globalchange  > 过去全球变化的重建
DOI: 10.1016/j.palaeo.2012.10.041
论文题名:
Coastal-plain origin of trace-fossil bearing red beds in the Early Permian of Southern New Mexico, U.S.A.
作者: Voigt S.; Lucas S.G.; Krainer K.
刊名: Palaeogeography, Palaeoclimatology, Palaeoecology
ISSN: 0031-0182
出版年: 2013
卷: 369
起始页码: 323
结束页码: 334
语种: 英语
英文关键词: Coastal floodplain ; Continental ichnology ; Lagerstätte ; Late Paleozoic ; North America
英文摘要: The Early Permian Robledo Mountains Formation of the Hueco Group in the Robledo Mountains, south-central New Mexico, U.S.A., is a world-class ichnofossil Lagerstätte of supposed peritidal origin. Abundant and diverse invertebrate and vertebrate trace fossils occur in several thin horizons of siliciclastic red beds that are intercalated with thick successions of shallow marine limestone and shale. The depositional environment of the red beds has been discussed for decades but without any detailed sedimentary facies analysis. A recently completed systematic excavation shows that the majority of trace fossils is related to mud-draped surfaces within distal crevasse-splay siltstone to fine-grained sandstone. Interbedded mudstone with well-preserved macrofloral remains and a lungfish aestivation burrow represents a hitherto disregarded facies in overbank fines. Both environmental subzones were at least loosely covered with low-growing plants and experienced common periods of subaerial exposure. None of the physical and biological structures recorded in the measured section indicates tidal influence, but instead they support the reconstruction of a freshwater ecosystem dominated by arthropods and tetrapods. Given their proximity to carbonates of unambiguous subtidal origin, we propose that the trace-fossil-bearing red beds of the Robledo Mountains Formation formed in distal parts of an extensive coastal floodplain during alternating wet and dry conditions. If this interpretation is correct, it provides an impetus to continue ichnological and sedimentological field research in the study area, because the true tidal-flat ichnoguilds still await elucidation. © 2012 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/69887
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作者单位: Urweltmuseum GEOSKOP, Burg Lichtenberg (Pfalz), Burgstraße 19, D-66871 Thallichtenberg, Germany; New Mexico Museum of Natural History and Science, 1801 Mountain Road N.W., Albuquerque, New MEX 87104, United States; Institute of Geology and Paleontology, University of Innsbruck, Innsbruck A-6020, Austria

Recommended Citation:
Voigt S.,Lucas S.G.,Krainer K.. Coastal-plain origin of trace-fossil bearing red beds in the Early Permian of Southern New Mexico, U.S.A.[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2013-01-01,369
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