Planktonic foraminiferal flux seasonality in Subantarctic sediment traps: A test for paleoclimate reconstructions
Sediment trap moorings deployed during 1997 and 1998 in the Subantarctic to Polar Frontal regions of theSouthern Ocean reveal distinct seasonality in foraminiferal flux. Foraminiferal assemblages vary between eachsite, yet major species exhibit very similar patterns of seasonal succession which can...
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American Geophysical Union
2003
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Online Access: | http://www.agu.org/ https://doi.org/10.1029/2002PA000839 http://ecite.utas.edu.au/56323 |
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ftunivtasecite:oai:ecite.utas.edu.au:56323 2023-05-15T18:25:19+02:00 Planktonic foraminiferal flux seasonality in Subantarctic sediment traps: A test for paleoclimate reconstructions King, AL Howard, W 2003 application/pdf http://www.agu.org/ https://doi.org/10.1029/2002PA000839 http://ecite.utas.edu.au/56323 en eng American Geophysical Union http://ecite.utas.edu.au/56323/2/King&Howard_PA_03[2].pdf http://dx.doi.org/10.1029/2002PA000839 King, AL and Howard, W, Planktonic foraminiferal flux seasonality in Subantarctic sediment traps: A test for paleoclimate reconstructions, Paleoceanography, 18, (1) pp. 1019. ISSN 0883-8305 (2003) [Refereed Article] http://ecite.utas.edu.au/56323 Earth Sciences Atmospheric Sciences Climate Change Processes Refereed Article PeerReviewed 2003 ftunivtasecite https://doi.org/10.1029/2002PA000839 2019-12-13T21:28:39Z Sediment trap moorings deployed during 1997 and 1998 in the Subantarctic to Polar Frontal regions of theSouthern Ocean reveal distinct seasonality in foraminiferal flux. Foraminiferal assemblages vary between eachsite, yet major species exhibit very similar patterns of seasonal succession which can be associated with changesin mixed layer depth. Enhanced foraminiferal productivity is also associated with periods of high biogenic silicaand particulate organic carbon flux. On a broader scale, foraminiferal assemblages are strongly delineated bytemperature. Temperature estimates derived from the assemblages using the modern analog technique (MAT) aremostly within 2.5 C of the satellite advanced very high resolution radiometer temperatures observed during thedeployment period. This indicates that core top sediments included in the MAT database do reflect modernobserved conditions at the sea surface, providing a robust technique for estimating past temperature change fromforaminiferal assemblages in Southern Ocean environments. Article in Journal/Newspaper Southern Ocean eCite UTAS (University of Tasmania) Southern Ocean Paleoceanography 18 1 n/a n/a |
institution |
Open Polar |
collection |
eCite UTAS (University of Tasmania) |
op_collection_id |
ftunivtasecite |
language |
English |
topic |
Earth Sciences Atmospheric Sciences Climate Change Processes |
spellingShingle |
Earth Sciences Atmospheric Sciences Climate Change Processes King, AL Howard, W Planktonic foraminiferal flux seasonality in Subantarctic sediment traps: A test for paleoclimate reconstructions |
topic_facet |
Earth Sciences Atmospheric Sciences Climate Change Processes |
description |
Sediment trap moorings deployed during 1997 and 1998 in the Subantarctic to Polar Frontal regions of theSouthern Ocean reveal distinct seasonality in foraminiferal flux. Foraminiferal assemblages vary between eachsite, yet major species exhibit very similar patterns of seasonal succession which can be associated with changesin mixed layer depth. Enhanced foraminiferal productivity is also associated with periods of high biogenic silicaand particulate organic carbon flux. On a broader scale, foraminiferal assemblages are strongly delineated bytemperature. Temperature estimates derived from the assemblages using the modern analog technique (MAT) aremostly within 2.5 C of the satellite advanced very high resolution radiometer temperatures observed during thedeployment period. This indicates that core top sediments included in the MAT database do reflect modernobserved conditions at the sea surface, providing a robust technique for estimating past temperature change fromforaminiferal assemblages in Southern Ocean environments. |
format |
Article in Journal/Newspaper |
author |
King, AL Howard, W |
author_facet |
King, AL Howard, W |
author_sort |
King, AL |
title |
Planktonic foraminiferal flux seasonality in Subantarctic sediment traps: A test for paleoclimate reconstructions |
title_short |
Planktonic foraminiferal flux seasonality in Subantarctic sediment traps: A test for paleoclimate reconstructions |
title_full |
Planktonic foraminiferal flux seasonality in Subantarctic sediment traps: A test for paleoclimate reconstructions |
title_fullStr |
Planktonic foraminiferal flux seasonality in Subantarctic sediment traps: A test for paleoclimate reconstructions |
title_full_unstemmed |
Planktonic foraminiferal flux seasonality in Subantarctic sediment traps: A test for paleoclimate reconstructions |
title_sort |
planktonic foraminiferal flux seasonality in subantarctic sediment traps: a test for paleoclimate reconstructions |
publisher |
American Geophysical Union |
publishDate |
2003 |
url |
http://www.agu.org/ https://doi.org/10.1029/2002PA000839 http://ecite.utas.edu.au/56323 |
geographic |
Southern Ocean |
geographic_facet |
Southern Ocean |
genre |
Southern Ocean |
genre_facet |
Southern Ocean |
op_relation |
http://ecite.utas.edu.au/56323/2/King&Howard_PA_03[2].pdf http://dx.doi.org/10.1029/2002PA000839 King, AL and Howard, W, Planktonic foraminiferal flux seasonality in Subantarctic sediment traps: A test for paleoclimate reconstructions, Paleoceanography, 18, (1) pp. 1019. ISSN 0883-8305 (2003) [Refereed Article] http://ecite.utas.edu.au/56323 |
op_doi |
https://doi.org/10.1029/2002PA000839 |
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Paleoceanography |
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18 |
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1 |
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1766206683491598336 |