globalchange  > 气候变化与战略
DOI: 10.1016/j.earscirev.2018.12.011
论文题名:
Tetrapod ichnotaxonomy in eolian paleoenvironments (Coconino and De Chelly formations, Arizona) and late Cisuralian (Permian) sauropsid radiation
作者: Marchetti L.; Voigt S.; Lucas S.G.; Francischini H.; Dentzien-Dias P.; Sacchi R.; Mangiacotti M.; Scali S.; Gazzola A.; Ronchi A.; Millhouse A.
刊名: Earth Science Reviews
ISSN: 00128252
出版年: 2019
卷: 190
起始页码: 148
结束页码: 170
语种: 英语
中文关键词: Coconino ; Eolian ; Footprint taphonomy ; Permian ; Sauropsid radiation
英文关键词: amphibian ; eolian deposit ; footprint ; ichnology ; lizard ; paleoenvironment ; Permian ; taphonomy ; trackway ; Arizona ; Coconino Plateau ; United States ; Amphibia ; Podarcis muralis ; Sauria ; Sauropsida ; Synapsida ; Tetrapoda
英文摘要: The tetrapod footprint record of Permian eolian environments has long been underestimated because of overall poor preservation and its apparent monospecifity. The best known and most abundant Cisuralian record of tetrapod footprints is from the Coconino and De Chelly formations of Arizona, which, however, thus far encompassed only the ichnogenera Chelichnus and Dromopus. We revised the locomotion and taphonomy of these footprints and propose a new model, basing it on: 1) trackways changing direction, 2) trackways heading in different directions on the same surface, 3) trackways in situ, and 4) laboratory experiments with common wall lizards, Podarcis muralis. In all cases, the Chelichnus-like appearance of footprints is due to digit tip sliding on inclined depositional surfaces, masking the original footprint shape and orientation. Also, the trackway pattern and body position are largely influenced by the angle of inclination (dip) of the substrate being walked on. Based on an anatomy-consistent ichnotaxonomy, Chelichnus and Laoporus are here considered nomina dubia, and the footprints from the Coconino and De Chelly formations are revised and assigned to: parareptiles/captorhinomorph eureptiles (Erpetopus, Varanopus curvidactylus), bolosaurid parareptiles/ diapsid eureptiles (cf. Dromopus), varanopid synapsid (cf. Tambachichnium) and reptiliomorph amphibians (Amphisauropus, Ichniotherium sphaerodactylum). The ichnoassociation is dominated by parareptile/captorhinomorph tracks, similarly to all the late Cisuralian marginal marine, floodplain, alluvial fan and ephemeral lacustrine tetrapod ichnoassociations of North America, Europe and North Africa. A review of all the available data including the new results suggests a facies-crossing transition between an early-Cisuralian amphibian- and synapsid-dominated ichnofauna (Dromopus track biochron) and a late Cisuralian parareptile/captorhinomorph-dominated ichnofauna (Erpetopus track biochron) at low latitudes of Pangea. © 2018 Elsevier B.V.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/165876
Appears in Collections:气候变化与战略

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作者单位: Urweltmuseum GEOSKOP/Burg Lichtenberg (Pfalz), Burgstrasse 19, Thallichtenberg, 66871, Germany; New Mexico Museum of Natural History and Science, 1801 Mountain Road N.W., Albuquerque, NM 87104, United States; Laboratório de Paleontologia de Vertebrados, Instituto de Geociencias, Universidade Federal do Rio Grande do Sul, Porto Alegre, Rio Grande do Sul, Brazil; Laboratório de Geologia e Paleontologia, Instituto de Oceanografia, Universidade Federal do Rio Grande, Rio Grande, Rio Grande do Sul, Brazil; Dipartimento di Scienze della Terra e dell'Ambiente, Università di Pavia, Via Taramelli 24, Pavia, 27100, Italy; Museo Civico di Storia Naturale di Milano, Corso Venezia 55, Milano, 20121, Italy; Dipartimento di Scienze della Terra e dell'Ambiente, Università di Pavia, Via Ferrata 1, Pavia, 27100, Italy; Department of Paleobiology, Smithsonian Institution, National Museum of Natural History, 10th St. & Constitution Ave. NW, Washington, DC 20560, United States

Recommended Citation:
Marchetti L.,Voigt S.,Lucas S.G.,et al. Tetrapod ichnotaxonomy in eolian paleoenvironments (Coconino and De Chelly formations, Arizona) and late Cisuralian (Permian) sauropsid radiation[J]. Earth Science Reviews,2019-01-01,190
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