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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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Anti-Atlas (2)
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High Atlas (2)
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Morocco
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Moroccan Atlas Mountains
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Anti-Atlas (2)
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High Atlas (2)
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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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Saragossa Spain (3)
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Iberian Mountains (7)
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United States
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Texas
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fossils
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ichnofossils (1)
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Invertebrata
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Arthropoda
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Mandibulata
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Crustacea
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Malacostraca
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Trilobitomorpha
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Echinodermata
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geologic age
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Cenozoic
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Tertiary
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Paleogene
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Eocene
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lower Eocene
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Ypresian (1)
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Paleozoic
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Cambrian
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Lancara Formation (1)
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Paibian (1)
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Wilberns Formation (1)
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Devonian
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Emsian (1)
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Ordovician
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Darriwilian (1)
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Silurian
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Lower Silurian
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Llandovery
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Telychian (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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Anti-Atlas (2)
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High Atlas (2)
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-
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Morocco
-
Moroccan Atlas Mountains
-
Anti-Atlas (2)
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High Atlas (2)
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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 (6)
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Canada
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Eastern Canada
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Quebec
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Anticosti Island (1)
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Western Canada
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British Columbia (1)
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-
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Cenozoic
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Tertiary
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Paleogene
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Eocene
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lower Eocene
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Ypresian (1)
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diagenesis (1)
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Europe
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Pyrenees
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Spanish Pyrenees (1)
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Southern Europe
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Iberian Peninsula
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Spain
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Aragon Spain
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Huesca Spain (1)
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Saragossa Spain (3)
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Teruel Spain (1)
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-
Cantabrian Mountains (2)
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Iberian Mountains (7)
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Spanish Pyrenees (1)
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-
-
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Western Europe
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France
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Central Massif
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Montagne Noire (1)
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Herault France (1)
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-
United Kingdom
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Great Britain
-
Scotland
-
Ayrshire Scotland
-
Girvan Scotland (1)
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-
-
-
-
-
-
ichnofossils (1)
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Invertebrata
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Arthropoda
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Mandibulata
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Crustacea
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Malacostraca
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Brachyura (1)
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Trilobitomorpha
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Trilobita (5)
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Echinodermata
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Crinozoa
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Crinoidea (2)
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Eocrinoidea (4)
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Echinozoa
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Cyclocystoidea (1)
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Edrioasteroidea (2)
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Homalozoa
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Stylophora (1)
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paleoecology (2)
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paleogeography (2)
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Paleozoic
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Cambrian
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Lancara Formation (1)
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Lower Cambrian (1)
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Middle Cambrian
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Burgess Shale (1)
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Upper Cambrian
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Furongian
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Paibian (1)
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Wilberns Formation (1)
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Devonian
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Lower Devonian
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Emsian (1)
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Ordovician
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Middle Ordovician
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Darriwilian (1)
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Silurian
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Lower Silurian
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Llandovery
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Telychian (1)
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sedimentary rocks
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clastic rocks
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mudstone (1)
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sedimentary structures
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secondary structures
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concretions (1)
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symposia (1)
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United States
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Texas
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McCulloch County Texas (1)
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sedimentary rocks
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sedimentary rocks
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clastic rocks
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mudstone (1)
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sedimentary structures
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sedimentary structures
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secondary structures
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concretions (1)
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A highly diverse dromioid crab assemblage (Decapoda, Brachyura) associated with pinnacle reefs in the lower Eocene of Spain
New rhenopyrgid edrioasteroids (Echinodermata) and their implications for taxonomy, functional morphology, and paleoecology
Stratigraphic and paleogeographic distributions of Devonian crinoids from Spain with description of new taxa from the Iberian Chains
QUANTITATIVE ANALYSIS OF REPAIRED AND UNREPAIRED DAMAGE TO TRILOBITES FROM THE CAMBRIAN (STAGE 4, DRUMIAN) IBERIAN CHAINS, NE SPAIN
Morphological assessment of the earliest paradoxidid trilobites (Cambrian Series 3) from Morocco and Spain
Progress in echinoderm paleobiology
The first Ordovician cyclocystoid (Echinodermata) from Gondwana and its morphology, paleoecology, taphonomy, and paleogeography
Filling the Gondwanan gap: paleobiogeographic implications of new crinoids from the Castillejo and Fombuena formations (Middle and Upper Ordovician, Iberian Chains, Spain)
A new stemmed echinoderm from the Furongian of China and the origin of Glyptocystitida (Blastozoa, Echinodermata)
A columnal-bearing eocrinoid from the Cambrian Burgess Shale (British Columbia, Canada)
New long-stemmed eocrinoid from the Furongian Point Peak Shale Member of the Wilberns Formation, central Texas
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