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all geography including DSDP/ODP Sites and Legs
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Asia
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fossils
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Invertebrata
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Echinodermata
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Eocrinoidea (4)
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geologic age
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Paleozoic
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Cambrian
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Middle Cambrian
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Burgess Shale (1)
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Primary terms
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Asia
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Far East
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China
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Guizhou China (3)
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Yangtze Platform (1)
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Canada
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Western Canada
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British Columbia (1)
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Invertebrata
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Echinodermata
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Crinozoa
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Eocrinoidea (4)
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paleoecology (1)
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Paleozoic
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Cambrian
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Middle Cambrian
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Burgess Shale (1)
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GeoRef Categories
Era and Period
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Book Series
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Availability
Gogiida
A NEW TURBAN-SHAPED GOGIID EOCRINOID FROM THE KAILI FORMATION (KAILI BIOTA), BALANG, JIANHE COUNTY, GUIZHOU PROVINCE, CHINA Available to Purchase
Revision of Lyracystid Eocrinoids from the Middle Cambrian of South China and Western Laurentia Available to Purchase
Basal Middle Cambrian Short-Stalked Eocrinoids from the Kaili Biota: Guizhou Province, China Available to Purchase
New eocrinoids from the Burgess Shale, southern British Columbia, Canada, and the Spence Shale, northern Utah, USA Available to Purchase
Cambrian echinoderm diversity and palaeobiogeography Available to Purchase
Abstract The distribution of all known Cambrian echinoderm taxa, encompassing both articulated specimens and taxonomically diagnostic isolated ossicles, is documented for the first time. The database described by 2011 comprises 188 species recorded from 65 formations from around the world. Formations that have yielded articulated echinoderms are unequally distributed in space and time. Only Laurentia and West Gondwana provide reasonably complete records at the resolution of Stage. The review of the biogeographical distributions of the eight major echinoderm clades shows that faunas from Laurentia and Northeast Gondwana (China and Korea) are distinct from those of West Gondwana and Southeast Gondwana (Australia); other regions are too poorly sampled to make firm palaeobiogeographical statements. Analysis of alpha diversity (species per formation) shows that diversity rose initially to Cambrian Stage 5, declined into Guzhangian and Paibian before returning to Stage 5 levels by the end of the Cambrian. This pattern is replicated in Laurentia and West Gondwana. We show that taxonomically diagnostic ossicles found in isolation typically occur significantly earlier than the first articulated specimens of the same taxa and provide important information on the first occurrence and palaeobiogeographical distribution of key taxa, and of the phylum as a whole. Supplementary material: Articulated Cambrian echinoderms and Isolated plates of Cambrian echinoderms are provided at: http://www.geolsoc.org.uk/SUP18668