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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引用次数: 0
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.
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.