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Paleoindian environmental change and landscape response in Barger Gulch, Middle Park, Colorado

机译:科罗拉多州米德尔公园的巴格谷古环境变化与景观响应

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Middle Park, a high-altitude basin in the Southern Rocky Mountains of north-central Colorado, contains at least 59 known Paleoindian localities. At Barger Gulch Locality B, an extensive Folsom assemblage (similar to 10,500 C-14 yr B.P.) occurs within a buried soil. Radiocarbon ages of charcoal and soil organic matter, as well as stratigraphic positions of artifacts, indicate the soil is a composite of a truncated, latest-Pleistocene soil and a younger mollic epipedon formed between similar to 6000 and 5200 C-14 yr B.P and partially welded onto the older soil following erosion and truncation. Radiocarbon ages from an alluvial terrace adjacent to the excavation area indicate that erosion followed by aggradation occurred between similar to 10,200 and 9700 C-14 yr B.P, and that the erosion is likely related to truncation of the latest-Pleistocene soil. Erosion along the main axis of Barger Gulch occurring between similar to 10,000 and 9700 C-14 yr B.P was followed by rapid aggradation between similar to 9700 and 9550 C-14 yr B.P., which, along with the erosion at Locality B, coincides with the abrupt onset of monsoonal precipitation following cooling in the region similar to 11,000-10,000 C-14 yr B.P. during the Younger Dryas oscillation. Buried soils dated between similar to 9500 and 8000 C-14 yr B.P. indicate relative landscape stability and soil formation throughout Middle Park. Morphological characteristics displayed by early Holocene soils suggest pedogenesis under parkland vegetation in areas currently characterized by sagebrush steppe. The expansion of forest cover into lower elevations during the early Holocene may have resulted in lower productivity in regards to mammalian fauna, and may partly explain the abundance of early Paleoindian sites (similar to 11,000-10,000 C-14 yr B.P., 76%) relative to late Paleoindian sites (similar to 10,000-8000 C-14 yr B.P., 24%) documented in Middle Park. (c) 2005 Wiley Periodicals, Inc.
机译:中央公园是科罗拉多州中北部洛矶山脉南部的一个高海拔盆地,至少包含59个已知的古印第安人地区。在Barger Gulch地点B,埋藏的土壤中发生了广泛的Folsom组合(类似于10,500 C-14 yr B.P.)。木炭和土壤有机质的放射性碳年龄以及人工制品的地层位置表明,土壤是截断的,最新更新世的土壤和较年轻的分子表皮的复合物,其形成于6000至5200 C-14 yr BP之间,部分在侵蚀和截断之后焊接到较旧的土壤上。与开挖区相邻的冲积阶地的放射性碳年龄表明,侵蚀和随后的凝结发生在大约10,200和9700 C-14 yr B.P之间,并且该侵蚀很可能与最新更新世土壤的截断有关。沿Barger Gulch主轴的侵蚀发生在大约10,000和9700 C-14 yr BP之间,随后迅速凝结,类似于9700和9550 C-14 yr BP,这与位置B处的侵蚀相吻合。在类似于11,000-10,000 C-14 yr BP的区域降温后突然出现季风降水在年轻树妖的振荡期间。埋在土壤中的土壤大约在公元前9500年至8000年C-14年之间。表明整个中部公园的相对景观稳定性和土壤形成。全新世早期土壤显示的形态学特征表明,在目前以鼠尾草草原为特征的地区,公园植被下的成岩作用。全新世早期森林覆盖范围的扩展到较低的海拔可能导致哺乳动物区系的生产力降低,并且可能部分解释了早期古印第安人遗址的丰富性(类似于11,000-10,000 C-14 yr BP,76%)到中东公园记载的古印度晚期遗址(类似于10,000-8000 C-14 yr BP,占24%)。 (c)2005年Wiley Periodicals,Inc.

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