Cited by 216Paleontology and Stratigraphy of FossilsGeology and Paleoclimatology ResearchEarth Systems and Cosmic Evolution

The DOI matches its Crossref record; 227 of the 227 references it cites were found in a registry or an index; none of the 132 sources its claims cite is checked for support yet.

Evolution of the Global Carbon Cycle and Climate Regulation on Earth

Open access

Abstract

The existence of stabilizing feedbacks within Earth's climate system is generally thought to be necessary for the persistence of liquid water and life. Over the course of Earth's history, Earth's atmospheric composition appears to have adjusted to the gradual increase in solar luminosity, resulting in persistently habitable surface temperatures. With limited exceptions, the Earth system has been observed to recover rapidly from pulsed climatic perturbations. Carbon dioxide (CO 2) regulation via negative feedbacks within the coupled global carbon‐silica cycles are classically viewed as the main processes giving rise to climate stability on Earth. Here we review the long‐term global carbon cycle budget, and how the processes modulating Earth's climate system have evolved over time. Specifically, we focus on the relative roles that shifts in carbon sources and sinks have played in driving long‐term changes in atmospheric pCO 2. We make the case that marine processes are an important component of the canonical silicate weathering feedback, and have played a much more important role in p CO 2 regulation than traditionally imagined. Notably, geochemical evidence indicate that the weathering of marine sediments and off‐axis basalt alteration act as major carbon sinks. However, this sink was potentially dampened during Earth's early history when oceans had higher levels of dissolved silicon (Si), iron (Fe), and magnesium (Mg), and instead likely fostered more extensive carbon recycling within the ocean‐atmosphere system via reverse weathering—that in turn acted to elevate ocean‐atmosphere CO 2 levels.

Overview

Integrity signals

Registry

Crossref · 10.1029/2018gb006061

Cites

227 of 227 references verified0 citation errors · 0 not checkable

Statistics

Nothing to recompute.

Verification

Claims the paper makes

84 Not checked yet · 54 Own interpretation · 44 No basis given · 4 Own result

Verify all 132 references — free account

Show all 117 claims

  • It may state two separate claims as one. 46
  • Probably not a substantial claim. 27
69 of 69
  • The authors state this as an assumption.

    All CO2 produced by methanogenesis in marine sediments is neutralized by silicate mineral dissolution.

    “and the assumption that all this CO 2 is neutralized through silicate mineral dissolution in marine sediments (Wallmann et al., 2008)”
  • The authors state this as an assumption.

    Careful assessment of detrital zircon age data can provide first-order insights into global continental magmatism and CO2 outgassing through time.

    “it is reasonable to assume that careful assessment of detrital zircon age-data may provide first order insights into global continental magmatism and CO 2 outgassing through time.”
  • The paper relies on this without support.

    The oceans remained anoxic through most of the Precambrian and possibly into the early Phanerozoic.

    “Further, the oceans appear to have remained anoxic through most of the Precambrian and potentially even in the early Phanerozoic.”
  • The paper relies on this without support.

    The Archean continental crust contained abundant iron carbonates.

    “Although there is strong evidence that the crust contained abundant Fe carbonates in the Archean-there is also abundant evidence for the deposition of Fe silicates (e.g., Johnson et al., 2018;Rasmussen et al., 2017) and Fe oxides (e.g., Bekker et al., 2014).”
  • The authors state this as an assumption.

    Rainwater is quantitatively neutralized by weathering in the water-rock mass balance model.

    “This model assumes quantitative neutralization of rainwater through weathering.”
  • The authors state this as an assumption.

    All infiltrating carbon dioxide is neutralized in the water-rock mass balance model.

    “New CO 2 input into the system is set at 10 Tmol yr -1 and all infiltrating CO 2 is assumed to be neutralized.”
6 of 6

Self-check

Percentages, sums and reported differences re-computed from the paper’s own numbers.

Each contradiction between two passages listed here was confirmed by an independent check.

1 of 1

Citations

Cites

Research works printed but not linked: 6

  1. Algeo T. J., 1995, Late Devonian oceanic anoxic events and biotic crises:“rooted” in the evolution of vascular land plants, GSA Today, 5, 45
  2. Dole S., 1964, Habitable planets for man
  3. Högbom A., 1894, On the probability of secular variations of atmospheric carbon dioxide (in Swedish), Svensk Kemisk Tidskrift, 6, 169
  4. Hoyle F., 1957, The black cloud, 26
  5. Krissansen‐Totton J., 2017, Constraining climate sensitivity and continental versus seafioor weathering using an inverse geological carbon cycle model, Nature, 8, 1
  6. Ronov A., 1990, Chemical composition of the Earth's crust and geochemical balance of main elements

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Metadata

Authors
Isson, T. T., Planavsky, N. J., Coogan, L. A., Stewart, E. M., Ague, J. J., Bolton, E. W., Zhang, S., McKenzie, N. R., & Kump, L. R.
Affiliations
  • Yale University (US)
  • University of Victoria (CA)
  • University of Hong Kong (HK)
  • Pennsylvania State University (US)
Corresponding author
  • Isson, T. T.
  • Planavsky, N. J.
Venue
Global Biogeochemical Cycles
Published
2020-01-31
Volume
34
Issue
2
ISSN
  • 0886-6236 (ISSN-L)
  • 1944-9224
OpenAlex
W2998006343
Cited by
216
References
227
Citations by year
2026: 32 · 2025: 42 · 2024: 40 · 2023: 44 · 2022: 23 · 2021: 27 · 2020: 8
FWCI
11.05
Type
journal article
Language
en
Open access
Locations
  • Global Biogeochemical Cycles (publishedVersion)
  • Research Commons (University of Waikato) (submittedVersion)
Funders
  • National Science Foundation (EAR‐1650329)
  • Heising-Simons Foundation
  • NASA Astrobiology Institute
  • National Aeronautics and Space Administration
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 › Environmental Science › Global and Planetary Change › Earth Systems and Cosmic Evolution
Keywords
carbon cycle, climate regulation, atmospheric pCO2, silicate weathering, basalt alteration, reverse weathering, carbon sink, carbon source, climate stability, early Earth, air-sea CO2 flux, dissolved silica, Earth system evolution

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