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首页> 外文期刊>Geobios: Paleontologie, Stratigraphie, Paleoecologie >Taphonomy of Sheridan College Quarry 1, Buffalo, Wyoming: Implications for reconstructing historic dinosaur localities including Utterback's 1902-1910 Morrison dinosaur expeditions
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Taphonomy of Sheridan College Quarry 1, Buffalo, Wyoming: Implications for reconstructing historic dinosaur localities including Utterback's 1902-1910 Morrison dinosaur expeditions

机译:怀俄明州布法罗谢里登学院采石场1的音标:重建包括Utterback的1902-1910 Morrison恐龙探险在内的历史悠久的恐龙地区的意义

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The Upper Jurassic Morrison Formation has yielded some of the most important, voluminous and diverse dinosaur bonebeds in western North America, yet many of its historic sites were excavated during the celebrated period of vertebrate paleontology in western North America referred to as the first and second " Great Dinosaur Rush" (1870-1910s). Because of the large quantity of fossils collected during this era, a considerable amount of data pertaining to patterns of sedimentation, preservation, and paleoecology across broad portions of the Morrison Formation (and indeed many other Mesozoic and Cenozoic units) is still poorly understood. This paper critically re-evaluates the Sheridan College Quarry 1 dinosaur bonebed which lies along the western rim of the Powder River Basin in the region of localities excavated during Utterback's expeditions in the 1900s. Sedimentologically, the bonebed is interpreted as having been formed by episodic flooding events affecting the proximal floodplain depocenter of a meandering river system. Limited evidence of bone abrasion or rounding and progressive upsection changes in bone orientations suggest that minimal transport occurred, but that at least four episodes of overbank flooding resulted in the concentration and burial of attritional, time averaged vertebrate skeletal material that accumulated in topographic lows on the floodplain. Taphonomic analysis indicates that multiple unassociated to partially associated fossil elements excavated represent at least three taxa of sauropod dinosaurs, whereas isolated elements from the site indicate the presence of several other small vertebrate taxa. This work provides significant new information not only about the Sheridan College Quarry 1, but also about local sedimentary and taphonomic conditions that were likely influential to burial and preservation of other nearby Morrison dinosaur localities in the Big Horn Mountains, most notably those excavated during the famous Utterback expeditions. This study highlights the research potential in reconstructing lost data for historic dinosaur localities.
机译:上侏罗统莫里森组已形成了北美西部一些最重要,数量最多且种类繁多的恐龙骨床,但其许多历史遗迹是在北美西部脊椎动物古生物学的著名时期发掘的,被称为“第一和第二”大恐龙冲”(1870-1910年代)。由于在这个时代收集了大量的化石,关于莫里森地层(乃至许多其他中生代和新生代单元)的沉积,保存和古生态模式的大量数据仍然知之甚少。这篇论文对Sheridan College Quarry 1恐龙骨骼进行了重新评估,该恐龙骨骼位于1900年代Utterback探险期间发掘的地方,沿粉河盆地西缘的地方。在沉积学上,骨床被解释为由影响蜿蜒河流系统近端洪泛区沉积中心的突发性洪水事件形成。有限的证据表明,骨磨损或变圆以及骨骼方向逐渐上移改变表明发生了最小限度的运输,但是至少有四次溢洪泛滥导致了时间平均的耗损脊椎动物骨骼材料的集中和埋葬,这些材料积聚在海底地形的低处。洪泛区。音速谱分析表明,发掘出的多个未关联至部分关联的化石元素至少代表了蜥脚类恐龙的三个分类单元,而从该地点分离出的元素则表明存在其他几个小型脊椎动物分类单元。这项工作不仅提供了有关Sheridan College Quarry 1的重要新信息,而且还提供了可能影响大霍恩山附近其他莫里森恐龙地区的埋葬和保存的当地沉积和沉积条件,尤其是在乌特巴克远征队。这项研究突出了为历史悠久的恐龙地区重建丢失数据的研究潜力。

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