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首页> 外文期刊>Geodiversitas >Nouvelles faunes de rongeurs (Mammalia, Rodentia) d'?¢ge mioc?¨ne moyen en Languedoc-Roussillon (sud de la France) ; biostratigraphie et corr??lations
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Nouvelles faunes de rongeurs (Mammalia, Rodentia) d'?¢ge mioc?¨ne moyen en Languedoc-Roussillon (sud de la France) ; biostratigraphie et corr??lations

机译:朗格多克-鲁西永(法国南部)的中年新啮齿类动物(哺乳动物,啮齿类);生物地层学及其相关性

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The fossil mammal bearing localities Blanquat?¨re 3 (Roussillon; filling of a fissure in a karst) and Puisserguier (Languedoc; brackish to lake deposit) have provided Middle Miocene rodents that first allow correlating these sites to Blanquat?¨re 1 (Roussillon; older) and La Grenati?¨re (Languedoc; younger). Second, the occurrence of the genus Cricetodon in these newly discovered localities similarly allow revisiting the correlations already proposed with the well-known localities from the Lyon area, Vieux-Collonges and La Grive. Blanquat?¨re 3 and Puisserguier are older than La Grive, and Blanquat?¨re 3 is slightly older than Vieux-Collonges. The fossil bearing levels of Puisserguier is interstratified in a mainly marine succession ending with brackish to lake deposits, which includes the level of La Grenati?¨re. The onshore (Western B??ziers area) and off shore (Tramontane 1 drilling) data on the marine Miocene agree referring these deposits to the Serravallian stage, the uppermost marine levels belonging to zone NN9 (drill) and NN6 (onshore), the uppermost brackish to lake deposits cannot be younger that the Miocene deposits encountered by the drill. According to the new collected data on one side, and the Miocene chronostratigraphy, it can be hypothesized that Blanquat?¨re 3 is c. 15.5 Myr old and Puisserguier, c. 14 Myr.
机译:化石哺乳动物的产地为Blanquat?re 3(鲁西永;喀斯特裂隙中充满)和Puisserguier(朗格多克;微咸至湖泊沉积)提供了中新世啮齿动物,这些啮齿动物首先使这些地点与Blanquat?re 1(鲁西永)相关。 (年龄较大)和La Grenati?rére(朗格多克;年龄较小)。其次,在这些新近发现的地区, Cricetodon 属的出现同样使人们能够重新审视已经提出的与里昂地区著名的地区,维约-科隆日斯和La Grive的相关性。 Blanquat?re 3和Puisserguier比La Grive年龄大,而Blanquat?re 3比Vieux-Collonges略大。 Puisserguier的化石方位在主要是海相演替中错层,最后以微咸的湖沉积物为准,其中包括La Grenati?re的水平。海洋中新世的陆上(西B ?? ziers地区)和近海(Tramontane 1钻探)数据同意将这些沉积物称为Serravallian阶段,即属于NN9区(钻探)和NN6区(陆上)的最高海平面,钻探遇到的中新世沉积物最年轻的是湖相沉积物。根据一侧新收集的数据和中新世年代地层学,可以假设Blanquat?re 3是 c。 15.5 Myr old和Puisserguier, c。 14马币

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