Environmental history of the South Caspian Sea basin and its relation to the Siberian High dynamics since 14,000 years ago

IF 2.6 3区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY
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Abstract

The Caspian Sea (CS) is an endorheic basin located at the boundary of Asia and Europe, which has undergone remarkable environmental transformations since the late glacial period. Its present dimensions and oceanographic features are determined by a complex interaction between climatic change and tectonic processes. However, the link between past climatic variations, especially the dynamics of the Siberian High (SH), and the CS oceanographic characteristics remains poorly constrained, leading to uncertainty in projecting its future rapid changes. In this study, a 1.7 m sediment core from the 584 m of water depth at the eastern side of the southern CS was obtained to reconstruct the climatically-driven environmental changes in the CS region during the last 14,000 years. High-resolution XRF measurements and detailed sedimentological analyses were conducted on the core samples. The outcomes were then systematically compared with a diverse array of extant palaeoclimatological datasets from Central Asia and Europe, regions dominated by two pivotal climatic systems impacting the CS. The objective of this comparative analysis was to clarify the impact of the SH and to define its dynamic interaction with the Westerlies over the CS. It was demonstrated that the SH dynamics exerted a significant influence on the CS environment. When the SH was strong and expanded over a large area, precipitation occurred outside of the CS watershed area and led to sea-level fall. Conversely, when the SH expansion was confined to the CS catchment basin, precipitation over the basin and lower evaporation resulted in sea-level rise.

自 1.4 万年前以来南里海盆地的环境历史及其与西伯利亚高原动态的关系
里海(CS)是位于亚欧交界处的一个内流盆地,自冰川晚期以来经历了显著的环境变化。里海目前的面积和海洋学特征是由气候变化和构造过程之间复杂的相互作用决定的。然而,过去的气候变迁,特别是西伯利亚高原(SH)的动态变化,与 CS 海洋特征之间的联系仍未得到很好的解释,导致对其未来快速变化的预测存在不确定性。本研究从 CS 南部东侧水深 584 米处获取了 1.7 米的沉积物岩芯,以重建 CS 区域在过去 14,000 年中由气候驱动的环境变化。对岩心样本进行了高分辨率 XRF 测量和详细的沉积学分析。然后,将分析结果与中亚和欧洲的各种现存古气候学数据集进行了系统比较。比较分析的目的是阐明 SH 的影响,并确定其与西风在 CS 上的动态相互作用。结果表明,SH 的动态对 CS 环境产生了重大影响。当 SH 强大并向大面积扩张时,降水发生在 CS 流域之外,导致海平面下降。反之,当 SH 扩展范围仅限于 CS 集水盆地时,盆地上方的降水和较低的蒸发导致海平面上升。
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来源期刊
Marine Geology
Marine Geology 地学-地球科学综合
CiteScore
6.10
自引率
6.90%
发文量
175
审稿时长
21.9 weeks
期刊介绍: Marine Geology is the premier international journal on marine geological processes in the broadest sense. We seek papers that are comprehensive, interdisciplinary and synthetic that will be lasting contributions to the field. Although most papers are based on regional studies, they must demonstrate new findings of international significance. We accept papers on subjects as diverse as seafloor hydrothermal systems, beach dynamics, early diagenesis, microbiological studies in sediments, palaeoclimate studies and geophysical studies of the seabed. We encourage papers that address emerging new fields, for example the influence of anthropogenic processes on coastal/marine geology and coastal/marine geoarchaeology. We insist that the papers are concerned with the marine realm and that they deal with geology: with rocks, sediments, and physical and chemical processes affecting them. Papers should address scientific hypotheses: highly descriptive data compilations or papers that deal only with marine management and risk assessment should be submitted to other journals. Papers on laboratory or modelling studies must demonstrate direct relevance to marine processes or deposits. The primary criteria for acceptance of papers is that the science is of high quality, novel, significant, and of broad international interest.
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