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首页> 外文期刊>Ameghiniana: Revista de la Asociacion Paleontologica Argentina >NEW BRACHIOPOD RECORDS AND CONSIDERATIONS ON THE TIVERTONIA-STREPTORHYNCHUS (MOSCOVIAN) AND COSTATULUMUSAMOSI (SAKMARIAN-ARTINSKIAN) FAUNAS FROM WESTERN ARGENTINA: THE KEY SECTIONS AT QUEBRADA AGUA DEL JAGüEL AND QUEBRADA SANTA ELENA REVISITED
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NEW BRACHIOPOD RECORDS AND CONSIDERATIONS ON THE TIVERTONIA-STREPTORHYNCHUS (MOSCOVIAN) AND COSTATULUMUSAMOSI (SAKMARIAN-ARTINSKIAN) FAUNAS FROM WESTERN ARGENTINA: THE KEY SECTIONS AT QUEBRADA AGUA DEL JAGüEL AND QUEBRADA SANTA ELENA REVISITED

机译:来自阿根廷西部的蕨类植物-链霉菌病(莫斯科人)和Costatulumusamosi(SAKMARIAN-ARTINSKIAN)Faunas的新腕足动物记录和注意事项:QUEBRADA AGUA DELJAGüEL和QUEBRADA SANTA ELENA REVIS的关键部分

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摘要

The brachiopod Coolkilella aredesi sp. nov. and Calytrixia piersoni sp. nov. are proposed on the basis of specimens from the Del Salto, Rio del Pe?ón and Agua del Jagiiel formations. Their biostratigraphic implications are discussed together with new records of Septosyringothyris (Precosyringothyris) jaguelensis Lech and Streptorhynchus inaequiornatus Leanza at the top of the latter unit. The stratigraphic record, paleontological content and age of both the Tivertonia-Streptorhynchus assemblage (Moscovian) and the younger Costatumulus amosi fauna (Sakmarian-Artinskian) were reviewed and assessed based on outcrops at Quebrada Agua del Jagüel and Quebrada Santa Elena. Faunal content confirms the most recent stratigraphic, biostratigraphic and paleoclimatic frameworks. These recognize a diachronic nature of the Agua del Jagiiel and Cordón del Jagüel formations, supporting the absence of an early Permian glacial event in western Argentina.
机译:腕足类Coolkilella aredesi sp.。十一月和Calytrixia piersoni sp。十一月是根据Del Salto,Rio del Pe?ón和Agua del Jagiiel地层的标本提出的。讨论了它们的生物地层学意义,并在后一单元的顶部记录了琼脂Sep(Septosyringothyris)jaguelensis Lech和Streptorhynchus inaequiornatus Leanza的新记录。根据Quebrada Agua delJagüel和Quebrada Santa Elena的露头,回顾并评估了Tivertonia-Streptorhynchus组合(莫斯科)和较年轻的Costatumulus amosi动物群(Sakmarian-Artinskian)的地层记录,古生物学内容和年龄。动物的内容证实了最新的地层,生物地层和古气候框架。这些认识到Agua del Jagiiel和CordóndelJagüel地层具有历时性,这表明阿根廷西部没有早期的二叠纪冰川事件。

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