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367 results for “crinoid”

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zenodo32/100

FIGURE 11 in Early Miocene stalked crinoids (Echinodermata) from the southern Rhodanian basin (southeastern France). Paleoenvironments and taxonomy

FIGURE 11. Columnals and pluricolumnals of Metacrinus berthei from the Palais des Papes in Avignon (MHNL 20.062719). A–B: pluricolumnal from the distal stalk of a young individual, A: oblique view, B: side view; C: distal end of a noditaxis from distal stalk, oblique distal view showing the flat, slightly concave cryptosymplexial facet; D–E: distal nodal from a young individual, D: oblique proximal view, E: proximal symplexial facet; F: pentagonal internodal; G: nodal, proximal symplexial facet, close up of center showing inner crenularium with interpetaloid grooves; H: subcircular internodal; I–J: nodal, I: proximal symplexial facet, J: concave cryptosymplexial facet, oblique distal view; K–L: infranodal, convexe distal cryptosymplexial facet, L: close up of lumen filled in by secondary stereom. Scale bar equals 1 mm, except in L where it equals 0.1 mm.

opennotspecifiedOct 2021View details →
zenodo32/100

FIGURE 8 in Early Miocene stalked crinoids (Echinodermata) from the southern Rhodanian basin (southeastern France). Paleoenvironments and taxonomy

FIGURE 8. Type series of Metacrinus berthei from Les Angles (after Nicolas 1898 modified). The arrowhead indicates the break separating in two fragments the syntype 1 (A: fragment MRA 3.009.192; B: fragment UCBL-FSL 19099-1); C–D: isolated internodals, C: syntype 3 (MRA 3.009.194.1), D: syntype 4 (MRA 3.009.194.2); E: syntype 5 considered as lost, F: syntype 2 (UCBL-FSL 19099-2); ci: proximal fragments of cirri (3 to 4 cirrals) connected to the nodal, Nd: nodal. Scale bar equals 5 mm, except in C–D where it equals 4 mm.

opennotspecifiedOct 2021View details →
zenodo32/100

FIGURE 1 in Early Miocene stalked crinoids (Echinodermata) from the southern Rhodanian basin (southeastern France). Paleoenvironments and taxonomy

FIGURE 1. Miocene sites with stalked crinoids in western Paratethys area, and detailed locations within the Rhône-Provence Bay. Upper left: paleogeographic map (Al: Algeria, BR: Betic Ranges in Spain, Co: Corsica, It: northern Italy, H: Hungary, M: Malta, RP: Rhône-Provence Bay). Rhône-Provence Basin: schematic map with sites (1: Avignon, Palais des Papes; 2: Les Angles; 3: Pierre Longue; 4: Védène; 5: Picabrier, 6: St Rémy-de-Provence; 7: N.D. du Château; 8: Tarascon, 9: Beaucaire; 10: Vigne Gaste, 11: Le Barroux; 12: Entrechaux; A: presumed limit of the Miocene Rhône-Provence Bay, B: enveloppe of Burdigalian marine sediment outcrops, C: sites with stalked crinoids, D: main faults (D1: Nîmes fault, D2a: middle Durance fault, D2b: Aix fault, D3: Salon-Cavaillon fault), E: island or submarine shoal).

opennotspecifiedOct 2021View details →
zenodo32/100

FIGURE 10 in Early Miocene stalked crinoids (Echinodermata) from the southern Rhodanian basin (southeastern France). Paleoenvironments and taxonomy

FIGURE 10. Brachials of Metacrinus berthei from the Palais des Papes in Avignon (MHNL 20.062717). A–C: IBr1, A–B: distal facet, A: close up of marginal symplexial crenumarium, C: proximal muscular facet; D–E: IBr2, D: oblique distal view showing large pinnule socket (p), E: oblique proximal view showing synostosial facet; F: proximal IIIBr, distal muscular facet; G: IBr4, distal facet with growth lines marked by syzygial stereom; H: IBrax; I: free proximal IIBr, proximal facet; J: IBr5, proximal facet; K: free IBr3, distal facet; L: free IIIBr. Scale bar equals 1 mm.

opennotspecifiedOct 2021View details →
zenodo32/100

FIGURE 6 in Early Miocene stalked crinoids (Echinodermata) from the southern Rhodanian basin (southeastern France). Paleoenvironments and taxonomy

FIGURE 6. Variation in quantitative characters of Metacrinus berthei columnals in the main sites studied. N: number of measures, horizontal bar: variation range, vertical bar: mean, in red: nodals, in green: internodals.

opennotspecifiedOct 2021View details →
zenodo32/100

FIGURE 13 in Early Miocene stalked crinoids (Echinodermata) from the southern Rhodanian basin (southeastern France). Paleoenvironments and taxonomy

FIGURE 13. Variations in columnal general shape of Paraconocrinus rhodanicus n. sp. from the Palais des Papes in Avignon. See Fig. 2G–H for abbreviations. Values in mm, except for ratios.

opennotspecifiedOct 2021View details →
zenodo32/100

FIGURE 5 in Early Miocene stalked crinoids (Echinodermata) from the southern Rhodanian basin (southeastern France). Paleoenvironments and taxonomy

FIGURE 5. Variation in the general shape and size of isocrinid columnals of the two main isocrinid species from the different sites in the Rhône-Provence Bay. Entr.: Entrechaux, IN: internodals, N: nodals. The envelopes of points corresponding to the sites Picabrier and Avignon (Palais des Papes) are only figured (see Figs. 3 and 4), except for E. gastaldii from Avignon. Values in mm, except for ratios H/D.

opennotspecifiedOct 2021View details →
dryad32/100

Species diagnosis tables for: Crinoids from the Wooster Shale Member of the Cuyahoga Formation, Carboniferous (Mississippian, Tournaisian) of Northeastern Ohio

<p>Nine crinoids are described from the Wooster Shale Member of the Cuyahoga Formation from Wayne and Ashland counties, Ohio, USA. Identifiable elements of the fauna include five camerate crinoids, one flexible crinoid, and three other eucladid crinoids. Five new species are described, including <em>Cactocrinus</em> <em>woosterensis</em> n. sp., <em>Cusacrinus</em> <em>brushi</em> n. sp., <em>Agaricocrinus</em> <em>murphyi</em> n. sp., <em>Decadocrinus</em> <em>laevis</em> n. sp., and <em>Decadocrinus</em> <em>inordinatus</em> n. sp. Overall, the distribution of crinoid clades in the Wooster Shale is similar to that of the stratigraphically lower Meadville Shale Member of the Cuyahoga Formation, although less diverse and with only one species (<em>Cyathocrinites</em> <em>simplex</em>) in common. Many of the Wooster Shale crinoids are completely or partially preserved with siderite in either nodules or within siderite beds. These crinoids are commonly preserved in trauma postures, which is characteristic of burial in episodic high turbulence events. The paleoenvironments and taxa of the two Cuyahoga Formation crinoid faunas more closely resemble Viséan faunas in siliciclastic settings than typical carbonate faunas of the Tournaisian. Supplemental tables included here are species diagnostic tables listing characters for differentiating species in the following Mississippian crinoid (Phylum Echinodermata) genera: <em>Agaricocrinus</em>, <em>Cactocrinus</em>, <em>Cusacrinus</em>, and <em>Decadocrinus</em>. </p>

opencc-zeroApr 2023View details →
zenodo32/100

Crinoid

Species: unknown Collected from the Kaibab Limestone in Grand Canyon National Park. This fossil is in the collections at Grand Canyon National Park, Arizona. Learn about paleontology in the National Park Service: https://www.nps.gov/subjects/fossils/index.htm Learn more about Grand Canyon National Park's Centennial: https://www.nps.gov/grca/getinvolved/centennial.htm Source: Objaverse 1.0 / Sketchfab

opencc-by-nc-1.0May 2019View details →
dryad32/100

Data from: Early phylogeny of crinoids within the pelmatozoan clade

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publicSep 2016View details →
dryad32/100

Data from: Hierarchical controls on extinction selectivity across the diplobathrid crinoid phylogeny

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publicSep 2019View details →
dryad32/100

Data from: Phylogeny and evolutionary history of diplobathrid crinoids (Echinodermata)

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publicAug 2019View details →
dryad32/100

Data from: New crinoids from the Baltic region (Estonia): fossil tip-dating phylogenetics constrains the origin and Ordovician–Silurian diversification of the Flexibilia (Echinodermata)

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publicJul 2018View details →
dryad32/100

Data from: Kalana Lagerstatte crinoids: early Silurian (Llandovery) of central Estonia

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publicMar 2019View details →
dryad32/100

Data from: Crinoid assemblages from the Fort Payne Formation (late Osagean, early Viséan, Mississippian) from Kentucky, Tennessee, and Alabama

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publicJul 2014View details →
dryad32/100

Data from: Testing for escalation in Lower Mississippian camerate crinoids

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publicSep 2014View details →
dryad32/100

Data from: An echinoderm Lagerstätte from the Upper Ordovician (Katian), Ontario: taxonomic re-evaluation and description of new dicyclic camerate crinoids

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publicNov 2017View details →
dryad32/100

Data from: Disparid and hybocrinid crinoids (Echinodermata) from the Upper Ordovician (lower Katian) Brechin Lagerstätte of Ontario

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publicDec 2017View details →
dryad32/100

Data from: Camerate crinoids from the Nunn Member (Osagean) of the Lower Mississippian Lake Valley Formation, New Mexico

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publicNov 2012View details →
dryad32/100

Data from: Camerate and disparid crinoids from the late Kinderhookian Meadville Shale, Cuyahoga Formation of Ohio

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publicFeb 2012View details →

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