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Protracted development of bioturbation through the early Palaeozoic Era
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“although pervasive deep mixing of sediments would not be seen until well into the Paleozoic, more than 100 million years after the Ediacaran (Tarhan et al., 2015).”
From Oxygenation, Life, and the Planetary System during Earth's Middle History: An Overview (2021) · cites this paper as Tarhan et al., 2015
In the citing paper
“In any case, this hypothesis is largely irrelevant to our discussion, as biological mixing of sediments on marine shelves at the levels required to impact global-scale biogeochemical cycles was delayed well into the Paleozoic (likely at least the late Silurian)—hundreds of millions of years after our ∼800 Ma window (Tarhan et al., 2015).”
From Oxygenation, Life, and the Planetary System during Earth's Middle History: An Overview (2021) · cites this paper as Tarhan et al., 2015
Citations
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Metadata
- Authors
- Tarhan, L. G., Droser, M. L., Planavsky, N. J., & Johnston, D. T.
- Affiliations
- University of California, Riverside (US)
- Yale University (US)
- Harvard University (US)
- Corresponding author
- Tarhan, Lidya G.
- Venue
- Nature Geoscience
- Published
- 2015-09-28
- Volume
- 8
- Issue
- 11
- Pages
- 865-869
- ISSN
- 1752-0894 (ISSN-L)
- 1752-0908
- OpenAlex
- W2208461948
- Cited by
- 163
- References
- 41
- Citations by year
- 2026: 13 · 2025: 19 · 2024: 15 · 2023: 12 · 2022: 12 · 2021: 15 · 2020: 10 · 2019: 16 · 2018: 17 · 2017: 16 · 2016: 16 · 2015: 2
- FWCI
- 12.89
- Type
- journal article
- Language
- en
- Open access
- closed
- Licence
- www.springer.com/tdm (tdm)
- Locations
- Nature Geoscience (publishedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Physical Sciences › Earth and Planetary Sciences › Earth-Surface Processes › Geological formations and processes
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Evolutionary Biology
- Keywords
- bioturbation, Precambrian-Cambrian transition, Lower Paleozoic, sediment mixing, infauna, sulfur cycling, Great Ordovician Biodiversification Event, Cambrian explosion, taphonomy, ichnology
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