Extensive marine anoxia during the terminal Ediacaran Period
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Summary
The results suggest that an expansion of oceanic anoxia and temporal-spatial redox heterogeneity, independent of other environmental and ecological factors, may have contributed to the decline of the Ediacara biota and may have also stimulated animal motility.
- Type
- article
- Published
- 2018-06-01
- Cited by
- 169
- References
- 115
- Access
- Open access
- OpenAlex
- https://openalex.org/W2809225447
- Semantic Scholar
- https://api.semanticscholar.org/CorpusID:49358738
Keywords
Biota, Period (music), Anoxic waters, Seafloor spreading, Geology
References
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- 238 U, 234 U and 232 Th in seawater
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- Uranium removal in oceanic sediments and the oceanic U balance
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- New distribution coefficient for the incorporation of strontium into dolomite and its implications for the formation of ancient dolomites
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- Low Mid-Proterozoic atmospheric oxygen levels and the delayed rise of animals
- The Sr, C and O isotopic evolution of Neoproterozoic seawater
- Distribution of trace elements between carbonate minerals and aqueous solutions
- Ediacaran δ13C chemostratigraphy of South China
- Uranium behavior in a permanently anoxic fjord : microbial control ?
Cited by
- Controls of eustasy and diagenesis on the 238U/235U of carbonates and evolution of the seawater (234U/238U) during the last 1.4 Myr
- Attenborites janeae: a new enigmatic organism from the Ediacara Member (Rawnsley Quartzite), South Australia
- Global-ocean redox variations across the Smithian-Spathian boundary linked to concurrent climatic and biotic changes
- Uranium isotope evidence for an expansion of anoxia in terminal Ediacaran oceans
- Integrated records of environmental change and evolution challenge the Cambrian Explosion
- Sedimentology and chemostratigraphy of the terminal Ediacaran Dengying Formation at the Gaojiashan section, South China
- Uranium isotope evidence for limited euxinia in mid-Proterozoic oceans
- Global marine redox changes drove the rise and fall of the Ediacara biota
- The Uranium Isotope Paleoredox Proxy
- Long-term evolution of terrestrial inputs from the Ediacaran to early Cambrian: Clues from Nd isotopes in shallow-marine carbonates, South China
- Early animal evolution and highly oxygenated seafloor niches hosted by microbial mats
- Surfing in and on microbial mats: Oxygen-related behavior of a terminal Ediacaran bilaterian animal
- Rare earth element geochemistry of Australian Neoproterozoic carbonate: Constraints on the Neoproterozoic oxygenation events
- Stretched, mangled, and torn: Responses of the Ediacaran fossil Dickinsonia to variable forces
- Increase in metazoan ecosystem engineering prior to the Ediacaran–Cambrian boundary in the Nama Group, Namibia
- Uranium isotopes as a proxy for primary depositional redox conditions in organic-rich marine systems
- Multiple S-isotopic constraints on paleo-redox and sulfate concentrations across the Ediacaran-Cambrian transition in South China
- Calcium isotopes as a record of the marine calcium cycle versus carbonate diagenesis during the late Ediacaran
- Spatial and temporal evolution of Ediacaran carbon and sulfur cycles in the Lower Yangtze Block, South China
- Examining pelagic carbonate-rich sediments as an archive for authigenic uranium and molybdenum isotopes using reductive cleaning and leaching experiments
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