Cited by 37Ocean Acidification Effects and ResponsesCO2 Sequestration and Geologic InteractionsCalcium Carbonate Crystallization and Inhibition

CaCO3 dissolution in carbonate-poor shelf sands increases with ocean acidification and porewater residence time

Lunstrum, Abby, Berelson, William·2022·Geochimica et Cosmochimica Acta

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Crossref · 10.1016/j.gca.2022.04.031

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1 of 1 references verified0 citation errors · 0 not checkable

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  • Benthic alkalinity flux from CaCO3 dissolution is expected to increase in the future in response to ocean acidification, in both shallow coastal and deep ocean sediments.

    “Projections of OAE scalability must also consider that benthic alkalinity flux from CaCO3 dissolution is expected to increase in the future in response to ocean acidification, in both shallow coastal and deep ocean sediments. 70-72”

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Authors
Lunstrum, A., & Berelson, W.
Affiliations
University of Southern California (US)
Corresponding author
Lunstrum, Abby
Venue
Geochimica et Cosmochimica Acta
Publisher
Elsevier BV
Published
2022-07
Volume
329
Pages
168-184
ISSN
0016-7037 (ISSN-L)
OpenAlex
W4229069362
Cited by
37
References
1
Citations by year
2026: 12 · 2025: 8 · 2024: 6 · 2023: 10 · 2022: 1
FWCI
2.98
Type
journal article
Language
en
Open access
closed
Locations
Geochimica et Cosmochimica Acta (publishedVersion)
Funders
Wrigley Institute for Environmental Studies, University of Southern California
Topics
  • Physical Sciences › Earth and Planetary Sciences › Oceanography › Ocean Acidification Effects and Responses
  • Physical Sciences › Environmental Science › Environmental Engineering › CO2 Sequestration and Geologic Interactions
  • Physical Sciences › Materials Science › Biomaterials › Calcium Carbonate Crystallization and Inhibition
Keywords
carbonate dissolution, ocean acidification, continental shelf sediments, carbonate saturation state, aragonite saturation state, calcite saturation, alkalinity, dissolved inorganic carbon, buffering capacity, aerobic respiration, Santa Catalina Island

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