Mantle buffering of the early oceans
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The Archean oceans were 'mantle buffered' by vigorous circulation of seawater via submarine hydrothermal systems.
“The Archean oceans were 'mantle buffered' (Veizer et al., 1982) by vigorous circulation of seawater via submarine hydrothermal systems.”
From Evolution of Sedimentary Rocks (2014) · cites this paper as Veizer et al., 1982
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- Authors
- Veizer, J., Compston, W., Hoefs, J., & Nielsen, H.
- Affiliations
- University of Ottawa (CA)
- Australian National University (AU)
- University of Göttingen (DE)
- Venue
- Naturwissenschaften
- Published
- 1982-04
- Volume
- 69
- Issue
- 4
- Pages
- 173-180
- ISSN
- 0028-1042 (ISSN-L)
- 1432-1904
- OpenAlex
- W2084340623
- Cited by
- 126
- References
- 71
- Citations by year
- 2024: 1 · 2023: 2 · 2021: 1 · 2019: 2 · 2018: 4 · 2017: 4 · 2016: 1 · 2015: 2 · 2014: 3 · 2013: 1 · 2012: 2
- FWCI
- 11.58
- Type
- journal article
- Language
- en
- Open access
- closed
- Licence
- www.springer.com/tdm (tdm)
- Locations
- Die Naturwissenschaften (publishedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
- Keywords
- Archean ocean, seawater composition, strontium isotopes, sulfur isotopes, oxygen isotopes, Early Proterozoic, atmospheric oxygenation, metallogeny, tectonics, sedimentology
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