Phytoplankton pigments at the Weddell-Scotia confluence during the 1993 austral spring
During a 1993 austral spring cruise, a complex biomass was encountered near South Orkney Island that ranged from a low-biomass, Chaetoceros tortissimus assemblage south of the front towards the ice edge, to a high-biomass, Thalassiosira gravida -dominated assemblage at the northern edge. The maximum...
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2000
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fthighwire:oai:open-archive.highwire.org:plankt:22/10/1989 2023-05-15T18:25:40+02:00 Phytoplankton pigments at the Weddell-Scotia confluence during the 1993 austral spring Sigleo, A.C. Neale, P.J. Spector, A.M. 2000-10-01 00:00:00.0 text/html http://plankt.oxfordjournals.org/cgi/content/short/22/10/1989 https://doi.org/10.1093/plankt/22.10.1989 en eng Oxford University Press http://plankt.oxfordjournals.org/cgi/content/short/22/10/1989 http://dx.doi.org/10.1093/plankt/22.10.1989 Copyright (C) 2000, Oxford University Press ORIGINAL ARTICLES TEXT 2000 fthighwire https://doi.org/10.1093/plankt/22.10.1989 2016-11-16T18:12:51Z During a 1993 austral spring cruise, a complex biomass was encountered near South Orkney Island that ranged from a low-biomass, Chaetoceros tortissimus assemblage south of the front towards the ice edge, to a high-biomass, Thalassiosira gravida -dominated assemblage at the northern edge. The maximum levels of chlorophyll (Chl) a (up to 6 mg m–3) were higher than those observed in previous high-performance liquid chromatography-based studies of pigments in the pelagic Southern Ocean. The non-photosynthetic pigment chlorophyllide a comprised up to 75% of the chlorophyllous pigments in the southern assemblage, but < 5% in the northern assemblage. Concentrations of the xanthophylls diadinoxanthin (DD) and diatoxanthin (DT), used as indicators of mean irradiance, indicated low-light-adapted populations. Low-light DD + DT/Chl a ratios in surface waters indicated that vertical mixing limited phytoplankton residence time in the near-surface layer, and thus limited exposure to maximum irradiance. Deck incubations of natural assemblages indicated that the dark epoxidation reaction (i.e. the return of DT to DD) was a two-step reaction with the initial rate being more rapid ( t 1/2 = 9.5 min) than the second ( t 1/2 = 55 min). Fucoxanthin, a major diatom pigment, was more stable chemically in the water column than Chl a , and the vertical profiles of fucoxanthin followed those of chlorophyllide a in some cases. The formation and apparent stability of chlorophyllide a and fucoxanthin are important considerations when estimating photosynthetically active biomass over large regions of the ocean. Text Southern Ocean HighWire Press (Stanford University) Southern Ocean Austral Weddell Journal of Plankton Research 22 10 1989 2006 |
institution |
Open Polar |
collection |
HighWire Press (Stanford University) |
op_collection_id |
fthighwire |
language |
English |
topic |
ORIGINAL ARTICLES |
spellingShingle |
ORIGINAL ARTICLES Sigleo, A.C. Neale, P.J. Spector, A.M. Phytoplankton pigments at the Weddell-Scotia confluence during the 1993 austral spring |
topic_facet |
ORIGINAL ARTICLES |
description |
During a 1993 austral spring cruise, a complex biomass was encountered near South Orkney Island that ranged from a low-biomass, Chaetoceros tortissimus assemblage south of the front towards the ice edge, to a high-biomass, Thalassiosira gravida -dominated assemblage at the northern edge. The maximum levels of chlorophyll (Chl) a (up to 6 mg m–3) were higher than those observed in previous high-performance liquid chromatography-based studies of pigments in the pelagic Southern Ocean. The non-photosynthetic pigment chlorophyllide a comprised up to 75% of the chlorophyllous pigments in the southern assemblage, but < 5% in the northern assemblage. Concentrations of the xanthophylls diadinoxanthin (DD) and diatoxanthin (DT), used as indicators of mean irradiance, indicated low-light-adapted populations. Low-light DD + DT/Chl a ratios in surface waters indicated that vertical mixing limited phytoplankton residence time in the near-surface layer, and thus limited exposure to maximum irradiance. Deck incubations of natural assemblages indicated that the dark epoxidation reaction (i.e. the return of DT to DD) was a two-step reaction with the initial rate being more rapid ( t 1/2 = 9.5 min) than the second ( t 1/2 = 55 min). Fucoxanthin, a major diatom pigment, was more stable chemically in the water column than Chl a , and the vertical profiles of fucoxanthin followed those of chlorophyllide a in some cases. The formation and apparent stability of chlorophyllide a and fucoxanthin are important considerations when estimating photosynthetically active biomass over large regions of the ocean. |
format |
Text |
author |
Sigleo, A.C. Neale, P.J. Spector, A.M. |
author_facet |
Sigleo, A.C. Neale, P.J. Spector, A.M. |
author_sort |
Sigleo, A.C. |
title |
Phytoplankton pigments at the Weddell-Scotia confluence during the 1993 austral spring |
title_short |
Phytoplankton pigments at the Weddell-Scotia confluence during the 1993 austral spring |
title_full |
Phytoplankton pigments at the Weddell-Scotia confluence during the 1993 austral spring |
title_fullStr |
Phytoplankton pigments at the Weddell-Scotia confluence during the 1993 austral spring |
title_full_unstemmed |
Phytoplankton pigments at the Weddell-Scotia confluence during the 1993 austral spring |
title_sort |
phytoplankton pigments at the weddell-scotia confluence during the 1993 austral spring |
publisher |
Oxford University Press |
publishDate |
2000 |
url |
http://plankt.oxfordjournals.org/cgi/content/short/22/10/1989 https://doi.org/10.1093/plankt/22.10.1989 |
geographic |
Southern Ocean Austral Weddell |
geographic_facet |
Southern Ocean Austral Weddell |
genre |
Southern Ocean |
genre_facet |
Southern Ocean |
op_relation |
http://plankt.oxfordjournals.org/cgi/content/short/22/10/1989 http://dx.doi.org/10.1093/plankt/22.10.1989 |
op_rights |
Copyright (C) 2000, Oxford University Press |
op_doi |
https://doi.org/10.1093/plankt/22.10.1989 |
container_title |
Journal of Plankton Research |
container_volume |
22 |
container_issue |
10 |
container_start_page |
1989 |
op_container_end_page |
2006 |
_version_ |
1766207254842834944 |