Unveiling the Transition From Paleolake Lisan to Dead Sea Through the Analysis of Lake Paleoshorelines and Radiometric Dating of Fossil Stromatolites

IF 2.9 2区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Geochemistry Geophysics Geosystems Pub Date : 2024-08-05 DOI:10.1029/2024GC011541
Julius Jara-Muñoz, Amotz Agnon, Jens Fohlmeister, Sara Tomás, Jürgen Mey, Norbert Frank, Birgit Schröder, Andrea Schröder-Ritzrau, Yannick Garcin, Yaniv Darvasi, Daniel Melnick, Maria Mutti, Manfred R. Strecker
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Abstract

To date, the most complete paleolake-level reconstructions for the late Pleistocene water bodies that once occupied the Dead Sea depression have been based on the combination of dating of lake sediments and terrestrial materials. However, despite these major accomplishments, there is still limited spatial control regarding the water levels, suggesting some degree of uncertainty concerning the magnitude and rate of lake-level changes. Here, we re-examine the late Pleistocene lake-level changes in the Dead Sea during the transition from paleolake Lisan to the present-day Dead Sea. We rely on systematic dating of fossil stromatolites including 84 radiocarbon and 15 U-series ages, stable-isotope measurements, paleobiology, high-resolution topography, and numerical modeling to assess lake-level changes. Our results indicate that the highstand of paleolake Lisan was of shorter duration and the transition between Lake Lisan and the Dead Sea occurred at least 5 Kyrs earlier than previously indicated. By refining the timeline and accuracy of lake-level positions during the transition paleolake Lisan—Dead Sea, our study offers new insights into the regional and local paleo-climatic conditions during the last glacial period in this region.

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通过分析湖泊古海岸线和化石叠层石的辐射测定,揭示古湖利桑到死海的过渡过程
迄今为止,对曾经占据过死海洼地的晚更新世水体进行的最完整的古湖泊水位重建是基于对湖泊沉积物和陆地材料的测年相结合。然而,尽管取得了这些重大成就,有关水位的空间控制仍然有限,这表明湖泊水位变化的幅度和速度存在一定程度的不确定性。在此,我们重新研究了死海晚更新世从古湖利桑湖向今天的死海过渡期间的湖面变化。我们依靠对化石叠层石的系统测年(包括 84 个放射性碳年龄和 15 个 U 系列年龄)、稳定同位素测量、古生物学、高分辨率地形学和数值建模来评估湖面变化。我们的研究结果表明,古利山湖高地的持续时间较短,利山湖与死海之间的过渡至少比以前所指出的要早 5 个纪元。通过完善古湖里桑-死海过渡期间湖面位置的时间线和准确性,我们的研究为了解该地区末次冰川期的区域和地方古气候条件提供了新的视角。
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来源期刊
Geochemistry Geophysics Geosystems
Geochemistry Geophysics Geosystems 地学-地球化学与地球物理
CiteScore
5.90
自引率
11.40%
发文量
252
审稿时长
1 months
期刊介绍: Geochemistry, Geophysics, Geosystems (G3) publishes research papers on Earth and planetary processes with a focus on understanding the Earth as a system. Observational, experimental, and theoretical investigations of the solid Earth, hydrosphere, atmosphere, biosphere, and solar system at all spatial and temporal scales are welcome. Articles should be of broad interest, and interdisciplinary approaches are encouraged. Areas of interest for this peer-reviewed journal include, but are not limited to: The physics and chemistry of the Earth, including its structure, composition, physical properties, dynamics, and evolution Principles and applications of geochemical proxies to studies of Earth history The physical properties, composition, and temporal evolution of the Earth''s major reservoirs and the coupling between them The dynamics of geochemical and biogeochemical cycles at all spatial and temporal scales Physical and cosmochemical constraints on the composition, origin, and evolution of the Earth and other terrestrial planets The chemistry and physics of solar system materials that are relevant to the formation, evolution, and current state of the Earth and the planets Advances in modeling, observation, and experimentation that are of widespread interest in the geosciences.
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