Rare-earth elements in seawater near hydrothermal vents
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Europium enrichment in chemical sedimentary rocks that precipitated from seawater indicates a strong influence of high-temperature hydrothermal fluids on the seawater dissolved REE+Y load.
“Europium enrichment in chemical sedimentary rocks that precipitated from seawater indicates a strong influence of high-temperature hydrothermal fluids on the seawater dissolved REE+Y load (e.g., Klinkhammer et al., 1983; Derry and Jacobsen, 1988, 1990; Bau and Dulski, 1996; Viehmann et al., 2015).”
From Iron formations: A global record of Neoarchaean to Palaeoproterozoic environmental history (2017) · cites this paper as Klinkhammer et al., 1983
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- Authors
- Klinkhammer, G., Elderfield, H., & Hudson, A.
- Affiliations
- University of Leeds (GB)
- University of Rhode Island (US)
- Venue
- Nature
- Published
- 1983-09
- Volume
- 305
- Issue
- 5931
- Pages
- 185-188
- ISSN
- 0028-0836 (ISSN-L)
- 1476-4687
- OpenAlex
- W1996138242
- Cited by
- 309
- References
- 23
- Citations by year
- 2026: 4 · 2025: 8 · 2024: 13 · 2023: 3 · 2022: 5 · 2021: 10 · 2020: 5 · 2019: 11 · 2018: 19 · 2017: 10 · 2016: 5 · 2015: 12 · 2014: 4 · 2013: 7 · 2012: 3
- FWCI
- 14.48
- Type
- journal article
- Language
- en
- Open access
- closed
- Licence
- www.springer.com/tdm (tdm)
- Locations
- Nature (publishedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Physical Sciences › Earth and Planetary Sciences › Geology › Geological and Geophysical Studies
- Keywords
- rare earth elements, seawater geochemistry, hydrothermal vents, cerium anomaly, deep Pacific Ocean, hydrothermal plumes, metalliferous sediments
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