Anoxic Sedimentation is a geological process denoting the deposition and accumulation of sediments under oxygen-depleted (anoxic) aquatic conditions, distinguished from other sedimentation processes by the absence of dissolved oxygen that inhibits organic matter degradation and promotes preservation of organic-rich facies in lacustrine and marine basins.
450
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Citations
1.5K
Authors
623
Institutions
Publications per year
2017–2026
81
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450
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1.5K
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- PB
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- GJ
7
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- LM
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Institutions
623
Centre National de la Recherche Scientifique
Paris, France
17 h-index
86 publications
4.2K citations
Utrecht University
Utrecht, The Netherlands
14 h-index
31 publications
1.5K citations
University of Leeds
Leeds, United Kingdom
12 h-index
22 publications
1.8K citations
Texas A&M University
College Station, United States
11 h-index
18 publications
2.7K citations
Yale University
New Haven, United States
11 h-index
22 publications
2.9K citations
United States Geological Survey
Reston, United States
10 h-index
15 publications
1.6K citations
Chinese Academy of Sciences
Beijing, China
8 h-index
24 publications
976 citations
ETH Zurich
Zurich, Switzerland
7 h-index
12 publications
2.3K citations
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- Geochimica et Cosmochimica Acta
22 publications · 4.3K citations
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- Palaeogeography Palaeoclimatology Palaeoecology
19 publications · 1.1K citations
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- Organic Geochemistry
18 publications · 2.4K citations
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- Marine Geology
16 publications · 2.7K citations
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- Limnology and Oceanography
15 publications · 1.8K citations
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