Th-234 in surface waters: Distribution of particle export flux across the Antarctic Circumpolar Current and in the Weddell Sea during the GEOTRACES expedition ZERO and DRAKE
ESA; Humboldt foundation; AB the Helmholtz Initiative and Networking Fund As part of the GEOTRACES Polarstern expedition ANTXXIV/3 (ZERO and DRAKE) we have measured the vertical distribution of Th-234 on sections through the Antarctic Circumpolar Current along the zero meridian and in Drake Passage...
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DEEP-SEA RES PT II
2011
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ftxiamenuniv:oai:dspace.xmu.edu.cn:2288/87793 2023-05-15T13:51:20+02:00 Th-234 in surface waters: Distribution of particle export flux across the Antarctic Circumpolar Current and in the Weddell Sea during the GEOTRACES expedition ZERO and DRAKE van der Loeff, Michiel Rutgers Cai, Pinghe H. Stimac, Ingrid Bracher, Astrid Middag, Rob Klunder, Maarten B. van Heuven, Steven M. A. C. 蔡平河 2011-12-15 http://dspace.xmu.edu.cn/handle/2288/87793 en_US eng DEEP-SEA RES PT II DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY, 2011,58(25-26):2749-2766 WOS:000297002300017 http://dspace.xmu.edu.cn/handle/2288/87793 http://dx.doi.org/10.1016/j.dsr2.2011.02.004 PARTICULATE ORGANIC-CARBON NATURAL IRON FERTILIZATION SMALL-VOLUME TECHNIQUE OCEAN ATLANTIC SECTOR SOUTHERN-OCEAN POLAR FRONT ATMOSPHERIC CO2 SPRING BLOOM MIXED-LAYER SEAWATER Article 2011 ftxiamenuniv 2020-07-21T11:42:26Z ESA; Humboldt foundation; AB the Helmholtz Initiative and Networking Fund As part of the GEOTRACES Polarstern expedition ANTXXIV/3 (ZERO and DRAKE) we have measured the vertical distribution of Th-234 on sections through the Antarctic Circumpolar Current along the zero meridian and in Drake Passage and on an EW section through the Weddell Sea. Steady state export fluxes of Th-234 from the upper 100 m, derived from the depletion of Th-234 with respect to its parent U-238, ranged from 621 +/- 105 to 1773 +/- 90 dpm m(-2) d(-1). This Th-234 flux was converted into an export flux of organic carbon ranging from 3.1 to 13.2 mmol C m(-2) d(-1) (2.1-9.0 mmol C m(-2) d(-1)) using POC/Th-234 ratio of bulk (respectively > 50 mu m) suspended particles at the export depth (100 m). Non-steady state fluxes assuming zero flux under ice cover were up to 23% higher. In addition, particulate and dissolved Th-234 were measured underway in high resolution in the surface water with a semi-automated procedure. Particulate Th-234 in surface waters is inversely correlated with light transmission and pCO(2) and positively with fluorescence and optical backscatter and is interpreted as a proxy for algal biomass. High resolution underway mapping of particulate and dissolved Th-234 in surface water shows clearly where trace elements are absorbed by plankton and where they are exported to depth. Quantitative determination of the export flux requires the full Th-234 profile since surface depletion and export flux become decoupled through changes in wind mixed layer depth and in contribution to export from subsurface layers. In a zone of very low algal abundance (54-58 degrees S at the zero meridian), confirmed by satellite Chl-a data, the lowest carbon export of the ACC was observed, allowing Fe and Mn to maintain their highest surface concentrations. An ice-edge bloom that had developed in December/January in the zone 60-65 degrees S as studied during the previous leg had caused a high export flux at 64.5 degrees S when we visited the area 2 months later (February/March). The ice-edge bloom had then shifted south to 65-69 degrees S evident from uptake of CO2 and dissolved Fe, Mn and Th-234, without causing export yet. In this way, the parallel analysis of Th-234 can help to explain the scavenging behavior of other trace elements. (C) 2011 Elsevier Ltd. All rights reserved. Article in Journal/Newspaper Antarc* Antarctic Drake Passage Southern Ocean Weddell Sea Xiamen University Institutional Repository Antarctic Drake Passage Southern Ocean The Antarctic Weddell Weddell Sea |
institution |
Open Polar |
collection |
Xiamen University Institutional Repository |
op_collection_id |
ftxiamenuniv |
language |
English |
topic |
PARTICULATE ORGANIC-CARBON NATURAL IRON FERTILIZATION SMALL-VOLUME TECHNIQUE OCEAN ATLANTIC SECTOR SOUTHERN-OCEAN POLAR FRONT ATMOSPHERIC CO2 SPRING BLOOM MIXED-LAYER SEAWATER |
spellingShingle |
PARTICULATE ORGANIC-CARBON NATURAL IRON FERTILIZATION SMALL-VOLUME TECHNIQUE OCEAN ATLANTIC SECTOR SOUTHERN-OCEAN POLAR FRONT ATMOSPHERIC CO2 SPRING BLOOM MIXED-LAYER SEAWATER van der Loeff, Michiel Rutgers Cai, Pinghe H. Stimac, Ingrid Bracher, Astrid Middag, Rob Klunder, Maarten B. van Heuven, Steven M. A. C. 蔡平河 Th-234 in surface waters: Distribution of particle export flux across the Antarctic Circumpolar Current and in the Weddell Sea during the GEOTRACES expedition ZERO and DRAKE |
topic_facet |
PARTICULATE ORGANIC-CARBON NATURAL IRON FERTILIZATION SMALL-VOLUME TECHNIQUE OCEAN ATLANTIC SECTOR SOUTHERN-OCEAN POLAR FRONT ATMOSPHERIC CO2 SPRING BLOOM MIXED-LAYER SEAWATER |
description |
ESA; Humboldt foundation; AB the Helmholtz Initiative and Networking Fund As part of the GEOTRACES Polarstern expedition ANTXXIV/3 (ZERO and DRAKE) we have measured the vertical distribution of Th-234 on sections through the Antarctic Circumpolar Current along the zero meridian and in Drake Passage and on an EW section through the Weddell Sea. Steady state export fluxes of Th-234 from the upper 100 m, derived from the depletion of Th-234 with respect to its parent U-238, ranged from 621 +/- 105 to 1773 +/- 90 dpm m(-2) d(-1). This Th-234 flux was converted into an export flux of organic carbon ranging from 3.1 to 13.2 mmol C m(-2) d(-1) (2.1-9.0 mmol C m(-2) d(-1)) using POC/Th-234 ratio of bulk (respectively > 50 mu m) suspended particles at the export depth (100 m). Non-steady state fluxes assuming zero flux under ice cover were up to 23% higher. In addition, particulate and dissolved Th-234 were measured underway in high resolution in the surface water with a semi-automated procedure. Particulate Th-234 in surface waters is inversely correlated with light transmission and pCO(2) and positively with fluorescence and optical backscatter and is interpreted as a proxy for algal biomass. High resolution underway mapping of particulate and dissolved Th-234 in surface water shows clearly where trace elements are absorbed by plankton and where they are exported to depth. Quantitative determination of the export flux requires the full Th-234 profile since surface depletion and export flux become decoupled through changes in wind mixed layer depth and in contribution to export from subsurface layers. In a zone of very low algal abundance (54-58 degrees S at the zero meridian), confirmed by satellite Chl-a data, the lowest carbon export of the ACC was observed, allowing Fe and Mn to maintain their highest surface concentrations. An ice-edge bloom that had developed in December/January in the zone 60-65 degrees S as studied during the previous leg had caused a high export flux at 64.5 degrees S when we visited the area 2 months later (February/March). The ice-edge bloom had then shifted south to 65-69 degrees S evident from uptake of CO2 and dissolved Fe, Mn and Th-234, without causing export yet. In this way, the parallel analysis of Th-234 can help to explain the scavenging behavior of other trace elements. (C) 2011 Elsevier Ltd. All rights reserved. |
format |
Article in Journal/Newspaper |
author |
van der Loeff, Michiel Rutgers Cai, Pinghe H. Stimac, Ingrid Bracher, Astrid Middag, Rob Klunder, Maarten B. van Heuven, Steven M. A. C. 蔡平河 |
author_facet |
van der Loeff, Michiel Rutgers Cai, Pinghe H. Stimac, Ingrid Bracher, Astrid Middag, Rob Klunder, Maarten B. van Heuven, Steven M. A. C. 蔡平河 |
author_sort |
van der Loeff, Michiel Rutgers |
title |
Th-234 in surface waters: Distribution of particle export flux across the Antarctic Circumpolar Current and in the Weddell Sea during the GEOTRACES expedition ZERO and DRAKE |
title_short |
Th-234 in surface waters: Distribution of particle export flux across the Antarctic Circumpolar Current and in the Weddell Sea during the GEOTRACES expedition ZERO and DRAKE |
title_full |
Th-234 in surface waters: Distribution of particle export flux across the Antarctic Circumpolar Current and in the Weddell Sea during the GEOTRACES expedition ZERO and DRAKE |
title_fullStr |
Th-234 in surface waters: Distribution of particle export flux across the Antarctic Circumpolar Current and in the Weddell Sea during the GEOTRACES expedition ZERO and DRAKE |
title_full_unstemmed |
Th-234 in surface waters: Distribution of particle export flux across the Antarctic Circumpolar Current and in the Weddell Sea during the GEOTRACES expedition ZERO and DRAKE |
title_sort |
th-234 in surface waters: distribution of particle export flux across the antarctic circumpolar current and in the weddell sea during the geotraces expedition zero and drake |
publisher |
DEEP-SEA RES PT II |
publishDate |
2011 |
url |
http://dspace.xmu.edu.cn/handle/2288/87793 |
geographic |
Antarctic Drake Passage Southern Ocean The Antarctic Weddell Weddell Sea |
geographic_facet |
Antarctic Drake Passage Southern Ocean The Antarctic Weddell Weddell Sea |
genre |
Antarc* Antarctic Drake Passage Southern Ocean Weddell Sea |
genre_facet |
Antarc* Antarctic Drake Passage Southern Ocean Weddell Sea |
op_source |
http://dx.doi.org/10.1016/j.dsr2.2011.02.004 |
op_relation |
DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY, 2011,58(25-26):2749-2766 WOS:000297002300017 http://dspace.xmu.edu.cn/handle/2288/87793 |
_version_ |
1766255148005326848 |