首页> 外文期刊>Journal of Paleontology >CRUSTACEAN-BEARING CONTINENTAL DEPOSITS IN THE PETROLIA FORMATION (LEONARDIAN SERIES, LOWER PERMIAN) OF NORTH-CENTRAL TEXAS
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CRUSTACEAN-BEARING CONTINENTAL DEPOSITS IN THE PETROLIA FORMATION (LEONARDIAN SERIES, LOWER PERMIAN) OF NORTH-CENTRAL TEXAS

机译:得克萨斯州北部中部彼得罗里亚组含砾岩的陆相沉积(LEONARDIAN系列,下二叠统)

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摘要

Numerous pygocephalomorph crustaceans occur with conchostracans, plants, fishes, amphibians, and amniotes in the Petrolia Formation (Leonardian Series, Lower Permian) of Baylor and Archer counties, Texas. Two pygocephalomorph species are represented; Mamayocaris serendipitous, new species, by hundreds of specimens that appear to be molted exoskeletons, and Paulocaris schrami, new species, by only a few specimens. Mamayocaris has been reported previously from the Lower Permian of Texas and South Dakota and the Upper Carboniferous of Illinois; Paulocaris was previously known only from South America. Associated plant assemblages are dominated by conifers accompanied by other Early Permian and some Late Carboniferous elements. Accompanying vertebrate remains include aquatic to fully terrestrial forms with close taxonomic ties to genera or families recorded in Upper Carboniferous deposits. The fossils are preserved in local deposits of thin (<2 cm), lenticular to nodular beds of limestone and thin (<15 cm) intervals of dark-gray claystone. These deposits accumulated in abandoned, standing-water segments of suspended-load fluvial channels. The archaic nature of these plant and animal assemblages supports previous interpretations that the Permian Petrolia Formation contains paleoenvironmentally isolated biotic elements characteristic of the Carboniferous and underscores prior depictions of the assemblages as relictual.
机译:贝勒县和阿切尔县的彼得罗里亚组中的伴生链球菌, 植物,鱼类,两栖动物和羊膜动物都出现了许多pygocephalomorph甲壳类动物。 / sup>得克萨斯州。代表了两种小头畸形种类。 Mamayocaris 偶然出现的新物种,由成百上千个标本蜕皮骨骼的标本组成,而Paulocaris schrami,新物种, 仅由少数标本组成。 Mamayocaris以前曾在得克萨斯州和南达科他州的下二叠纪和伊利诺伊州的石炭纪的上 报道过; Paulocaris以前仅是南美地区的 。关联的植物组合以针叶树为主,并伴以其他早二叠世和一些晚期 石炭纪元素。伴随的脊椎动物遗骸包括 水生到完全陆生形式,与上石炭纪沉积物中的属或科具有紧密的分类学联系。 化石保存在当地薄的(<2 cm), 到球状灰岩的沉积物和薄的(<15 cm) 间隔的深灰色黏土沉积。这些沉积物在悬浮水河道的废弃的死水段中积累 。这些动植物组合的古本性 支持以前的解释,即二叠纪Petrolia 地层包含古环境隔离的生物元素 石炭纪和下划线特征。对组合的描述为

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  • 来源
    《Journal of Paleontology》 |2002年第3期|486-494|共9页
  • 作者单位

    Department of Paleobiology, National Museum of Natural History, Smithsonian Institution, Washington, D.C. 20560,|Deceased, Rodney M. Feldmann is the corresponding author;

    Department of Geology, Kent State University, Kent, OH 44242, ,;

    Texas Memorial Museum, Vertebrate Paleontology Lab, University of Texas at Austin, Austin 78758-4445,;

    Department of Paleobiology, National Museum of Natural History, Smithsonian Institution, Washington, D.C. 20560,;

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