E
Elisa J. Kagan
Researcher at Hebrew University of Jerusalem
Publications - 16
Citations - 721
Elisa J. Kagan is an academic researcher from Hebrew University of Jerusalem. The author has contributed to research in topics: Radiocarbon dating & Bronze Age. The author has an hindex of 12, co-authored 16 publications receiving 641 citations. Previous affiliations of Elisa J. Kagan include Tel Aviv University.
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Palynology, sedimentology and palaeoecology of the late Holocene Dead Sea
TL;DR: Palynological and sedimentological studies were performed at two Holocene profiles in erosion gullies (Ze’elim and Ein Feshkha) which dissect the retreating western shore of the Dead Sea as mentioned in this paper.
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Dating large infrequent earthquakes by damaged cave deposits
TL;DR: In this article, the authors presented a rigorously dated record of earthquakes from an extensive number of well-preserved pre- seismic and postseismic precipitates from caves located off the Dead Sea transform.
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Dead Sea pollen record and history of human activity in the Judean Highlands (Israel) from the Intermediate Bronze into the Iron Ages (∼2500–500 BCE)
Dafna Langgut,Frank H. Neumann,Frank H. Neumann,Mordechai Stein,Allon Wagner,Elisa J. Kagan,Elisa J. Kagan,Elisabetta Boaretto,Israel Finkelstein +8 more
TL;DR: A detailed pollen record for the time interval of ∼2500-500 BCE, which covers the time period of the Intermediate Bronze Age (Early Bronze Age IV) into the Iron Ages in the Levant, is presented in this paper.
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Sea-land paleoclimate correlation in the Eastern Mediterranean region during the late Holocene
TL;DR: In this paper, a link between land and marine isotopic records is established, which can be considered reliable recorders of the climatic conditions that prevailed in the land-locked Eastern Mediterranean region during the late Holocene.
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Vegetation history and climate fluctuations on a transect along the Dead Sea west shore and their impact on past societies over the last 3500 years.
TL;DR: In this paper, the authors represent the vegetation history of the last 3500 years and conduct an analysis of the climatic fluctuations on a 75 km long transect on the western Dead Sea shore.