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Adaptive evolution in Paleozoic coiled cephalopods
Abstract
Coiled cephalopods constitute a major part of the Paleozoic nekton. They emerged in the Early Ordovician but nearly vanished in the Silurian. The Emsian appearance of ammonoids started a story of evolutionary success of coiled cephalopods, which lasted until the end-Permian extinction event. This story is investigated by using a taxonomic database of 1346 species of 253 genera of coiled nautiloids and 1114 genera of ammonoids. The per capita sampling diversities, the Van Valen metrics of origination and extinction, and the probabilities of origination and extinction were calculated at stage intervals. The outcome of these estimations largely reflects the known biotic events of the Paleozoic. The polyphyletic, iterative appearance of coiled cephalopods within this time frame is interpreted to be a process of adaptation to shell-crushing predatory pressure. The evolution of the diversity of coiled nautiloids and ammonoids is strongly correlated within the time intervals. Once established, assemblages of coiled cephalopods are related to changes in sea level. The general trends of decreasing mean (or background) origination and extinction rates during the Paleozoic are interpreted to reflect a successive stabilization of the coiled cephalopod assemblages. Different reproduction strategies in ammonoids and nautiloids apparently resulted in different modes of competition and morphological trends. Significant morphological trends toward a stronger ornamentation and a centrally posi…
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“For example, the occupation of the water columnbynektonic metazoans began already in the Cambrian (Rigby & Milsom 2000, Butterfield 2001), but the nekton became important only in the Silurian and even more so in the Devonian, at the cost of large planktonic organisms (Bambach 1999; Kröger 2005; Klug et al. 2010, 2015a; Dahl et al. 2011).”
From Palaeozoic evolution of animal mouthparts (2017) · cites this paper as Kröger 2005
In the citing paper
“Large paired injuries in Ordovician nautiloids might have been caused by shell-breaking predators including nautiloids and eurypterids (Kröger 2005), although the culprits are hard to pin down (Kröger 2005, 2011).”
From Palaeozoic evolution of animal mouthparts (2017) · cites this paper as Kröger 2005
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Kröger, B., Vinther, J., & Fuchs, D. (2011) · BioEssays · doi:10.1002/bies.201100001 · Cited by 327
Self-citationPalaeozoic evolution of animal mouthparts
Klug, C., Frey, L., Pohle, A., De Baets, K., & Korn, D. (2017) · Bulletin of Geosciences · doi:10.3140/bull.geosci.1648 · Cited by 54
Metadata
- Authors
- Kröger, B.
- Affiliations
- Museum für Naturkunde (DE)
- Corresponding author
- Kröger, Björn
- ORCID
- Kröger, Björn
- Venue
- Paleobiology
- Publisher
- Cambridge University Press (CUP)
- Published
- 2005-06
- Volume
- 31
- Issue
- 2
- Pages
- 253-268
- ISSN
- 0094-8373 (ISSN-L)
- 1938-5331
- OpenAlex
- W2172539587
- Cited by
- 59
- References
- 2
- Citations by year
- 2026: 2 · 2025: 2 · 2023: 2 · 2022: 4 · 2021: 5 · 2020: 1 · 2019: 8 · 2018: 1 · 2017: 2 · 2016: 1 · 2015: 8 · 2014: 2 · 2012: 4
- FWCI
- 1.42
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Paleobiology (publishedVersion)
- BioOne Complete (BioOne) (submittedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Evolution and Paleontology Studies
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Evolutionary Biology
- Keywords
- coiled cephalopods, Paleozoic, ammonoids, nautiloids, adaptive evolution, origination and extinction rates, sea-level change, siphuncle, shell ornamentation, reproductive strategies
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