Figure 2. Barium excess of sediment core PS1506-1 ...

Over the last decade many regional palaeoceanographic studies have found evidence for enhanced primary productivity during glacial episodes, particularly in the equatorial Pacific and off northwest Africa. These studies have given rise to the "glacial productivity hypothesis" which has sug...

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Bibliographic Details
Main Authors: Shimmield, Graham, Derrick, S, Mackensen, Andreas, Grobe, Hannes, Pudsey, Carol J
Format: Dataset
Language:English
Published: PANGAEA 2009
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.730146
https://doi.pangaea.de/10.1594/PANGAEA.730146
id ftdatacite:10.1594/pangaea.730146
record_format openpolar
spelling ftdatacite:10.1594/pangaea.730146 2024-09-15T17:47:51+00:00 Figure 2. Barium excess of sediment core PS1506-1 ... Shimmield, Graham Derrick, S Mackensen, Andreas Grobe, Hannes Pudsey, Carol J 2009 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.730146 https://doi.pangaea.de/10.1594/PANGAEA.730146 en eng PANGAEA https://dx.doi.org/10.1007/978-3-642-78737-9_24 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 DEPTH, sediment/rock Barium excess Gravity corer Kiel type X-ray fluorescence XRF ANT-V/4 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Dataset dataset Supplementary Dataset 2009 ftdatacite https://doi.org/10.1594/pangaea.73014610.1007/978-3-642-78737-9_24 2024-07-03T13:10:33Z Over the last decade many regional palaeoceanographic studies have found evidence for enhanced primary productivity during glacial episodes, particularly in the equatorial Pacific and off northwest Africa. These studies have given rise to the "glacial productivity hypothesis" which has suggested that enhanced oceanic biomass during glacial times supported an efficient removal of organic carbon from the euphotic zone, contributing to lower atmospheric CO2 levels recorded in ice cores. Recently, studies from the Southern Ocean have shown that south of the Antarctic Polar Front glacial palaeoproductivity was lower than during interglacial times. Here we present further evidence for enhanced interglacial productivity in the Southern Ocean using a transect of cores collected from the Scotia Sea and Weddell Sea. Biogenic silica, organic carbon and barium are presented as proxy indicators of past productivity. In order to establish such palaeoproductivity records for this region, where an absence of foraminifera ... : Data are retrodigitized from graf. ... Dataset Antarc* Antarctic Scotia Sea Southern Ocean Weddell Sea DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic DEPTH, sediment/rock
Barium excess
Gravity corer Kiel type
X-ray fluorescence XRF
ANT-V/4
Polarstern
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
spellingShingle DEPTH, sediment/rock
Barium excess
Gravity corer Kiel type
X-ray fluorescence XRF
ANT-V/4
Polarstern
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
Shimmield, Graham
Derrick, S
Mackensen, Andreas
Grobe, Hannes
Pudsey, Carol J
Figure 2. Barium excess of sediment core PS1506-1 ...
topic_facet DEPTH, sediment/rock
Barium excess
Gravity corer Kiel type
X-ray fluorescence XRF
ANT-V/4
Polarstern
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
description Over the last decade many regional palaeoceanographic studies have found evidence for enhanced primary productivity during glacial episodes, particularly in the equatorial Pacific and off northwest Africa. These studies have given rise to the "glacial productivity hypothesis" which has suggested that enhanced oceanic biomass during glacial times supported an efficient removal of organic carbon from the euphotic zone, contributing to lower atmospheric CO2 levels recorded in ice cores. Recently, studies from the Southern Ocean have shown that south of the Antarctic Polar Front glacial palaeoproductivity was lower than during interglacial times. Here we present further evidence for enhanced interglacial productivity in the Southern Ocean using a transect of cores collected from the Scotia Sea and Weddell Sea. Biogenic silica, organic carbon and barium are presented as proxy indicators of past productivity. In order to establish such palaeoproductivity records for this region, where an absence of foraminifera ... : Data are retrodigitized from graf. ...
format Dataset
author Shimmield, Graham
Derrick, S
Mackensen, Andreas
Grobe, Hannes
Pudsey, Carol J
author_facet Shimmield, Graham
Derrick, S
Mackensen, Andreas
Grobe, Hannes
Pudsey, Carol J
author_sort Shimmield, Graham
title Figure 2. Barium excess of sediment core PS1506-1 ...
title_short Figure 2. Barium excess of sediment core PS1506-1 ...
title_full Figure 2. Barium excess of sediment core PS1506-1 ...
title_fullStr Figure 2. Barium excess of sediment core PS1506-1 ...
title_full_unstemmed Figure 2. Barium excess of sediment core PS1506-1 ...
title_sort figure 2. barium excess of sediment core ps1506-1 ...
publisher PANGAEA
publishDate 2009
url https://dx.doi.org/10.1594/pangaea.730146
https://doi.pangaea.de/10.1594/PANGAEA.730146
genre Antarc*
Antarctic
Scotia Sea
Southern Ocean
Weddell Sea
genre_facet Antarc*
Antarctic
Scotia Sea
Southern Ocean
Weddell Sea
op_relation https://dx.doi.org/10.1007/978-3-642-78737-9_24
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.73014610.1007/978-3-642-78737-9_24
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