Cited by 279Geology and Paleoclimatology ResearchGeological and Geochemical AnalysisPaleontology and Stratigraphy of Fossils

Arc-continent collisions in the tropics set Earth’s climate state

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Macdonald, Francis A., Swanson-Hysell, Nicholas L., Park, Yuem, Lisiecki, Lorraine, Jagoutz, Oliver·2019·Science

Abstract

On multimillion-year time scales, Earth has experienced warm ice-free and cold glacial climates, but it is unknown whether transitions between these background climate states were the result of changes in carbon dioxide sources or sinks. Low-latitude arc-continent collisions are hypothesized to drive cooling by exhuming and eroding mafic and ultramafic rocks in the warm, wet tropics, thereby increasing Earth's potential to sequester carbon through chemical weathering. To better constrain global weatherability through time, the paleogeographic position of all major Phanerozoic arc-continent collisions was reconstructed and compared to the latitudinal distribution of ice sheets. This analysis reveals a strong correlation between the extent of glaciation and arc-continent collisions in the tropics. Earth's climate state is set primarily by global weatherability, which changes with the latitudinal distribution of arc-continent collisions.

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  • Similar feedback mechanisms between tectonic activity and climate are well documented in the Phanerozoic and likely occurred in the geological past.

    “Similar feedback mechanisms between tectonic activity and climate are well documented in the Phanerozoic rock record (e.g.Macdonald et al., 2019), so likely also occurred in the geological past.”

    From Secular change and the onset of plate tectonics on Earth (2020) · cites this paper as Macdonald et al., 2019

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Authors
Macdonald, F. A., Swanson-Hysell, N. L., Park, Y., Lisiecki, L., & Jagoutz, O.
Affiliations
  • University of California, Santa Barbara (US)
  • Department of Earth and Planetary Science, University of California, Berkeley, CA 94720, USA.
  • University of California, Berkeley (US)
  • Massachusetts Institute of Technology (US)
Corresponding author
Macdonald, Francis A.
Venue
Science
Published
2019-04-12
Volume
364
Issue
6436
Pages
181-184
ISSN
  • 0036-8075 (ISSN-L)
  • 1095-9203
OpenAlex
W2922233977
Cited by
279
References
219
Citations by year
2026: 30 · 2025: 41 · 2024: 31 · 2023: 45 · 2022: 51 · 2021: 33 · 2020: 37 · 2019: 11
FWCI
13.04
Type
journal article
Language
en
Open access
Locations
  • Science (publishedVersion)
  • PubMed (publishedVersion)
  • eScholarship (California Digital Library) (submittedVersion)
Topics
  • Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Geology and Paleoclimatology Research
  • Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
  • Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
Keywords
arc-continent collision, chemical weathering, carbon sequestration, glaciation, ice sheets, paleogeography, Phanerozoic, mafic-ultramafic rocks, exhumation, climate transition, carbon dioxide

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