The DOI matches its Crossref record; 126 of the 127 references it cites were found in a registry or an index.
The role of the global carbonate cycle in the regulation and evolution of the Earth system
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In the citing paper
“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 2 by deep‐sea sediments in an Earth system model (2007) · cites this paper as Ridgwell and Zeebe [2005]
In the citing paper
“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 2 by deep‐sea sediments in an Earth system model (2007) · cites this paper as Ridgwell and Zeebe, 2005
In the citing paper
“The subsequent fate of this residual CO 2 would be drawdown by silicate weathering feedback [Ridgwell and Zeebe, 2005].”
From Regulation of atmospheric CO 2 by deep‐sea sediments in an Earth system model (2007) · cites this paper as Ridgwell and Zeebe, 2005
In the citing paper
“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
In the citing paper
“(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
In the citing paper
“an estimated ten-fold greater size compared to that of the modern reservoir seems reasonable (Hotinski et al., 2004; Ridgwell and Zeebe, 2005; Higgins et al., 2009)”
From Iron formations: A global record of Neoarchaean to Palaeoproterozoic environmental history (2017) · cites this paper as Ridgwell and Zeebe, 2005
In the citing paper
“(ii) most IF precursor sediments were deposited in offshore environments with limited siliciclastic input and low sedimentation rates”
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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Metadata
- Authors
- RIDGWELL, A., & ZEEBE, R.
- Affiliations
- University of British Columbia (CA)
- University of Hawaiʻi at Mānoa (US)
- Corresponding author
- RIDGWELL, A
- ORCID
- 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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