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Human settlement and Mid-Late Holocene coastal environmental change at Cape Krusenstern, Northwest Alaska

机译:阿拉斯加州西北部Krusenstern的人类住区和中期全新世沿海环境变化

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Archaeologists hypothesize that mid-late Holocene environmental variability played a role in several significant western Arctic cultural developments including population fluctuations, the evolution of Arctic maritime adaptations, and Arctic-wide migrations. Further evaluation of these hypotheses requires higher resolution archaeological and paleoecological datasets than are currently available. In response, we undertook an interdisciplinary study at Cape Krusenstern, a large coastal site complex in northwest Alaska, which was occupied over the last ca. 5000-6000 years. Our goals were to refine local cultural and paleoenvironmental chronologies and to explore the question of how local environmental change may have influenced local settlement history. The resulting revised chronology and depositional units confirm and refine prior interpretation of the local archaeological settlement history. New geomorphological data on coastal environmental change and post -depositional modification of the Cape Krusenstern beach ridge system also provide information about patterns of archaeological site preservation, indicating periods of potentially poorer site preservation around 3990 cal BP; this informs interpretation of forager settlement data. Furthermore, our findings suggest that climate-driven changes in the coastal environment at Cape Krusenstern may not be as determinative in terms of landscape evolution as previously thought. Future work should focus on further investigating the relationship between beach ridge development and regional climatic patterns on a regional scale, as this has implications for use of beach ridges as a mid-late Holocene climate proxy. Continued efforts to build paleoenvironmental reconstructions of higher temporal and spatial resolution for the region will help address remaining questions about the relationship between local coastal environmental changes and regional patterns, and the impacts of these environmental shifts on local residents.
机译:考古学家假设中期全新世环境变异率在几个重要的西北北极文化发展中发挥了作用,包括人口波动,北极海上适应的演变和北极迁徙。对这些假设的进一步评估需要更高的分辨率考古和古生态数据集,而不是目前可用的。作为回应,我们在阿拉斯加西北部大型沿海网站综合体中开展了跨学科研究,该公司在西北阿拉斯加西北部占据了最后一个CA。 5000-6000年。我们的目标是改进当地文化和古环境的时间表,并探讨当地环境变化如何影响当地解决历史的问题。由此产生的修订的年表和沉积单位确认并详述了对当地考古结算史的先前解释。关于沿海环境变化的新地貌数据和凯普·克鲁森斯特尔海滩山脊系统的职位修改还提供了有关考古场所保存模式的信息,表明3990 Cal BP左右潜在较差的场地保存期间;这通知了对Forager结算数据的解释。此外,我们的研究结果表明,克鲁森斯特人类沿海环境的气候驱动的变化可能在景观演变中的景观演变中可能并非如此以前认为的。未来的工作应该侧重于进一步调查海滩山脊开发与区域规模的区域气候模式的关系,因为这对使用海滩山脊作为中期全新世气候代理的影响。继续努力为该地区建造古环境重建的古环境和空间决议将有助于解决当地沿海环境变化与区域模式之间关系的剩余问题,以及这些环境转型对当地居民的影响。

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