(Table 1) Water column silicic acid concentrations and Si isotopic composition during Marion Dufresne cruise MD166 off South Africa
Silicon isotopic signatures (d30Si) of water column silicic acid (Si(OH)4) were measured in the Southern Ocean, along a meridional transect from South Africa (Subtropical Zone) down to 57° S (northern Weddell Gyre). This provides the first reported data of a summer transect across the whole Antarcti...
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PANGAEA
2011
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.809699 https://doi.org/10.1594/PANGAEA.809699 |
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.809699 |
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record_format |
openpolar |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
BONUS-GOODHOPE GIPY6 Colorimetry CTD/Rosette CTD-RO Date/Time of event DEPTH water Event label GEOTRACES Global marine biogeochemical cycles of trace elements and their isotopes International Polar Year (2007-2008) IPY Latitude of event Longitude of event Marion Dufresne (1995) MD_Large_2 MD_Large_3 MD_Large_4 MD_Large_5 MD_Large_6 MD_Large_7 MD_Super_1 MD_Super_2 MD_Super_3 MD_Super_4 MD_Super_5 MD166 Multi-collector inductively coupled plasma mass spectrometer (MC-ICP-MS) off South Africa Sample comment Silicic acid δ30Si error |
spellingShingle |
BONUS-GOODHOPE GIPY6 Colorimetry CTD/Rosette CTD-RO Date/Time of event DEPTH water Event label GEOTRACES Global marine biogeochemical cycles of trace elements and their isotopes International Polar Year (2007-2008) IPY Latitude of event Longitude of event Marion Dufresne (1995) MD_Large_2 MD_Large_3 MD_Large_4 MD_Large_5 MD_Large_6 MD_Large_7 MD_Super_1 MD_Super_2 MD_Super_3 MD_Super_4 MD_Super_5 MD166 Multi-collector inductively coupled plasma mass spectrometer (MC-ICP-MS) off South Africa Sample comment Silicic acid δ30Si error Fripiat, François Cavagna, Anne-Julie Dehairs, Frank Speich, Sabrina André, Luc Cardinal, Damien (Table 1) Water column silicic acid concentrations and Si isotopic composition during Marion Dufresne cruise MD166 off South Africa |
topic_facet |
BONUS-GOODHOPE GIPY6 Colorimetry CTD/Rosette CTD-RO Date/Time of event DEPTH water Event label GEOTRACES Global marine biogeochemical cycles of trace elements and their isotopes International Polar Year (2007-2008) IPY Latitude of event Longitude of event Marion Dufresne (1995) MD_Large_2 MD_Large_3 MD_Large_4 MD_Large_5 MD_Large_6 MD_Large_7 MD_Super_1 MD_Super_2 MD_Super_3 MD_Super_4 MD_Super_5 MD166 Multi-collector inductively coupled plasma mass spectrometer (MC-ICP-MS) off South Africa Sample comment Silicic acid δ30Si error |
description |
Silicon isotopic signatures (d30Si) of water column silicic acid (Si(OH)4) were measured in the Southern Ocean, along a meridional transect from South Africa (Subtropical Zone) down to 57° S (northern Weddell Gyre). This provides the first reported data of a summer transect across the whole Antarctic Circumpolar Current (ACC). d30Si variations are large in the upper 1000 m, reflecting the effect of the silica pump superimposed upon meridional water transfer across the ACC: the transport of Antarctic surface waters northward by a net Ekman drift and their convergence and mixing with warmer upper-ocean Si-depleted waters to the north. Using Si isotopic signatures, we determine different mixing interfaces: the Antarctic Surface Water (AASW), the Antarctic Intermediate Water (AAIW), and thermoclines in the low latitude areas. The residual silicic acid concentrations of end-members control the d30Si alteration of the mixing products and with the exception of AASW, all mixing interfaces have a highly Si-depleted mixed layer end-member. These processes deplete the silicic acid AASW concentration northward, across the different interfaces, without significantly changing the AASW d30Si composition. By comparing our new results with a previous study in the Australian sector we show that during the circumpolar transport of the ACC eastward, the d30Si composition of the silicic acid pools is getting slightly, but significantly lighter from the Atlantic to the Australian sectors. This results either from the dissolution of biogenic silica in the deeper layers and/or from an isopycnal mixing with the deep water masses in the different oceanic basins: North Atlantic Deep Water in the Atlantic, and Indian Ocean deep water in the Indo-Australian sector. This isotopic trend is further transmitted to the subsurface waters, representing mixing interfaces between the surface and deeper layers. Through the use of d30Si constraints, net biogenic silica production (representative of annual export), at the Greenwich Meridian is ... |
format |
Dataset |
author |
Fripiat, François Cavagna, Anne-Julie Dehairs, Frank Speich, Sabrina André, Luc Cardinal, Damien |
author_facet |
Fripiat, François Cavagna, Anne-Julie Dehairs, Frank Speich, Sabrina André, Luc Cardinal, Damien |
author_sort |
Fripiat, François |
title |
(Table 1) Water column silicic acid concentrations and Si isotopic composition during Marion Dufresne cruise MD166 off South Africa |
title_short |
(Table 1) Water column silicic acid concentrations and Si isotopic composition during Marion Dufresne cruise MD166 off South Africa |
title_full |
(Table 1) Water column silicic acid concentrations and Si isotopic composition during Marion Dufresne cruise MD166 off South Africa |
title_fullStr |
(Table 1) Water column silicic acid concentrations and Si isotopic composition during Marion Dufresne cruise MD166 off South Africa |
title_full_unstemmed |
(Table 1) Water column silicic acid concentrations and Si isotopic composition during Marion Dufresne cruise MD166 off South Africa |
title_sort |
(table 1) water column silicic acid concentrations and si isotopic composition during marion dufresne cruise md166 off south africa |
publisher |
PANGAEA |
publishDate |
2011 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.809699 https://doi.org/10.1594/PANGAEA.809699 |
op_coverage |
MEDIAN LATITUDE: -46.966364 * MEDIAN LONGITUDE: 4.979091 * SOUTH-BOUND LATITUDE: -57.320000 * WEST-BOUND LONGITUDE: 0.000000 * NORTH-BOUND LATITUDE: -36.450000 * EAST-BOUND LONGITUDE: 13.100000 * DATE/TIME START: 2008-02-21T00:00:00 * DATE/TIME END: 2008-03-16T00:00:00 * MINIMUM DEPTH, water: 3 m * MAXIMUM DEPTH, water: 5000 m |
long_lat |
ENVELOPE(0.000000,13.100000,-36.450000,-57.320000) |
genre |
Antarc* Antarctic International Polar Year IPY North Atlantic Deep Water North Atlantic Southern Ocean |
genre_facet |
Antarc* Antarctic International Polar Year IPY North Atlantic Deep Water North Atlantic Southern Ocean |
op_source |
Supplement to: Fripiat, François; Cavagna, Anne-Julie; Dehairs, Frank; Speich, Sabrina; André, Luc; Cardinal, Damien (2011): Silicon pool dynamics and biogenic silica export in the Southern Ocean inferred from Si-isotopes. Ocean Science, 7(5), 533-547, https://doi.org/10.5194/os-7-533-2011 |
op_relation |
Fripiat, François; Cavagna, Anne-Julie; Dehairs, Frank; de Brauwere, A; André, Luc; Cardinal, Damien (2012): (Table 1) Water column biogenic silica concentrations and Si isotopic composition during Marion Dufresne cruise MD166 off South Africa [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.809702 (Data on biogenic silica can be found in Fripiat et al. (2012) dataset) https://doi.pangaea.de/10.1594/PANGAEA.809699 https://doi.org/10.1594/PANGAEA.809699 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1594/PANGAEA.80969910.5194/os-7-533-201110.1594/PANGAEA.809702 |
_version_ |
1810289177793658880 |
spelling |
ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.809699 2024-09-15T17:48:07+00:00 (Table 1) Water column silicic acid concentrations and Si isotopic composition during Marion Dufresne cruise MD166 off South Africa Fripiat, François Cavagna, Anne-Julie Dehairs, Frank Speich, Sabrina André, Luc Cardinal, Damien MEDIAN LATITUDE: -46.966364 * MEDIAN LONGITUDE: 4.979091 * SOUTH-BOUND LATITUDE: -57.320000 * WEST-BOUND LONGITUDE: 0.000000 * NORTH-BOUND LATITUDE: -36.450000 * EAST-BOUND LONGITUDE: 13.100000 * DATE/TIME START: 2008-02-21T00:00:00 * DATE/TIME END: 2008-03-16T00:00:00 * MINIMUM DEPTH, water: 3 m * MAXIMUM DEPTH, water: 5000 m 2011 text/tab-separated-values, 362 data points https://doi.pangaea.de/10.1594/PANGAEA.809699 https://doi.org/10.1594/PANGAEA.809699 en eng PANGAEA Fripiat, François; Cavagna, Anne-Julie; Dehairs, Frank; de Brauwere, A; André, Luc; Cardinal, Damien (2012): (Table 1) Water column biogenic silica concentrations and Si isotopic composition during Marion Dufresne cruise MD166 off South Africa [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.809702 (Data on biogenic silica can be found in Fripiat et al. (2012) dataset) https://doi.pangaea.de/10.1594/PANGAEA.809699 https://doi.org/10.1594/PANGAEA.809699 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess Supplement to: Fripiat, François; Cavagna, Anne-Julie; Dehairs, Frank; Speich, Sabrina; André, Luc; Cardinal, Damien (2011): Silicon pool dynamics and biogenic silica export in the Southern Ocean inferred from Si-isotopes. Ocean Science, 7(5), 533-547, https://doi.org/10.5194/os-7-533-2011 BONUS-GOODHOPE GIPY6 Colorimetry CTD/Rosette CTD-RO Date/Time of event DEPTH water Event label GEOTRACES Global marine biogeochemical cycles of trace elements and their isotopes International Polar Year (2007-2008) IPY Latitude of event Longitude of event Marion Dufresne (1995) MD_Large_2 MD_Large_3 MD_Large_4 MD_Large_5 MD_Large_6 MD_Large_7 MD_Super_1 MD_Super_2 MD_Super_3 MD_Super_4 MD_Super_5 MD166 Multi-collector inductively coupled plasma mass spectrometer (MC-ICP-MS) off South Africa Sample comment Silicic acid δ30Si error dataset 2011 ftpangaea https://doi.org/10.1594/PANGAEA.80969910.5194/os-7-533-201110.1594/PANGAEA.809702 2024-07-24T02:31:32Z Silicon isotopic signatures (d30Si) of water column silicic acid (Si(OH)4) were measured in the Southern Ocean, along a meridional transect from South Africa (Subtropical Zone) down to 57° S (northern Weddell Gyre). This provides the first reported data of a summer transect across the whole Antarctic Circumpolar Current (ACC). d30Si variations are large in the upper 1000 m, reflecting the effect of the silica pump superimposed upon meridional water transfer across the ACC: the transport of Antarctic surface waters northward by a net Ekman drift and their convergence and mixing with warmer upper-ocean Si-depleted waters to the north. Using Si isotopic signatures, we determine different mixing interfaces: the Antarctic Surface Water (AASW), the Antarctic Intermediate Water (AAIW), and thermoclines in the low latitude areas. The residual silicic acid concentrations of end-members control the d30Si alteration of the mixing products and with the exception of AASW, all mixing interfaces have a highly Si-depleted mixed layer end-member. These processes deplete the silicic acid AASW concentration northward, across the different interfaces, without significantly changing the AASW d30Si composition. By comparing our new results with a previous study in the Australian sector we show that during the circumpolar transport of the ACC eastward, the d30Si composition of the silicic acid pools is getting slightly, but significantly lighter from the Atlantic to the Australian sectors. This results either from the dissolution of biogenic silica in the deeper layers and/or from an isopycnal mixing with the deep water masses in the different oceanic basins: North Atlantic Deep Water in the Atlantic, and Indian Ocean deep water in the Indo-Australian sector. This isotopic trend is further transmitted to the subsurface waters, representing mixing interfaces between the surface and deeper layers. Through the use of d30Si constraints, net biogenic silica production (representative of annual export), at the Greenwich Meridian is ... Dataset Antarc* Antarctic International Polar Year IPY North Atlantic Deep Water North Atlantic Southern Ocean PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(0.000000,13.100000,-36.450000,-57.320000) |