In situ pore water oxygen microprofiles from the Polar Front, Southern South Atlantic Ocean ...
Without doubt, global climate change is directly linked to the anthropogenic release of greenhouse gases such as carbon dioxide (CO2) and methane (UN IPCC-Report 2007). Therefore, research efforts to comprehend the global carbon cycle have increased during the last years. In the context of the obser...
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ftdatacite:10.1594/pangaea.660529 2024-09-15T17:41:39+00:00 In situ pore water oxygen microprofiles from the Polar Front, Southern South Atlantic Ocean ... Sachs, Oliver Sauter, Eberhard-Jürgen 2007 application/zip https://dx.doi.org/10.1594/pangaea.660529 https://doi.pangaea.de/10.1594/PANGAEA.660529 en eng PANGAEA Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Bottom lander MultiCorer ANT-XXI/4 Polarstern Biological Oceanography @ AWI AWI_BioOce Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158 article Collection Publication Series of Datasets 2007 ftdatacite https://doi.org/10.1594/pangaea.660529 2024-07-03T13:10:16Z Without doubt, global climate change is directly linked to the anthropogenic release of greenhouse gases such as carbon dioxide (CO2) and methane (UN IPCC-Report 2007). Therefore, research efforts to comprehend the global carbon cycle have increased during the last years. In the context of the observed changes, it is of particular interest to decipher the role of the hydro-, bio- and atmospheres and how the different compartments of the earth system are affected by the increase of atmospheric CO2. Due to its huge carbon inventory, the marine carbon cycle represents the most important component in this respect. Numerous findings suggest that the Southern Ocean plays a key role in terms of oceanic CO2 uptake. However, an exact quantification of such fluxes of material is hard to achieve for large areas, not least on account of the inaccessibility of this remote region. In particular, there exist so far only few accurate data for benthic carbon fluxes. The latter can be derived from high resolution pore water ... Article in Journal/Newspaper Antarc* Antarctic Climate change Sea ice South Atlantic Ocean Southern Ocean DataCite |
institution |
Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Bottom lander MultiCorer ANT-XXI/4 Polarstern Biological Oceanography @ AWI AWI_BioOce Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158 |
spellingShingle |
Bottom lander MultiCorer ANT-XXI/4 Polarstern Biological Oceanography @ AWI AWI_BioOce Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158 Sachs, Oliver Sauter, Eberhard-Jürgen In situ pore water oxygen microprofiles from the Polar Front, Southern South Atlantic Ocean ... |
topic_facet |
Bottom lander MultiCorer ANT-XXI/4 Polarstern Biological Oceanography @ AWI AWI_BioOce Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158 |
description |
Without doubt, global climate change is directly linked to the anthropogenic release of greenhouse gases such as carbon dioxide (CO2) and methane (UN IPCC-Report 2007). Therefore, research efforts to comprehend the global carbon cycle have increased during the last years. In the context of the observed changes, it is of particular interest to decipher the role of the hydro-, bio- and atmospheres and how the different compartments of the earth system are affected by the increase of atmospheric CO2. Due to its huge carbon inventory, the marine carbon cycle represents the most important component in this respect. Numerous findings suggest that the Southern Ocean plays a key role in terms of oceanic CO2 uptake. However, an exact quantification of such fluxes of material is hard to achieve for large areas, not least on account of the inaccessibility of this remote region. In particular, there exist so far only few accurate data for benthic carbon fluxes. The latter can be derived from high resolution pore water ... |
format |
Article in Journal/Newspaper |
author |
Sachs, Oliver Sauter, Eberhard-Jürgen |
author_facet |
Sachs, Oliver Sauter, Eberhard-Jürgen |
author_sort |
Sachs, Oliver |
title |
In situ pore water oxygen microprofiles from the Polar Front, Southern South Atlantic Ocean ... |
title_short |
In situ pore water oxygen microprofiles from the Polar Front, Southern South Atlantic Ocean ... |
title_full |
In situ pore water oxygen microprofiles from the Polar Front, Southern South Atlantic Ocean ... |
title_fullStr |
In situ pore water oxygen microprofiles from the Polar Front, Southern South Atlantic Ocean ... |
title_full_unstemmed |
In situ pore water oxygen microprofiles from the Polar Front, Southern South Atlantic Ocean ... |
title_sort |
in situ pore water oxygen microprofiles from the polar front, southern south atlantic ocean ... |
publisher |
PANGAEA |
publishDate |
2007 |
url |
https://dx.doi.org/10.1594/pangaea.660529 https://doi.pangaea.de/10.1594/PANGAEA.660529 |
genre |
Antarc* Antarctic Climate change Sea ice South Atlantic Ocean Southern Ocean |
genre_facet |
Antarc* Antarctic Climate change Sea ice South Atlantic Ocean Southern Ocean |
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.660529 |
_version_ |
1810487881250111488 |