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Title: Limited Acute Influence of Aerobic Methane Oxidation on Ocean Carbon Dioxide and pH in Hudson Canyon, Northern U.S. Atlantic Margin

Abstract

The ocean continental shelves host the largest global reservoir of methane (CH 4). Despite the great extent of these CH 4 reservoirs, much of the CH 4 released into deep ocean environments appear to dissolve in seawater prior to atmospheric emission. Once dissolved in ocean water, the CH 4 emitted can be aerobically oxidized and converted into either carbon dioxide (CO 2) or biomass. While hypotheses have been levied suggesting that the CO 2 produced from aerobic methane oxidation could enhance ocean acidification, no empirical research has been performed to confirm or refute this hypothesis. The work presented here investigates local changes in seawater-dissolved CO 2 and pH in a region that is experiencing active CH 4 seepage near the upper stability boundary of methane clathrate hydrates. We show that in an area of elevated CH 4 concentrations and aerobic oxidation rates, Hudson Canyon, aerobic CH 4 oxidation is only responsible for 0.3 ± 0.2% of the observed change in dissolved inorganic carbon. Measurements further show that the remineralization of both old marine and young terrestrial organic carbon is contributing more substantially to the observed changes. While this investigation did not investigate chronic, multiyear changes in ocean acidification due tomore » CH 4 oxidation, these results suggest that over short timescales, CH 4 oxidation in seep fields does not have an acute influence on seawater pH.« less

Authors:
ORCiD logo [1]; ORCiD logo [1]
  1. Univ. of Rochester, NY (United States)
Publication Date:
Research Org.:
Univ. of Rochester, NY (United States)
Sponsoring Org.:
USDOE Office of Fossil Energy (FE)
OSTI Identifier:
1539765
Alternate Identifier(s):
OSTI ID: 1460427
Grant/Contract Number:  
FE0028980; 0028980
Resource Type:
Accepted Manuscript
Journal Name:
Journal of Geophysical Research. Biogeosciences
Additional Journal Information:
Journal Volume: 123; Journal Issue: 7; Journal ID: ISSN 2169-8953
Publisher:
American Geophysical Union
Country of Publication:
United States
Language:
English
Subject:
54 ENVIRONMENTAL SCIENCES; Environmental Sciences & Ecology; Geology

Citation Formats

Garcia‐Tigreros, Fenix, and Kessler, John D. Limited Acute Influence of Aerobic Methane Oxidation on Ocean Carbon Dioxide and pH in Hudson Canyon, Northern U.S. Atlantic Margin. United States: N. p., 2018. Web. doi:10.1029/2018jg004384.
Garcia‐Tigreros, Fenix, & Kessler, John D. Limited Acute Influence of Aerobic Methane Oxidation on Ocean Carbon Dioxide and pH in Hudson Canyon, Northern U.S. Atlantic Margin. United States. doi:10.1029/2018jg004384.
Garcia‐Tigreros, Fenix, and Kessler, John D. Sun . "Limited Acute Influence of Aerobic Methane Oxidation on Ocean Carbon Dioxide and pH in Hudson Canyon, Northern U.S. Atlantic Margin". United States. doi:10.1029/2018jg004384. https://www.osti.gov/servlets/purl/1539765.
@article{osti_1539765,
title = {Limited Acute Influence of Aerobic Methane Oxidation on Ocean Carbon Dioxide and pH in Hudson Canyon, Northern U.S. Atlantic Margin},
author = {Garcia‐Tigreros, Fenix and Kessler, John D.},
abstractNote = {The ocean continental shelves host the largest global reservoir of methane (CH4). Despite the great extent of these CH4 reservoirs, much of the CH4 released into deep ocean environments appear to dissolve in seawater prior to atmospheric emission. Once dissolved in ocean water, the CH4 emitted can be aerobically oxidized and converted into either carbon dioxide (CO2) or biomass. While hypotheses have been levied suggesting that the CO2 produced from aerobic methane oxidation could enhance ocean acidification, no empirical research has been performed to confirm or refute this hypothesis. The work presented here investigates local changes in seawater-dissolved CO2 and pH in a region that is experiencing active CH4 seepage near the upper stability boundary of methane clathrate hydrates. We show that in an area of elevated CH4 concentrations and aerobic oxidation rates, Hudson Canyon, aerobic CH4 oxidation is only responsible for 0.3 ± 0.2% of the observed change in dissolved inorganic carbon. Measurements further show that the remineralization of both old marine and young terrestrial organic carbon is contributing more substantially to the observed changes. While this investigation did not investigate chronic, multiyear changes in ocean acidification due to CH4 oxidation, these results suggest that over short timescales, CH4 oxidation in seep fields does not have an acute influence on seawater pH.},
doi = {10.1029/2018jg004384},
journal = {Journal of Geophysical Research. Biogeosciences},
number = 7,
volume = 123,
place = {United States},
year = {2018},
month = {7}
}

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