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Relevant bibliographies by topics / Fossil Pelmatozoa

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Academic literature on the topic 'Fossil Pelmatozoa'

Author: Grafiati

Published: 4 June 2021

Last updated: 31 July 2024

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Journal articles on the topic "Fossil Pelmatozoa"

1

ZAMORA, SAMUEL. "The first Furongian (late Cambrian) echinoderm from the British Isles." Geological Magazine 149, no. 5 (2012): 940–43. http://dx.doi.org/10.1017/s0016756812000350.

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AbstractFurongian (late Cambrian) echinoderms are extremely rare in the fossil record and only two previous reports have been described from the Paibian Stage worldwide. Here, the third occurrence of an echinoderm from the Paibian, and the first ever reported in the Furongian of Britain is presented. It is a primitive pelmatozoan which shows intermediate characteristics between eocrinoids with columnal-bearing stems and primitive glyptocystitid rhombiferans. The palaeobiogeographic affinities of Cambrian echinoderm faunas from Britain, eastern Avalonia, are shown to be with Gondwana.

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2

Zell, Paul D., and Roger J. Cuffey. "Early ordovician assemblages and their possible relation to communities and biofacies – with an example from the Nittany Dolomite of central Pennsylvania." Paleontological Society Special Publications 6 (1992): 327. http://dx.doi.org/10.1017/s247526220000887x.

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Historically, six Early Ordovician fossil-bearing facies have been recognized in North America, based on both their lithology and the most abundant types of fossils: the cryptalgal facies, cherty-carbonate - molluscan facies, thrombolite mound facies, sponge-algal mound facies, limestone-brachiopod facies, and graptolitic shale facies. However, complete or representative fossil assemblages characterizing these facies have not yet been defined. Paleogeographic controls on the distribution of these facies are primarily water depth and circulation; much of the North American continent exhibits a

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3

Martino, Ronald L. "Trace fossils from marginal marine facies of the Kanawha Formation (Middle Pennsylvanian), West Virginia." Journal of Paleontology 63, no. 4 (1989): 389–403. http://dx.doi.org/10.1017/s0022336000019648.

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Seven sedimentary facies have been identified in a 40-m-thick portion of the Kanawha Formation near Chelyan in southern West Virginia. Lithology, sedimentary and biogenic structures, body fossils, paleocurrent patterns, and facies geometry have been used to identify the following paleoenvironments: Facies 1, fluviodeltaic channels represented by thick, cross-stratified channel sandstone; Facies 2, crevasse splays and tidal creeks represented by thin, cross-stratified wedge and channel sandstone; Facies 3, coastal swamps and lakes represented by coal seat and carbonaceous shale; Facies 4, restr

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4

Brett, Carlton E., Heather A. Moffat, and Wendy L. Taylor. "Echinoderm taphonomy, taphofacies, and Lagerstätten." Paleontological Society Papers 3 (October 1997): 147–90. http://dx.doi.org/10.1017/s1089332600000243.

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Taphonomic study of echinoderms provides useful information on sedimentary conditions before, during, and after burial. Taphonomic studies of Recent echinoderms indicate that much skeletal disarticulation occurs within a few days after death. However, experiments also indicate that within a short period after death echinoderm carcasses remain rather resistant to disarticulation, and thus may be transported a considerable distance by currents; following periods of a few hours of decay, more delicate portions of echinoderm skeletons are readily disarticulated. Some skeletal modules (e.g., crinoi

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5

Poschmann, Markus. "Pelmatozoan “rooting grounds” from the Early Devonian (late Emsian) Heckelmann Mill Fossil-Lagerstätte (Lahn Syncline, Rhineland-Palatinate, SW-Germany): morphological, palaeoenvironmental and taphonomic aspects." PalZ 94, no. 2 (2019): 311–25. http://dx.doi.org/10.1007/s12542-019-00454-1.

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6

Ausich, William I., Chuck Ciampaglio, Alexander J. Fabian, and Jeremy R. Myers. "A Silurian (Homerian) pelmatozoan echinoderm fauna from west-central Ohio, USA." Journal of Paleontology, December 13, 2023, 1–22. http://dx.doi.org/10.1017/jpa.2023.74.

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Abstract A diverse echinoderm fauna lived in reef and non-reef Silurian facies of the upper Midwestern USA. However, these faunas are dominantly preserved in dolostones with moldic preservation, and fossils from dolostone facies have not been documented to the extent of Silurian crinoids in nondolostone strata. Herein, an echinoderm fauna is described from the dolostones of the Cedarville Member of the Laurel Limestone (Wenlock, Homerian) from the Pepcon Cement Quarry in west-central Ohio. The described fauna contains blastoids, hemicosmitoids, and crinoids, including Troosticrinus subcylindri

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Books on the topic "Fossil Pelmatozoa"

1

Simms, M. J. British Lower Jurassic crinoids. Palaeontographical Society, 1989.

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2

Donovan, S. K. Pelmatozoan columnals from the Ordovician of the British Isles. Palaeontographical Society, 1986.

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3

Donovan, S. K. Pelmatozoan columnals from the Ordovicianof the British Isles. Palaeontographical Society, 1986.

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