacent marine and freshwater systems shows that their rates of primary production are much the same but the marine phytoplankton shows characteristics of shade-adapted cells consistent with the greater turbulence to which it is exposed.
format Article in Journal/Newspaper
title Aquatic primary production in the Antarctic
spellingShingle Aquatic primary production in the Antarctic
title_short Aquatic primary production in the Antarctic
title_full Aquatic primary production in the Antarctic
title_fullStr Aquatic primary production in the Antarctic
title_full_unstemmed Aquatic primary production in the Antarctic
title_sort aquatic primary production in the antarctic
publisher The Royal Society
publishDate 1977
url http://dx.doi.org/10.1098/rstb.1977.0069
https://royalsocietypublishing.org/doi/pdf/10.1098/rstb.1977.0069
geographic Antarctic
Southern Ocean
The Antarctic
geographic_facet Antarctic
Southern Ocean
The Antarctic
genre Antarc*
Antarctic
British Antarctic Survey
Southern Ocean
genre_facet Antarc*
Antarctic
British Antarctic Survey
Southern Ocean
op_source Philosophical Transactions of the Royal Society of London. B, Biological Sciences
volume 279, issue 963, page 27-38
ISSN 0080-4622 2054-0280
op_rights https://royalsociety.org/journals/ethics-policies/data-sharing-mining/
op_doi https://doi.org/10.1098/rstb.1977.0069
container_title Philosophical Transactions of the Royal Society of London. B, Biological Sciences
container_volume 279
container_issue 963
container_start_page 27
op_container_end_page 38
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