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首页> 外文期刊>Palaeogeography, Palaeoclimatology, Palaeoecology: An International Journal for the Geo-Sciences >A new Late Cretaceous (late Campanian to early Maastrichtian) wood flora from southern Patagonia
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A new Late Cretaceous (late Campanian to early Maastrichtian) wood flora from southern Patagonia

机译:来自巴塔哥尼亚南部的新白垩纪晚期(白垩纪至马斯特里赫特晚期)木材植物区系

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摘要

The Cerro Fortaleza Formation, in southernmost Patagonia (Argentina), contains a unique Late Cretaceous (Campanian) flora and fauna. This formation is characterized by lithified fluvial sands, overbank mud deposits, and paleosols deposited in fluvial, fluvial-palustrine, and coastal plain environments from the northeastern margin of the Austral (Magellanes) Basin. The overlying and underlying formations have been dated as Campanian and Maastrichtian, respectively. Therefore, the Cerro Fortaleza Formation putatively falls within the late Campanian-Maastrichtian. This formation is known for its diverse fauna including dinosaurs, fishes, and turtles. Furthermore, poorly preserved leaf impressions from indeterminate conifers and cycads have also been discovered but not yet described.
机译:位于巴塔哥尼亚(阿根廷)最南端的塞罗·福塔雷萨组(Cerro Fortaleza)包含独特的白垩纪晚期(加拿大)动植物群。该地层的特征是从澳大利亚(麦哲伦)盆地东北缘的河床,河床-河床和沿海平原环境中形成的河床状砂砾岩,滩涂淤泥和古土壤。上层地层和下层地层的年代分别是坎帕尼阶和马斯特里奇阶。因此,塞罗福塔莱萨组可能位于坎帕尼-马斯特里赫特晚期。这种形态以其多样化的动物群而闻名,包括恐龙,鱼类和乌龟。此外,还发现但未描述来自不确定的针叶树和苏铁的保存不佳的叶子印象。

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