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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Africa
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North Africa
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Atlas Mountains
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Moroccan Atlas Mountains
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High Atlas (1)
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Morocco
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Moroccan Atlas Mountains
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High Atlas (1)
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Asia
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Far East
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China
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Guangxi China (1)
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Europe
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Central Europe
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Czech Republic
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Barrandian Basin (1)
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Western Europe
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United Kingdom
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Great Britain (1)
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fossils
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Invertebrata
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Arthropoda
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Trilobitomorpha
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Trilobita (1)
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Echinodermata
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Crinozoa
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Eocrinoidea (1)
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geologic age
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Paleozoic
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Cambrian
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Middle Cambrian (2)
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Upper Cambrian
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Furongian
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Paibian (1)
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Primary terms
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Africa
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North Africa
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Atlas Mountains
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Moroccan Atlas Mountains
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High Atlas (1)
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-
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Morocco
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Moroccan Atlas Mountains
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High Atlas (1)
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-
-
-
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Asia
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Far East
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China
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Guangxi China (1)
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-
-
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biogeography (1)
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Europe
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Central Europe
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Czech Republic
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Barrandian Basin (1)
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-
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Western Europe
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United Kingdom
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Great Britain (1)
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-
-
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Invertebrata
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Arthropoda
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Trilobitomorpha
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Trilobita (1)
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-
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Echinodermata
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Crinozoa
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Eocrinoidea (1)
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paleoecology (1)
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paleogeography (1)
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paleontology (1)
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Paleozoic
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Cambrian
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Middle Cambrian (2)
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Upper Cambrian
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Furongian
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Paibian (1)
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Ridersia
A new stemmed echinoderm from the Furongian of China and the origin of Glyptocystitida (Blastozoa, Echinodermata)
(a) Interpretation of the thecal plating in Ridersia watsonae from Furong...
Evolutionary implications of a new transitional blastozoan echinoderm from the middle Cambrian of the Czech Republic
Glyptocystitida and other related stemmed echinoderms. (a) Velieuxicystis ...
Stem Structure and Evolution in the Earliest Pelmatozoan Echinoderms
The first Furongian (late Cambrian) echinoderm from the British Isles
PHYLOGENETIC NOMENCLATURE AND PALEONTOLOGY
Cambrian echinoderm diversity and palaeobiogeography
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