{"title":"Environmental history of the South Caspian Sea basin and its relation to the Siberian High dynamics since 14,000 years ago","authors":"Hadi Gerivani , Abdolmajid Naderi Beni , Suzanne A.G. Leroy , Hamid K.A. Lahijani","doi":"10.1016/j.margeo.2024.107356","DOIUrl":null,"url":null,"abstract":"<div><p>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.</p></div>","PeriodicalId":18229,"journal":{"name":"Marine Geology","volume":"475 ","pages":"Article 107356"},"PeriodicalIF":2.6000,"publicationDate":"2024-07-11","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Marine Geology","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0025322724001403","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}
引用次数: 0
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.
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.