Cited by 705Paleontology and Stratigraphy of FossilsGeology and Paleoclimatology ResearchOcean Acidification Effects and Responses

The role of the global carbonate cycle in the regulation and evolution of the Earth system

RIDGWELL, A, ZEEBE, R·2005·Earth and Planetary Science Letters

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Registry

Crossref · 10.1016/j.epsl.2005.03.006

Cites

126 of 126 references verified0 citation errors · 0 not checkable

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  • Deep-sea sediments are fundamental to how atmospheric CO2 concentration is regulated on timescales of thousands to tens of thousands of years.

    “The sediments of the deep-sea are fundamental to how the concentration of CO 2 in the atmosphere is regulated on timescales of thousands to tens of thousands of years (see Ridgwell and Zeebe [2005] for a review).”

    From Regulation of atmospheric CO <sub>2</sub> by deep‐sea sediments in an Earth system model (2007) · cites this paper as Ridgwell and Zeebe [2005]

  • At the global scale, the large-scale circulation of the ocean and water mass geochemistry dominates the CaCO3 content of deep-sea sediments.

    “In contrast, at the global scale, the large-scale circulation of the ocean and water mass geochemistry dominates [Ridgwell and Zeebe, 2005].”

    From Regulation of atmospheric CO <sub>2</sub> by deep‐sea sediments in an Earth system model (2007) · cites this paper as Ridgwell and Zeebe, 2005

  • The subsequent fate of this residual CO2 would be drawdown by silicate weathering feedback.

    “The subsequent fate of this residual CO 2 would be drawdown by silicate weathering feedback [Ridgwell and Zeebe, 2005].”

    From Regulation of atmospheric CO <sub>2</sub> by deep‐sea sediments in an Earth system model (2007) · cites this paper as Ridgwell and Zeebe, 2005

  • The size of the DIC reservoir was significantly larger in the Archaean than in the modern ocean.

    “there is nearly unanimous agreement that (i) the size of the DIC reservoir was significantly larger in the Archaean than in the modern ocean”

    From Iron formations: A global record of Neoarchaean to Palaeoproterozoic environmental history (2017) · cites this paper as Ridgwell and Zeebe, 2005

  • Proportionally more Fe(III) existed than organic carbon buried with IF precursor sediments relative to typical modern continental margin sediments.

    “(iii) proportionally more Fe(III) existed than organic carbon buried with IF precursor sediments relative to typical modern continental margin sediments”

    From Iron formations: A global record of Neoarchaean to Palaeoproterozoic environmental history (2017) · cites this paper as Ridgwell and Zeebe, 2005

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Authors
RIDGWELL, A., & ZEEBE, R.
Affiliations
  • University of British Columbia (CA)
  • University of Hawaiʻi at Mānoa (US)
Corresponding author
RIDGWELL, A
Venue
Earth and Planetary Science Letters
Publisher
Elsevier BV
Published
2005-06-15
Volume
234
Issue
3-4
Pages
299-315
ISSN
0012-821X (ISSN-L)
OpenAlex
W1967408071
Cited by
705
References
127
Citations by year
2026: 41 · 2025: 46 · 2024: 48 · 2023: 75 · 2022: 49 · 2021: 46 · 2020: 52 · 2019: 33 · 2018: 29 · 2017: 33 · 2016: 42 · 2015: 30 · 2014: 13 · 2013: 26 · 2012: 26
FWCI
14.67
Type
journal article
Language
en
Open access
closed
Locations
  • Earth and Planetary Science Letters (publishedVersion)
  • Explore Bristol Research (submittedVersion)
Funders
Canada Research Chairs
Topics
  • Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
  • Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Geology and Paleoclimatology Research
  • Physical Sciences › Earth and Planetary Sciences › Oceanography › Ocean Acidification Effects and Responses
Keywords
calcium carbonate, calcareous plankton, ocean acidification, atmospheric CO2, ocean carbon uptake, seawater carbonate chemistry, Earth system evolution, fossil fuel CO2 emissions

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