The oldest evidence of bioturbation on Earth
Abstract
Research Article| May 01, 2012 The oldest evidence of bioturbation on Earth Vladimir Rogov; Vladimir Rogov Institute of Petroleum Geology and Geophysics, Koptyug Avenue 3, Novosibirsk 630090, Russia Search for other works by this author on: GSW Google Scholar Vasiliy Marusin; Vasiliy Marusin Institute of Petroleum Geology and Geophysics, Koptyug Avenue 3, Novosibirsk 630090, Russia Search for other works by this author on: GSW Google Scholar Natalia Bykova; Natalia Bykova Institute of Petroleum Geology and Geophysics, Koptyug Avenue 3, Novosibirsk 630090, Russia Search for other works by this author on: GSW Google Scholar Yuriy Goy; Yuriy Goy Institute of Petroleum Geology and Geophysics, Koptyug Avenue 3, Novosibirsk 630090, Russia Search for other works by this author on: GSW Google Scholar Konstantin Nagovitsin; Konstantin Nagovitsin Institute of Petroleum Geology and Geophysics, Koptyug Avenue 3, Novosibirsk 630090, Russia Search for other works by this author on: GSW Google Scholar Boris Kochnev; Boris Kochnev Institute of Petroleum Geology and Geophysics, Koptyug Avenue 3, Novosibirsk 630090, Russia Search for other works by this author on: GSW Google Scholar Galina Karlova; Galina Karlova Institute of Petroleum Geology and Geophysics, Koptyug Avenue 3, Novosibirsk 630090, Russia Search for other works by this author on: GSW Google Scholar Dmitriy Grazhdankin Dmitriy Grazhdankin Institute of Petroleum Geology and Geophysics, Koptyug Avenue 3, Novosibirsk 630090, Russia…
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Higher BIs indicated recently for the Ediacaran consist of serially repeated elements identical to problematic body fossils, arguing against a trace-fossil origin.
“Higher BIs have been indicated recently for the Ediacaran [23], but the illustrated structures consist of serially repeated elements, identical to those in problematic body fossils such as Helanoichnus , Palaeopascichnus and Shaanxilithes [24], arguing against a trace-fossil origin [25].”
From Decoupling of body-plan diversification and ecological structuring during the Ediacaran–Cambrian transition: evolutionary and geobiological feedbacks (2014) · cites this paper as [23]
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- Authors
- Rogov, V., Marusin, V., Bykova, N., Goy, Y., Nagovitsin, K., Kochnev, B., Karlova, G., & Grazhdankin, D.
- Affiliations
- Institute of Petroleum Geology and Geophysics (RU)
- ORCID
- Venue
- Geology
- Publisher
- Geological Society of America
- Published
- 2012-05
- Volume
- 40
- Issue
- 5
- Pages
- 395-398
- ISSN
- 0091-7613 (ISSN-L)
- 1943-2682
- OpenAlex
- W2099210656
- Cited by
- 110
- References
- 7
- Citations by year
- 2026: 1 · 2025: 5 · 2024: 4 · 2023: 7 · 2022: 5 · 2021: 7 · 2020: 6 · 2019: 4 · 2018: 8 · 2017: 8 · 2016: 13 · 2015: 13 · 2014: 9 · 2013: 14 · 2012: 6
- FWCI
- 9.99
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Geology (publishedVersion)
- Funders
- National Science Foundation
- National Geographic Society
- Russian Academy of Sciences
- 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 › Geology › Geological Studies and Exploration
- Keywords
- bioturbation, Precambrian, microbial mats, microbial communities, Precambrian sedimentary rocks, early life on Earth, Precambrian paleontology, Precambrian geology
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