id ftdatacite:10.1594/pangaea.761833
record_format openpolar
spelling ftdatacite:10.1594/pangaea.761833 2024-09-15T18:37:21+00:00 Hydrochemistry measured on water bottle samples during POLARSTERN cruise ANT-VIII/2 ... Mackensen, Andreas Hubberten, Hans-Wolfgang Scheele, Norbert Schlitzer, Reiner 1996 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.761833 https://doi.pangaea.de/10.1594/PANGAEA.761833 en eng PANGAEA https://dx.doi.org/10.1029/95pa03840 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Event label Date/Time of event Latitude of event Longitude of event Elevation of event DEPTH, water Pressure, water Temperature, water, potential Salinity Oxygen δ13C, dissolved inorganic carbon δ18O, water Δδ13C Phosphate Multiple investigations MultiCorer CTD/Rosette Water sample CTD, Neil Brown, Mark III B Oxygen, Winkler Culberson, 1991, WOCE Report 68/91 Mass spectrometer Finnigan MAT 252 Mass spectrometer Finnigan Delta-S Calculated after Broecker & Maier-Reimer 1992 Continuous Flow Analysis ANT-VIII/2 ANT-VIII/3 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo South Atlantic in Late Quaternary Reconstruction of Budget and Currents SFB261 Dataset dataset Supplementary Dataset 1996 ftdatacite https://doi.org/10.1594/pangaea.76183310.1029/95pa03840 2024-07-03T13:10:33Z On a section between 72°S and 42°S and a transect between 60°E and 10°E through the Weddell Sea and the southernmost eastern Atlantic Ocean, the water column was sampled on 72 stations, and the stable carbon isotopic composition of total dissolved inorganic carbon (delta13C(SumCO2)) as well as the stable oxygen isotopic composition of seawater (delta18O) was determined. These data were compared with potential temperature, salinity, dissolved oxygen and phosphate data from the same stations. The observed delta13C(SumCO2)/PO4[3-] relationship in the deep Weddell Sea strongly differs from the global Redfield-driven deep water relationship. We attribute this to enhanced thermodynamic fractionation at sites of bottom water formation that decouples the nutrient signal from the delta13C(SumCO2) signal not only in surface and intermediate water masses but also in deep and bottom water. Different, water-mass specific thermodynamic imprints due to different modes of bottom water formation are assumed to cause the ... : Supplement to: Mackensen, Andreas; Hubberten, Hans-Wolfgang; Scheele, Norbert; Schlitzer, Reiner (1996): Decoupling of d13CSUMCO2 and phosphate in recent Weddell Sea deep and bottom water: implications for glacial Southern Ocean paleoceanography. Paleoceanography, 11(2), 203-215 ... Dataset Southern Ocean Weddell Sea DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Event label
Date/Time of event
Latitude of event
Longitude of event
Elevation of event
DEPTH, water
Pressure, water
Temperature, water, potential
Salinity
Oxygen
δ13C, dissolved inorganic carbon
δ18O, water
Δδ13C
Phosphate
Multiple investigations
MultiCorer
CTD/Rosette
Water sample
CTD, Neil Brown, Mark III B
Oxygen, Winkler Culberson, 1991, WOCE Report 68/91
Mass spectrometer Finnigan MAT 252
Mass spectrometer Finnigan Delta-S
Calculated after Broecker & Maier-Reimer 1992
Continuous Flow Analysis
ANT-VIII/2
ANT-VIII/3
Polarstern
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
South Atlantic in Late Quaternary Reconstruction of Budget and Currents SFB261
spellingShingle Event label
Date/Time of event
Latitude of event
Longitude of event
Elevation of event
DEPTH, water
Pressure, water
Temperature, water, potential
Salinity
Oxygen
δ13C, dissolved inorganic carbon
δ18O, water
Δδ13C
Phosphate
Multiple investigations
MultiCorer
CTD/Rosette
Water sample
CTD, Neil Brown, Mark III B
Oxygen, Winkler Culberson, 1991, WOCE Report 68/91
Mass spectrometer Finnigan MAT 252
Mass spectrometer Finnigan Delta-S
Calculated after Broecker & Maier-Reimer 1992
Continuous Flow Analysis
ANT-VIII/2
ANT-VIII/3
Polarstern
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
South Atlantic in Late Quaternary Reconstruction of Budget and Currents SFB261
Mackensen, Andreas
Hubberten, Hans-Wolfgang
Scheele, Norbert
Schlitzer, Reiner
Hydrochemistry measured on water bottle samples during POLARSTERN cruise ANT-VIII/2 ...
topic_facet Event label
Date/Time of event
Latitude of event
Longitude of event
Elevation of event
DEPTH, water
Pressure, water
Temperature, water, potential
Salinity
Oxygen
δ13C, dissolved inorganic carbon
δ18O, water
Δδ13C
Phosphate
Multiple investigations
MultiCorer
CTD/Rosette
Water sample
CTD, Neil Brown, Mark III B
Oxygen, Winkler Culberson, 1991, WOCE Report 68/91
Mass spectrometer Finnigan MAT 252
Mass spectrometer Finnigan Delta-S
Calculated after Broecker & Maier-Reimer 1992
Continuous Flow Analysis
ANT-VIII/2
ANT-VIII/3
Polarstern
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
South Atlantic in Late Quaternary Reconstruction of Budget and Currents SFB261
description On a section between 72°S and 42°S and a transect between 60°E and 10°E through the Weddell Sea and the southernmost eastern Atlantic Ocean, the water column was sampled on 72 stations, and the stable carbon isotopic composition of total dissolved inorganic carbon (delta13C(SumCO2)) as well as the stable oxygen isotopic composition of seawater (delta18O) was determined. These data were compared with potential temperature, salinity, dissolved oxygen and phosphate data from the same stations. The observed delta13C(SumCO2)/PO4[3-] relationship in the deep Weddell Sea strongly differs from the global Redfield-driven deep water relationship. We attribute this to enhanced thermodynamic fractionation at sites of bottom water formation that decouples the nutrient signal from the delta13C(SumCO2) signal not only in surface and intermediate water masses but also in deep and bottom water. Different, water-mass specific thermodynamic imprints due to different modes of bottom water formation are assumed to cause the ... : Supplement to: Mackensen, Andreas; Hubberten, Hans-Wolfgang; Scheele, Norbert; Schlitzer, Reiner (1996): Decoupling of d13CSUMCO2 and phosphate in recent Weddell Sea deep and bottom water: implications for glacial Southern Ocean paleoceanography. Paleoceanography, 11(2), 203-215 ...
format Dataset
author Mackensen, Andreas
Hubberten, Hans-Wolfgang
Scheele, Norbert
Schlitzer, Reiner
author_facet Mackensen, Andreas
Hubberten, Hans-Wolfgang
Scheele, Norbert
Schlitzer, Reiner
author_sort Mackensen, Andreas
title Hydrochemistry measured on water bottle samples during POLARSTERN cruise ANT-VIII/2 ...
title_short Hydrochemistry measured on water bottle samples during POLARSTERN cruise ANT-VIII/2 ...
title_full Hydrochemistry measured on water bottle samples during POLARSTERN cruise ANT-VIII/2 ...
title_fullStr Hydrochemistry measured on water bottle samples during POLARSTERN cruise ANT-VIII/2 ...
title_full_unstemmed Hydrochemistry measured on water bottle samples during POLARSTERN cruise ANT-VIII/2 ...
title_sort hydrochemistry measured on water bottle samples during polarstern cruise ant-viii/2 ...
publisher PANGAEA
publishDate 1996
url https://dx.doi.org/10.1594/pangaea.761833
https://doi.pangaea.de/10.1594/PANGAEA.761833
genre Southern Ocean
Weddell Sea
genre_facet Southern Ocean
Weddell Sea
op_relation https://dx.doi.org/10.1029/95pa03840
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.76183310.1029/95pa03840
_version_ 1810481713070997504