Impact of Local Rivers On Coastal Acidification

Coastal ecosystems are highly dynamic areas for carbon cycling and are likely to be negatively impacted by increasing ocean acidification. This research focused on dissolved inorganic carbon (DIC) and total alkalinity (TA) in the Mississippi Sound to understand the influence of local rivers on coast...

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Main Authors: Savoie, Allison M., Moody, Amy, Gilbert, Melissa, Dillon, Kevin S., Howden, Stephan D., Shiller, Alan M., Hayes, Christopher T.
Format: Text
Language:unknown
Published: The Aquila Digital Community 2022
Subjects:
Online Access:https://aquila.usm.edu/fac_pubs/20576
https://aslopubs.onlinelibrary.wiley.com/doi/epdf/10.1002/lno.12237
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spelling ftsouthmissispun:oai:aquila.usm.edu:fac_pubs-21919 2023-07-30T04:06:05+02:00 Impact of Local Rivers On Coastal Acidification Savoie, Allison M. Moody, Amy Gilbert, Melissa Dillon, Kevin S. Howden, Stephan D. Shiller, Alan M. Hayes, Christopher T. 2022-12-01T08:00:00Z https://aquila.usm.edu/fac_pubs/20576 https://aslopubs.onlinelibrary.wiley.com/doi/epdf/10.1002/lno.12237 unknown The Aquila Digital Community https://aquila.usm.edu/fac_pubs/20576 https://aslopubs.onlinelibrary.wiley.com/doi/epdf/10.1002/lno.12237 Faculty Publications text 2022 ftsouthmissispun 2023-07-15T18:57:25Z Coastal ecosystems are highly dynamic areas for carbon cycling and are likely to be negatively impacted by increasing ocean acidification. This research focused on dissolved inorganic carbon (DIC) and total alkalinity (TA) in the Mississippi Sound to understand the influence of local rivers on coastal acidification. This area receives large fluxes of freshwater from local rivers, in addition to episodic inputs from the Mississippi River through a human-built diversion, the Bonnet Carré Spillway. Sites in the Sound were sampled monthly from August 2018 to November 2019 and weekly from June to August 2019 in response to an extended spillway opening. Prior to the 2019 spillway opening, the contribution of the local, lower alkalinity rivers to the Sound may have left the study area more susceptible to coastal acidification during winter months, with aragonite saturation states (Ωar) < 2. After the spillway opened, despite a large increase in TA throughout the Sound, aragonite saturation states remained low, likely due to hypoxia and increased CO2 concentrations in subsurface waters. Increased Mississippi River input could represent a new normal in the Sound's hydrography during spring and summer months. The spillway has been utilized more frequently over the last two decades due to increasing precipitation in the Mississippi River watershed, which is primarily associated with climate change. Future increases in freshwater discharge and the associated declines in salinity, dissolved oxygen, and Ωar in the Sound will likely be detrimental to oyster stocks and the resilience of similar ecosystems to coastal acidification. Text Ocean acidification The University of Southern Mississippi: The Aquila Digital Community
institution Open Polar
collection The University of Southern Mississippi: The Aquila Digital Community
op_collection_id ftsouthmissispun
language unknown
description Coastal ecosystems are highly dynamic areas for carbon cycling and are likely to be negatively impacted by increasing ocean acidification. This research focused on dissolved inorganic carbon (DIC) and total alkalinity (TA) in the Mississippi Sound to understand the influence of local rivers on coastal acidification. This area receives large fluxes of freshwater from local rivers, in addition to episodic inputs from the Mississippi River through a human-built diversion, the Bonnet Carré Spillway. Sites in the Sound were sampled monthly from August 2018 to November 2019 and weekly from June to August 2019 in response to an extended spillway opening. Prior to the 2019 spillway opening, the contribution of the local, lower alkalinity rivers to the Sound may have left the study area more susceptible to coastal acidification during winter months, with aragonite saturation states (Ωar) < 2. After the spillway opened, despite a large increase in TA throughout the Sound, aragonite saturation states remained low, likely due to hypoxia and increased CO2 concentrations in subsurface waters. Increased Mississippi River input could represent a new normal in the Sound's hydrography during spring and summer months. The spillway has been utilized more frequently over the last two decades due to increasing precipitation in the Mississippi River watershed, which is primarily associated with climate change. Future increases in freshwater discharge and the associated declines in salinity, dissolved oxygen, and Ωar in the Sound will likely be detrimental to oyster stocks and the resilience of similar ecosystems to coastal acidification.
format Text
author Savoie, Allison M.
Moody, Amy
Gilbert, Melissa
Dillon, Kevin S.
Howden, Stephan D.
Shiller, Alan M.
Hayes, Christopher T.
spellingShingle Savoie, Allison M.
Moody, Amy
Gilbert, Melissa
Dillon, Kevin S.
Howden, Stephan D.
Shiller, Alan M.
Hayes, Christopher T.
Impact of Local Rivers On Coastal Acidification
author_facet Savoie, Allison M.
Moody, Amy
Gilbert, Melissa
Dillon, Kevin S.
Howden, Stephan D.
Shiller, Alan M.
Hayes, Christopher T.
author_sort Savoie, Allison M.
title Impact of Local Rivers On Coastal Acidification
title_short Impact of Local Rivers On Coastal Acidification
title_full Impact of Local Rivers On Coastal Acidification
title_fullStr Impact of Local Rivers On Coastal Acidification
title_full_unstemmed Impact of Local Rivers On Coastal Acidification
title_sort impact of local rivers on coastal acidification
publisher The Aquila Digital Community
publishDate 2022
url https://aquila.usm.edu/fac_pubs/20576
https://aslopubs.onlinelibrary.wiley.com/doi/epdf/10.1002/lno.12237
genre Ocean acidification
genre_facet Ocean acidification
op_source Faculty Publications
op_relation https://aquila.usm.edu/fac_pubs/20576
https://aslopubs.onlinelibrary.wiley.com/doi/epdf/10.1002/lno.12237
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