The role of ocean acidification in systemic carbonate mineral suppression in the Bering Sea

Ocean acidification driven by absorption of anthropogenic carbon dioxide (CO2) from the atmosphere is now recognized as a systemic, global process that could threaten diverse marine ecosystems and a number of commercially important species. The change in calcium carbonate (CaCO3) mineral saturation...

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Published in:Geophysical Research Letters
Main Authors: Mathis, Jeremy T., Cross, Jessica N., Bates, Nicholas R.
Format: Article in Journal/Newspaper
Language:English
Published: 2011
Subjects:
Online Access:https://eprints.soton.ac.uk/357317/
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spelling ftsouthampton:oai:eprints.soton.ac.uk:357317 2023-07-30T04:02:40+02:00 The role of ocean acidification in systemic carbonate mineral suppression in the Bering Sea Mathis, Jeremy T. Cross, Jessica N. Bates, Nicholas R. 2011 https://eprints.soton.ac.uk/357317/ English eng Mathis, Jeremy T., Cross, Jessica N. and Bates, Nicholas R. (2011) The role of ocean acidification in systemic carbonate mineral suppression in the Bering Sea. Geophysical Research Letters, 38 (19), L19602. (doi:10.1029/2011GL048884 <http://dx.doi.org/10.1029/2011GL048884>). Article PeerReviewed 2011 ftsouthampton https://doi.org/10.1029/2011GL048884 2023-07-09T21:49:12Z Ocean acidification driven by absorption of anthropogenic carbon dioxide (CO2) from the atmosphere is now recognized as a systemic, global process that could threaten diverse marine ecosystems and a number of commercially important species. The change in calcium carbonate (CaCO3) mineral saturation states (?) brought on by the reduction of seawater pH is most pronounced in high latitude regions where unique biogeochemical processes create an environment more susceptible to the suppression of ? values for aragonite and calcite, which are critical to shell building organisms. New observations from the eastern Bering Sea shelf show that remineralization of organic matter exported from surface waters rapidly increases bottom water CO2 concentrations over the shelf in summer and fall, suppressing ? values. The removal of CO2 from surface waters by high rates of phytoplankton primary production increases ? values between spring and summer, but these increases are partly counteracted by mixing with sea ice melt water and terrestrial river runoff that have low ? values. While these environmental processes play an important role in creating seasonally low saturation states, ocean uptake of anthropogenic CO2 has shifted ? values for aragonite to below the saturation horizon in broad regions across the shelf for at least several months each year. Furthermore, we also report that calcite became undersaturated in September of 2009 in the bottom waters over the shelf. The reduction in CaCO3 mineral saturation states could have profound implications for several keystone calcifying species in the Bering Sea, particularly the commercially important crab fisheries. Article in Journal/Newspaper Bering Sea Ocean acidification Sea ice University of Southampton: e-Prints Soton Bering Sea Geophysical Research Letters 38 19 n/a n/a
institution Open Polar
collection University of Southampton: e-Prints Soton
op_collection_id ftsouthampton
language English
description Ocean acidification driven by absorption of anthropogenic carbon dioxide (CO2) from the atmosphere is now recognized as a systemic, global process that could threaten diverse marine ecosystems and a number of commercially important species. The change in calcium carbonate (CaCO3) mineral saturation states (?) brought on by the reduction of seawater pH is most pronounced in high latitude regions where unique biogeochemical processes create an environment more susceptible to the suppression of ? values for aragonite and calcite, which are critical to shell building organisms. New observations from the eastern Bering Sea shelf show that remineralization of organic matter exported from surface waters rapidly increases bottom water CO2 concentrations over the shelf in summer and fall, suppressing ? values. The removal of CO2 from surface waters by high rates of phytoplankton primary production increases ? values between spring and summer, but these increases are partly counteracted by mixing with sea ice melt water and terrestrial river runoff that have low ? values. While these environmental processes play an important role in creating seasonally low saturation states, ocean uptake of anthropogenic CO2 has shifted ? values for aragonite to below the saturation horizon in broad regions across the shelf for at least several months each year. Furthermore, we also report that calcite became undersaturated in September of 2009 in the bottom waters over the shelf. The reduction in CaCO3 mineral saturation states could have profound implications for several keystone calcifying species in the Bering Sea, particularly the commercially important crab fisheries.
format Article in Journal/Newspaper
author Mathis, Jeremy T.
Cross, Jessica N.
Bates, Nicholas R.
spellingShingle Mathis, Jeremy T.
Cross, Jessica N.
Bates, Nicholas R.
The role of ocean acidification in systemic carbonate mineral suppression in the Bering Sea
author_facet Mathis, Jeremy T.
Cross, Jessica N.
Bates, Nicholas R.
author_sort Mathis, Jeremy T.
title The role of ocean acidification in systemic carbonate mineral suppression in the Bering Sea
title_short The role of ocean acidification in systemic carbonate mineral suppression in the Bering Sea
title_full The role of ocean acidification in systemic carbonate mineral suppression in the Bering Sea
title_fullStr The role of ocean acidification in systemic carbonate mineral suppression in the Bering Sea
title_full_unstemmed The role of ocean acidification in systemic carbonate mineral suppression in the Bering Sea
title_sort role of ocean acidification in systemic carbonate mineral suppression in the bering sea
publishDate 2011
url https://eprints.soton.ac.uk/357317/
geographic Bering Sea
geographic_facet Bering Sea
genre Bering Sea
Ocean acidification
Sea ice
genre_facet Bering Sea
Ocean acidification
Sea ice
op_relation Mathis, Jeremy T., Cross, Jessica N. and Bates, Nicholas R. (2011) The role of ocean acidification in systemic carbonate mineral suppression in the Bering Sea. Geophysical Research Letters, 38 (19), L19602. (doi:10.1029/2011GL048884 <http://dx.doi.org/10.1029/2011GL048884>).
op_doi https://doi.org/10.1029/2011GL048884
container_title Geophysical Research Letters
container_volume 38
container_issue 19
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