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Tectonic forcing of late cenozoic climate.

Raymo, M. E., Ruddiman, W. F.·1992·Nature

DOI 10.1038/359117a0

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Authors: Raymo, M. E., & Ruddiman, W. F.
Affiliations: Massachusetts Institute of Technology (US)
University of Virginia (US)
ORCID: Raymo, M. E.
Venue: Nature
Publisher: Springer Science and Business Media LLC
Published: 1992-09
Volume: 359
Issue: 6391
Pages: 117-122
ISSN: 0028-0836 (ISSN-L)
1476-4687
DOI: 10.1038/359117a0
OpenAlex: W1999924690
Cited by: 2,341
References: 68
Citations by year: 2026: 97 · 2025: 111 · 2024: 130 · 2023: 140 · 2022: 130 · 2021: 126 · 2020: 114 · 2019: 86 · 2018: 107 · 2017: 80 · 2016: 81 · 2015: 77 · 2014: 82 · 2013: 89 · 2012: 65
FWCI: 20.69
Type: journal article
Language: en
Open access: closed
Licence: www.springer.com/tdm (tdm)
Locations: Nature (publishedVersion)
Topics: Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Geology and Paleoclimatology Research
Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
Physical Sciences › Environmental Science › Global and Planetary Change › Climate variability and models
Keywords: tectonic forcing, global cooling, Tibetan Plateau uplift, continental ice sheets, chemical weathering, atmospheric CO2 concentration, positive feedback, paleoclimate

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Tectonic forcing of late cenozoic climate.

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