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14 - Pliocene–Pleistocene Water Bodies and Associated Deposits in Southern Israel and Southern Jordan

from Part II: - Palaeoclimates

Published online by Cambridge University Press:  04 May 2017

Yehouda Enzel
Affiliation:
Hebrew University of Jerusalem
Ofer Bar-Yosef
Affiliation:
Harvard University, Massachusetts
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Summary

Fine-grained, calcareous deposits associated with past water bodies are common features of arid environments worldwide. Distinguishing the hydrologic setting of these water bodies is crucial for reconstructing past climate and deducing the paleoecology of past human cultures that lived adjacent to them. In the southern Levant, fine-grained, calcareous, and often fossiliferous deposits have been used to infer large, shallow lakes during the Pleistocene. Here we assess the geologic evidence for three reported paleolakes on the southern Jordan Plateau: Wadi Hasa, Al Jafr Basin, and Mudawwara Basin. Based on the spatial distribution, sedimentological facies, and fossil assemblages of these deposits, we conclude that the water bodies in Wadi Hasa and Al Jafr Basin were formed by ground water discharging at the surface and maintaining wetland environments, not lakes. In Mudawwara, it is unclear if the deposits are associated with a former lake or wetland environments. The presence of wetland environments in the southern Levant indicates wetter conditions in the past, but they do not require the extreme changes in effective moisture needed to maintain large, shallow lakes.
Type
Chapter
Information
Quaternary of the Levant
Environments, Climate Change, and Humans
, pp. 127 - 134
Publisher: Cambridge University Press
Print publication year: 2017

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