Seasonal distribution of dissolved inorganic carbon and net community production on the Bering Sea shelf

In order to assess the current state of net community production (NCP) in the southeastern Bering Sea, we measured the spatio-temporal distribution and controls on dissolved inorganic carbon (DIC) concentrations in spring and summer of 2008 across six shelf domains defined by differing biogeochemica...

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Main Authors: J. T. Mathis, J. N. Cross, N. R. Bates, S. Bradley Moran, M. W. Lomas, C. W. Mordy, P. J. Stabeno
Format: Article
Language:English
Published: Copernicus Publications 2010-05-01
Series:Biogeosciences
Online Access:http://www.biogeosciences.net/7/1769/2010/bg-7-1769-2010.pdf
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author J. T. Mathis
J. N. Cross
N. R. Bates
S. Bradley Moran
M. W. Lomas
C. W. Mordy
P. J. Stabeno
author_facet J. T. Mathis
J. N. Cross
N. R. Bates
S. Bradley Moran
M. W. Lomas
C. W. Mordy
P. J. Stabeno
author_sort J. T. Mathis
collection DOAJ
description In order to assess the current state of net community production (NCP) in the southeastern Bering Sea, we measured the spatio-temporal distribution and controls on dissolved inorganic carbon (DIC) concentrations in spring and summer of 2008 across six shelf domains defined by differing biogeochemical characteristics. DIC concentrations were tightly coupled to salinity in spring and ranged from ~1900 μmoles kg<sup>−1</sup> over the inner shelf to ~2400 μmoles kg<sup>−1</sup> in the deeper waters of the Bering Sea. In summer, DIC concentrations were lower due to dilution from sea ice melt, terrestrial inputs, and primary production. Concentrations were found to be as low ~1800 μmoles kg<sup>−1</sup> over the inner shelf. We found that DIC concentrations were drawn down 30–150 μmoles kg<sup>−1</sup> in the upper 30 m of the water column due to primary production and calcium carbonate formation between the spring and summer occupations. Using the seasonal drawdown of DIC, estimated rates of NCP on the inner, middle, and outer shelf averaged 28 ± 9 mmoles C m<sup>−2</sup> d<sup>−1</sup>. However, higher rates of NCP (40–47 mmoles C m<sup>−2</sup> d<sup>−1</sup>) were observed in the "Green Belt" where the greatest confluence of nutrient-rich basin water and iron-rich shelf water occurs. We estimated that in 2008, total NCP across the shelf was on the order of ~96 Tg C yr<sup>−1</sup>. Due to the paucity of consistent, comparable productivity data, it is impossible at this time to quantify whether the system is becoming more or less productive. However, as changing climate continues to modify the character of the Bering Sea, we have shown that NCP can be an important indicator of how the ecosystem is functioning.
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spelling doaj.art-32d1b7f0bcdd450799772837b66430fd2022-12-22T03:21:11ZengCopernicus PublicationsBiogeosciences1726-41701726-41892010-05-01751769178710.5194/bg-7-1769-2010Seasonal distribution of dissolved inorganic carbon and net community production on the Bering Sea shelfJ. T. MathisJ. N. CrossN. R. BatesS. Bradley MoranM. W. LomasC. W. MordyP. J. StabenoIn order to assess the current state of net community production (NCP) in the southeastern Bering Sea, we measured the spatio-temporal distribution and controls on dissolved inorganic carbon (DIC) concentrations in spring and summer of 2008 across six shelf domains defined by differing biogeochemical characteristics. DIC concentrations were tightly coupled to salinity in spring and ranged from ~1900 μmoles kg<sup>−1</sup> over the inner shelf to ~2400 μmoles kg<sup>−1</sup> in the deeper waters of the Bering Sea. In summer, DIC concentrations were lower due to dilution from sea ice melt, terrestrial inputs, and primary production. Concentrations were found to be as low ~1800 μmoles kg<sup>−1</sup> over the inner shelf. We found that DIC concentrations were drawn down 30–150 μmoles kg<sup>−1</sup> in the upper 30 m of the water column due to primary production and calcium carbonate formation between the spring and summer occupations. Using the seasonal drawdown of DIC, estimated rates of NCP on the inner, middle, and outer shelf averaged 28 ± 9 mmoles C m<sup>−2</sup> d<sup>−1</sup>. However, higher rates of NCP (40–47 mmoles C m<sup>−2</sup> d<sup>−1</sup>) were observed in the "Green Belt" where the greatest confluence of nutrient-rich basin water and iron-rich shelf water occurs. We estimated that in 2008, total NCP across the shelf was on the order of ~96 Tg C yr<sup>−1</sup>. Due to the paucity of consistent, comparable productivity data, it is impossible at this time to quantify whether the system is becoming more or less productive. However, as changing climate continues to modify the character of the Bering Sea, we have shown that NCP can be an important indicator of how the ecosystem is functioning.http://www.biogeosciences.net/7/1769/2010/bg-7-1769-2010.pdf
spellingShingle J. T. Mathis
J. N. Cross
N. R. Bates
S. Bradley Moran
M. W. Lomas
C. W. Mordy
P. J. Stabeno
Seasonal distribution of dissolved inorganic carbon and net community production on the Bering Sea shelf
Biogeosciences
title Seasonal distribution of dissolved inorganic carbon and net community production on the Bering Sea shelf
title_full Seasonal distribution of dissolved inorganic carbon and net community production on the Bering Sea shelf
title_fullStr Seasonal distribution of dissolved inorganic carbon and net community production on the Bering Sea shelf
title_full_unstemmed Seasonal distribution of dissolved inorganic carbon and net community production on the Bering Sea shelf
title_short Seasonal distribution of dissolved inorganic carbon and net community production on the Bering Sea shelf
title_sort seasonal distribution of dissolved inorganic carbon and net community production on the bering sea shelf
url http://www.biogeosciences.net/7/1769/2010/bg-7-1769-2010.pdf
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