Hydroclimate reconstruction through MIS 3 in the Middle Paleolithic site of Crvena Stijena (Montenegro) based on hydrogen-isotopic composition of sedimentary n-alkanes

Hydroclimate reconstruction through MIS 3 in the Middle Paleolithic site of Crvena Stijena (Montenegro) based on hydrogen-isotopic composition of sedimentary n-alkanes
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DOI:
10.1016/j.quascirev.2022.107771
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发表时间:
2022-11
影响因子:
4
通讯作者:
M. Jambrina‐Enríquez;C. Mallol;G. Tostevin;G. Monnier;Goran Pajović;Nikola Borovinić;Mile Baković
M. Jambrina‐Enríquez;C. Mallol;G. Tostevin;G. Monnier;Goran Pajović;Nikola Borovinić;Mile Baković
中科院分区:
地球科学1区
文献类型:
--
作者:
M. Jambrina‐Enríquez;C. Mallol;G. Tostevin;G. Monnier;Goran Pajović;Nikola Borovinić;Mile Baković

文献摘要

相似文献

本研究提出了一个水文气候重建Crvena斯蒂耶纳(黑山,巴尔干半岛的半岛),岩石庇护所,已产生的证据,旧石器时代中期人类占领。在7米深的垂直沉积序列中,脂质生物标志物,氢(δD)同位素组成的正构烷烃,和有机元素地球化学的整合,使重建的主要水文和环境变化期间的MIS 3和它们的相关性在现场。我们应用凝聚层次聚类和主成分分析的地球化学,分子和稳定同位素数据,以获得一个强大的水文记录。我们发现证据的三个干旱趋势的研究期间,其中之一与海因里希事件5,潮湿和冷温带条件下,考古丰富的层。我们的数据集还有助于了解过去的水文变化在巴尔干半岛的半岛,一个敏感的地区,短暂的气候变化,并在整个地中海地区在最后一次冰期/间冰期循环。
This study presents a hydroclimatic reconstruction from Crvena Stijena (Montenegro, Balkan Peninsula), a rock shelter that has yielded evidence for Middle Paleolithic human occupation. The integration of lipid biomarkers, hydrogen (δD) isotopic compositions ofn-alkanes, and organic elemental geochemistry in the 7-m deep vertical sedimentary sequence enables reconstruction of the main hydrological and environmental changes during the MIS 3 and their correlation with the presence at the site. We apply agglomerative hierarchical clustering and principal component analysis to the geochemical, molecular, and stable isotopic data to obtain a robust hydrological record. We find evidence of three aridity trends from the studied period, one of them correlated with the Heinrich Event 5, and humid and cold-temperate conditions in archaeology-rich layers. Our dataset also contributes to the knowledge of past hydrological variability in the Balkan Peninsula, a sensitive area to short-lived climatic shifts, and overall, in the Mediterranean region during the last glacial/interglacial cycle.