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Behavioral and anatomical unity of the earliest burrowing animals and the cause of the “Cambrian explosion”
Abstract
All interpretable trace fossils from the Ediacarian–Cambrian transition strata of northern Siberia, Ukraine, and elsewhere represent shelters of infaunal animals feeding from the sediment surface. There is a gradation of forms ranging from (1) makers of horizontal galleries in soft sand with bilobed lower surface and proboscis extended to the surface, through (2) linear or zigzag series of short, widely U-shaped burrows in firm clay with bilobed or three-lobed lower surface, to (3) series of cylindrical chambers dug completely inside the sediment but opening to its surface. At the same time, protective skeleton originated in animals living above the sediment surface. Apparently, the diversification of predators in the earliest Cambrian forced other animals to invest energy either in digging or in a protective armor (“the Verdun Syndrome”). True mud-eaters appeared later, as documented by the late Tommotian horizontal spreite structures from central Siberia. Most, if not all, of those infaunal traces of activity were produced probably by relatives of priapulid worms. It appears that body cavities and segmentation in the Metazoa (diverse already in the Ediacarian) evolved independently of, and prior to, hydraulic burrowing.
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“the multi-tiered food webs that so typify the Phanerozoic were established with the eumetazoan invasion of both the pelagos and the infaunal benthos (Butterfield 1997, 2001; Vannier & Chen 2000, 2005; Dzik 2005; Peterson et al. 2005; Vannier et al. 2007).”
From The Ediacaran emergence of bilaterians: congruence between the genetic and the geological fossil records (2008) · cites this paper as Dzik 2005
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Metadata
- Authors
- Dzik, J.
- Affiliations
- Institute of Paleobiology (PL)
- Corresponding author
- Dzik, Jerzy
- ORCID
- Dzik, Jerzy
- Venue
- Paleobiology
- Publisher
- Cambridge University Press (CUP)
- Published
- 2005
- Volume
- 31
- Issue
- 3
- Pages
- 503-521
- ISSN
- 0094-8373 (ISSN-L)
- 1938-5331
- OpenAlex
- W2191553833
- Cited by
- 138
- References
- 9
- Citations by year
- 2026: 3 · 2025: 3 · 2024: 1 · 2023: 4 · 2022: 8 · 2021: 7 · 2020: 3 · 2019: 7 · 2018: 6 · 2017: 7 · 2016: 8 · 2015: 7 · 2014: 5 · 2013: 8 · 2012: 6
- FWCI
- 4.04
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Paleobiology (publishedVersion)
- BioOne Complete (BioOne) (submittedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Evolutionary Biology
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Evolution and Paleontology Studies
- Keywords
- Cambrian explosion, Ediacaran-Cambrian transition, trace fossils, burrowing behavior, infauna, priapulid worms, protective armor, Tommotian, segmentation, Ediacaran, early animal evolution
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