A Stratified Redox Model for the Ediacaran Ocean
By Chao Li, G. Love, T. Lyons, D. Fike, A. Sessions, X. Chu. Science, 2010
633 citations recorded by the source corpus.
Subfields: Astronomy and Astrophysics, Radiation
View Paper: https://www.semanticscholar.org/paper/0e3a8b4bfb30eec0d014d19802b589a8e789d873
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In Astronomy and Astrophysics
Citations in the corpus
- Mechanisms of Microbial Carbon Sequestration in the Ocean - Future Research Directions (2014, background): “It is likely that the great glaciations set up a lateral gradient of oxidants in the postglacial oceans (Li et al., 2010), which not only favored an intensive anaerobic MCP in shallow subsurface waters, but also created an extremely reduced deep ocean for storage of the resulting RDOC; these…”
- Late Ediacaran redox stability and metazoan evolution (2012, background): “Correlations among these basins and their stratigraphic successions are challenging, and the postulated role of sulfide as a key toxin in basins developed along the continental margin of the South China craton further complicates physiological interpretations (Li et al., 2010).”
- The Weng'an biota and the Ediacaran radiation of multicellular eukaryotes (2014, background): “depositional environment implies that the Weng’an biota was likely preserved beneath oxic marine waters, despite the frequent occurrence of euxinic or ferruginous anoxia in deeper water or restricted environments, such as shelf lagoon, slope, and basinal facies [86, 97, 101-104].”
- Remarkable insights into the paleoecology of the Avalonian Ediacaran macrobiota (2015, positive): “In several areas, basin transects through early- and middle-Ediacaran successions reveal oxic surface waters in some basins underlain by a euxinicwedge on the continental shelf, with ferruginous (anoxic) conditions in the deep oceans (cf. Li et al., 2010).”