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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Europe
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Southern Europe
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Iberian Peninsula
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Portugal (1)
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Spain
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Aragon Spain
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Saragossa Spain (1)
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Castilla-La Mancha Spain
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Ciudad Real Spain (2)
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Iberian Mountains (1)
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Montes de Toledo (1)
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Sierra Morena (1)
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fossils
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Invertebrata
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Echinodermata
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Crinozoa
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Crinoidea (4)
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geologic age
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Paleozoic
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Devonian (1)
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Ordovician
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Middle Ordovician
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Llandeilian (1)
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Upper Ordovician
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Ashgillian (1)
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Silurian (1)
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Primary terms
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biogeography (1)
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Europe
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Southern Europe
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Iberian Peninsula
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Portugal (1)
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Spain
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Aragon Spain
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Saragossa Spain (1)
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Castilla-La Mancha Spain
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Ciudad Real Spain (2)
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Iberian Mountains (1)
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Montes de Toledo (1)
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Sierra Morena (1)
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-
-
-
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Invertebrata
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Echinodermata
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Crinozoa
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Crinoidea (4)
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-
-
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paleogeography (1)
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Paleozoic
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Devonian (1)
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Ordovician
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Middle Ordovician
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Llandeilian (1)
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Upper Ordovician
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Ashgillian (1)
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-
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Silurian (1)
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Heviacrinus melendezi
Table 7 —Measurements of Heviacrinus melendezi Gil Cid et al. (1996)
ORDOVICIAN [DOBROTIVIAN (LLANDEILLIAN STAGE) TO ASHGILL] CRINOIDS (PHYLUM ECHINODERMATA) FROM THE MONTES DE TOLEDO AND SIERRA MORENA, SPAIN WITH IMPLICATIONS FOR PALEOGEOGRAPHY OF PERI-GONDWANA
NEW AND REVISED OCCURRENCES OF ORDOVICIAN CRINOIDS FROM SOUTHWESTERN EUROPE
Filling the Gondwanan gap: paleobiogeographic implications of new crinoids from the Castillejo and Fombuena formations (Middle and Upper Ordovician, Iberian Chains, Spain)
Figure 8 —Aboral cup plate interpretations from camera lucida drawings. 1...
Figure 6 — 1, 2, Delgadocrinus oportovinum n. gen. and sp., paratype, MG...
Figure 5 —Spanish Ordovician crinoids; photographs of latex casts. 1, 2, ...
Figure 5 — 1–4, 6, 7, Delgadocrinus oportovinum n. gen. and sp., 1, pa...
Bayesian estimation of fossil phylogenies and the evolution of early to middle Paleozoic crinoids (Echinodermata)
Abstract Anomalocystitid mitrates represent one of the most diverse and long ranging clade of stylophorans (Early Ordovician–Middle Devonian). Although they probably originated from a peri-Gondwanan stock of early mitrocystitids during the Floian, the fossil record of anomalocystitids in the Middle–Upper Ordovician of the Mediterranean Province remains extremely scarce and largely underestimated. The unusually shaped anomalocystitid genus Diamphidiocystis was originally described in the latest Katian–Hirnantian of North America (Illinois). However, earlier occurrences of this genus in the late Darriwilian of western France (Brittany) suggest a probable peri-Gondwanan origin. Based on new Middle to Late Ordovician material from the Anti-Atlas (Morocco), Bohemia (Czech Republic) and Brittany (France), all occurrences of Mediterranean Diamphidiocystis are considered as conspecific and formally described as D. regnaulti sp. nov. The palaeobiogeographical significance of Ordovician anomalocystitid mitrates is discussed.
New Middle and Late Ordovician cornute stylophorans (Echinodermata) from Morocco and other peri-Gondwanan areas
Abstract Cornute stylophorans are a minor, although typical, component of Middle–Late Ordovician echinoderm assemblages adapted to soft siliciclastic substrates in high-latitude peri-Gondwanan regions. All previously reported occurrences of Darriwilian–Katian cornutes from the Czech Republic, France, Morocco and Spain are revised and their plate homologies reassessed. The genera Beryllia and Juliaecarpus are reinterpreted as junior synonyms of Domfrontia , and Thoralicystis is synonymized with Bohemiaecystis . Several Mediterranean scotiaecystids previously assigned to Bohemiaecystis and/or Scotiaecystis are placed within Thoralicarpus gen. nov., and cornute taxa originally left in open nomenclature by Chauvel are formally described as Bohemiaecystis chouberti sp. nov. (AVI) and Destombesicarpus izegguirenensis gen. et sp. nov. (AVIII). Other new Mediterranean taxa include Arauricystis clariondi sp. nov., Destombesicarpus budili gen. et sp. nov., Milonicystis reboulorum sp. nov., Thoralicarpus bounemrouensis gen. et sp. nov., and T . prokopi gen. et sp. nov. The six cornute genera identified in Darriwilian–Katian Moroccan echinoderm Lagerstätten are also present in coeval assemblages of at least one other Mediterranean region, thus supporting the existence of strong faunal affinities between the Anti-Atlas, the Armorican Massif, the Barrandian area and the Iberian Peninsula.