首页> 外文期刊>Palaeogeography, Palaeoclimatology, Palaeoecology: An International Journal for the Geo-Sciences >A loess record of pre-Late Wisconsin glacial outburst flooding, Pleistocene paleoenvironment, and Irvingtonian fauna from the Rulo site, southeastern Washington, USA
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A loess record of pre-Late Wisconsin glacial outburst flooding, Pleistocene paleoenvironment, and Irvingtonian fauna from the Rulo site, southeastern Washington, USA

机译:美国威斯康星州晚鲁斯冰川爆发洪水,更新世古环境和爱尔文顿时期动物区系的黄土记录

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摘要

Worldwide, loess-paleosol sequences are archives of terrestrial Quaternary paleoenvironment data. The Rulo site is a newly described site in the Palouse loess of southeastern Washington State, USA. The site reveals a 19 m thick deposit of loess and flood sediment, preserving a total of 30 m of reconstructed stratigraphic section. Five unconformity-bound sequences of sediment are exposed at the site, the lowest two of which have yielded fossil remains, including the first reported occurrence of flat-headed peccary (Platygonus compressus) in northwestern North America. The unconformities, two diamicts bearing extrabasinal clasts, and a number of clastic dikes provide evidence for pre-Wisconsin glacial outburst floods in southeastern Washington. More than a dozen paleosols are preserved at the site. These soils are relatively unweathered and therefore primarily record periods of slow sedimentation accumulation in the Palouse, rather than changes in weathering rates. A paleosol near the base of the sequence is unusually weathered for Palouse paleosols, and records a period of increased weathering during the Middle Pleistocene. All units above the sand are normal paleomagnetic polarity; additional age control is provided by a tephra in the upper third of the sequence that matches a ca. 220 ka tephra from Newberry Volcano, and by stratigraphic correlation of later units to other sites in the Palouse. The Rulo site adds to the record of Irvingtonian fauna in North America, and supports accumulating evidence for pre-Late Wisconsin glacial outburst floods in the Pacific Northwest. (C) 2016 Elsevier B.V. All rights reserved.
机译:在世界范围内,黄土-古土壤序列是陆地第四纪古环境数据的档案。 Rulo站点是美国华盛顿州东南部Palouse黄土中的一个新描述站点。该地点发现了一个19 m厚的黄土和洪水沉积物,总共保留了30 m的重建地层剖面。在该地点暴露了五个不整合面约束的沉积物序列,其中最低的两个序列已产生化石残留物,包括在北美西北部首次报道的平头野猪(Platygonus compressus)。不整合面,两个带有基底外岩屑的破土amic虫和许多碎屑堤坝为华盛顿东南部的威斯康星州前冰川爆发洪水提供了证据。该地点保存了十几种古土壤。这些土壤是相对未风化的,因此主要记录了帕卢斯沉淀沉积缓慢的时期,而不是风化速率的变化。序列底部附近的古土壤对帕卢斯古土壤异常地风化,并记录了中更新世期间风化增加的时期。沙子上方的所有单位都是正常的古磁极性。在与ca匹配的序列的前三分之一中,由特非拉提供额外的年龄控制。来自纽伯里火山(Newberry Volcano)的220 ka tephra,以及后来的单位与帕卢斯其他地点的地层学联系。 Rulo站点增加了北美洲Irvingtonian动物群的记录,并为西北太平洋地区威斯康星州晚期冰川爆发洪水的证据积累提供了支持。 (C)2016 Elsevier B.V.保留所有权利。

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