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Caryosyntrips: a radiodontan from the Cambrian of Spain, USA and Canada

Abstract:

Caryosyntrips appendages have previously been reported from the Burgess Shale (Cambrian, Stage 5), British Columbia, Canada. New specimens of the genus are here reported from the Wheeler Formation (Cambrian, Drumian) and Langston Formation, Spence Shale Member (Cambrian, Stage 5), Utah, USA. The original Burgess Shale specimens are re-examined alongside the new specimens. Caryosyntrips is shown to have paired ventral spines on each podomere. Three species of Caryosyntrips are recognised:...

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Publication status:
Published
Peer review status:
Peer reviewed

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    APA Style

    Pates, S., & Daley, A. (2017). Caryosyntrips: a radiodontan from the Cambrian of Spain, USA and Canada. Papers in Palaeontology, 3(3), 461–470.

    MLA Style

    Pates, S., and A. Daley. “Caryosyntrips: a Radiodontan from the Cambrian of Spain, USA and Canada.” Papers in Palaeontology, vol. 3, no. 3, Wiley, 2017, pp. 461–70.

    Chicago Style

    Pates, S, and A Daley. 2017. “Caryosyntrips: a Radiodontan from the Cambrian of Spain, USA and Canada.” Papers in Palaeontology 3 (3): 461–70.
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10.1002/spp2.1084

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Authors


More by this author
Institution:
University of Oxford
Oxford college:
St Catherine's College
Role:
Author
More from this funder
Funding agency for:
Pates, S
Grant:
Brade-Natural Motion Scholarship
More from this funder
Funding agency for:
Pates, S
Grant:
Brade-Natural Motion Scholarship
More from this funder
Funding agency for:
Pates, S
Grant:
Brade-Natural Motion Scholarship
Publisher:
Wiley
Journal:
Papers in PalaeontologyMore from this journal
Volume:
3
Issue:
3
Pages:
461–470
Publication date:
2017-08-01
Acceptance date:
2017-06-01
DOI:
ISSN:
2056-2802
Keywords:
Pubs id:
pubs:698519
UUID:
uuid:2e8264d8-6b2b-4851-81f6-a0d3e57f3db0
Local pid:
pubs:698519
Source identifiers:
698519
Deposit date:
2017-06-05

Terms of use


Copyright holder:
The Palaeontological Association
Copyright date:
2017
Notes:
Copyright © 2017 The Palaeontological Association. This is the accepted manuscript version of the article. The final version is available online from Wiley at: https://doi.org/10.1002/spp2.1084
Licence:
Terms and Conditions of Use for Oxford University Research Archive

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