The Earliest Annelids: Lower Cambrian Polychaetes from the Sirius Passet Lagerstätte, Peary Land, North Greenland
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Apart from the Phyllopod Bed of the Burgess Shale (Middle Cambrian) polychaete annelids are practically unknown from any of the Cambrian Lagerstätten. This is surprising both because their diversity in the Burgess Shale is considerable, while to date the Chengjiang Lagerstätte which is equally impressive in terms of faunal diversity has no reliable records of any annelids. Here we describe, on the basis of about 40 specimens, Phragmochaeta canicularis gen. et sp. nov. from the Lower Cambrian Sirius Passet Lagerstätte of Peary Land, North Greenland. This makes it by far the oldest known polychaete, with a likely age of lower to middle Atdabanian, The body consists of approximately 20 segments, each bearing notochaetae and neurochaetae. The former appeared to have formed a felt-like covering on the dorsum, whilst the neurochaetae projected obliquely to the longitudinal axis. Apart from minor differences in chaetal size at either end there is no other tagmosis. Details of the head are obscure, and presence of palps, tentacles and eyes are conjectural. Jaws appear to have been absent. The gut was straight, and flanked by massive longitudinal musculature. P. canicularis was evidently benthic, propelling itself on the neurochaetae, with the dorsal neurochaetae conferring protection. Its stratigraphic position and generalized appearance are consistent with P. canicularis being primitive, but the phylogenetic relationships within the polychaetes remain problematic, principally because of paucity of relevant morphological information.
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Annelida does not have undisputed biomineralized representatives during the Cambrian radiation.
“Annelida does not have undisputed biomineralized representatives during the Cambrian radiation (Conway Morris & Peel, 2008), but such problematic groups as hyolithelminths, hyoliths and halwaxiids may share that affinity (see Section 3 and remarks in online Appendix 1 at http://journals.cambridge.org/geo).”
From Chronology of early Cambrian biomineralization (2012) · cites this paper as Conway Morris & Peel, 2008
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- Authors
- Morris, S. C., & Peel, J. S.
- Affiliations
- University of Cambridge (GB)
- Uppsala University (SE)
- ORCID
- Peel, John S.
- Venue
- Acta Palaeontologica Polonica
- Publisher
- Polska Akademia Nauk Instytut Paleobiologii (Institute of Paleobiology, Polish Academy of Sciences)
- Published
- 2008-01
- Volume
- 53
- Issue
- 1
- Pages
- 137-148
- ISSN
- 0567-7920 (ISSN-L)
- OpenAlex
- W2095644294
- Cited by
- 104
- References
- 48
- Citations by year
- 2026: 2 · 2025: 3 · 2024: 3 · 2023: 4 · 2022: 3 · 2021: 4 · 2020: 3 · 2019: 6 · 2018: 3 · 2017: 6 · 2016: 5 · 2015: 15 · 2014: 10 · 2013: 10 · 2012: 4
- FWCI
- 5.58
- Type
- journal article
- Language
- en
- Open access
- gold
- doi.org
- Licence
- cc-by
- Locations
- Acta Palaeontologica Polonica (publishedVersion, cc-by)
- Department of Earth Sciences EPrints Repository (acceptedVersion)
- BioOne Complete (BioOne) (submittedVersion)
- Zenodo (CERN European Organization for Nuclear Research) (submittedVersion, public-domain)
- Funders
- Department of Earth Sciences, University of Cambridge
- Uppsala Universitet
- Nationale Geologiske Undersøgelser for Danmark og Grønland
- Topics
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Evolutionary Biology
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Evolution and Paleontology Studies
- Keywords
- Polychaeta, Annelida, new genus and species, Lower Cambrian, Atdabanian, Burgess Shale, Chengjiang Lagerstätte, setae, neurochaetae, notochaetae, benthic feeding
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