Comparison of carbon and opal export rates between summer and spring bloom periods in the region of the Antarctic Polar Front, SE Atlantic
Although primary production in the Antarctic Circumpolar Current is not above the world average and carbon burial rates are low, 70 % of the world’s opal burial occurs in this zone and it has been suggested that blooms of large diatoms are responsible for this extraordinary situation. Here we compar...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.568.8142 2023-05-15T13:44:57+02:00 Comparison of carbon and opal export rates between summer and spring bloom periods in the region of the Antarctic Polar Front, SE Atlantic Ken Buesselerb Uli Bathmanna Inga Hensea John Andrewsb The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.568.8142 http://cafethorium.whoi.edu/website/images/VDL-DSRII2002V49.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.568.8142 http://cafethorium.whoi.edu/website/images/VDL-DSRII2002V49.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://cafethorium.whoi.edu/website/images/VDL-DSRII2002V49.pdf text ftciteseerx 2016-01-08T12:23:29Z Although primary production in the Antarctic Circumpolar Current is not above the world average and carbon burial rates are low, 70 % of the world’s opal burial occurs in this zone and it has been suggested that blooms of large diatoms are responsible for this extraordinary situation. Here we compare export fluxes during bloom and steady-state situations near the Antarctic Polar Front in the SE Atlantic. In a previous expedition during the austral spring, we observed the development of a bloom that led to the sudden export of particles (Deep-Sea Res. II 44 (1997) 457). Here we report the results of a second expedition to the same area in summer (December–January), 3 years later. 234Th was monitored in the surface water and in Rosette casts down to a water depth of 500m as tracer of export production in an intensive sampling program within a box of 275 375 km2. The distribution of particulate and dissolved 234Th was remarkably constant over time and location. Total (dissolved+particulate) 234Th activities were depleted relative to its parent 238U at the surface (234Th/238U activity ratio approximately 83%), reaching equilibrium at a depth of around 190m. This constant depletion corresponds to a 234Th export rate of 1115 dpm/m2/d, 35 % of the value observed during the spring bloom. Below 80m depth, 234Th on suspended particles correlates well with both particulate organic carbon (POC) and particulate biogenic silica (BSi), with a POC/234Th ratio of 10.270.8mmol/dpm and a BSi/234Th ratio of 2.970.2mmol/dpm. Using these ratios, the Text Antarc* Antarctic Unknown Antarctic Austral The Antarctic |
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English |
description |
Although primary production in the Antarctic Circumpolar Current is not above the world average and carbon burial rates are low, 70 % of the world’s opal burial occurs in this zone and it has been suggested that blooms of large diatoms are responsible for this extraordinary situation. Here we compare export fluxes during bloom and steady-state situations near the Antarctic Polar Front in the SE Atlantic. In a previous expedition during the austral spring, we observed the development of a bloom that led to the sudden export of particles (Deep-Sea Res. II 44 (1997) 457). Here we report the results of a second expedition to the same area in summer (December–January), 3 years later. 234Th was monitored in the surface water and in Rosette casts down to a water depth of 500m as tracer of export production in an intensive sampling program within a box of 275 375 km2. The distribution of particulate and dissolved 234Th was remarkably constant over time and location. Total (dissolved+particulate) 234Th activities were depleted relative to its parent 238U at the surface (234Th/238U activity ratio approximately 83%), reaching equilibrium at a depth of around 190m. This constant depletion corresponds to a 234Th export rate of 1115 dpm/m2/d, 35 % of the value observed during the spring bloom. Below 80m depth, 234Th on suspended particles correlates well with both particulate organic carbon (POC) and particulate biogenic silica (BSi), with a POC/234Th ratio of 10.270.8mmol/dpm and a BSi/234Th ratio of 2.970.2mmol/dpm. Using these ratios, the |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Ken Buesselerb Uli Bathmanna Inga Hensea John Andrewsb |
spellingShingle |
Ken Buesselerb Uli Bathmanna Inga Hensea John Andrewsb Comparison of carbon and opal export rates between summer and spring bloom periods in the region of the Antarctic Polar Front, SE Atlantic |
author_facet |
Ken Buesselerb Uli Bathmanna Inga Hensea John Andrewsb |
author_sort |
Ken Buesselerb |
title |
Comparison of carbon and opal export rates between summer and spring bloom periods in the region of the Antarctic Polar Front, SE Atlantic |
title_short |
Comparison of carbon and opal export rates between summer and spring bloom periods in the region of the Antarctic Polar Front, SE Atlantic |
title_full |
Comparison of carbon and opal export rates between summer and spring bloom periods in the region of the Antarctic Polar Front, SE Atlantic |
title_fullStr |
Comparison of carbon and opal export rates between summer and spring bloom periods in the region of the Antarctic Polar Front, SE Atlantic |
title_full_unstemmed |
Comparison of carbon and opal export rates between summer and spring bloom periods in the region of the Antarctic Polar Front, SE Atlantic |
title_sort |
comparison of carbon and opal export rates between summer and spring bloom periods in the region of the antarctic polar front, se atlantic |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.568.8142 http://cafethorium.whoi.edu/website/images/VDL-DSRII2002V49.pdf |
geographic |
Antarctic Austral The Antarctic |
geographic_facet |
Antarctic Austral The Antarctic |
genre |
Antarc* Antarctic |
genre_facet |
Antarc* Antarctic |
op_source |
http://cafethorium.whoi.edu/website/images/VDL-DSRII2002V49.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.568.8142 http://cafethorium.whoi.edu/website/images/VDL-DSRII2002V49.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766208903455965184 |