Description

Analyzed sediment cores from Dead Sea originated from two drilling sites: 1. Ein Gedi (21 m, 10,000 years BP) and 2. northern basin, site 5017-1 (455 m, ca. 220,000 years BP).

Related publications

• Litt, T., Ohlwein, C., Neumann, F., Hense, A., Stein, M. (2012): Holocene climate variability in the Levant from the Dead Sea pollen record. – In: Quaternary Science Reviews, Vol. 49, p: 95-105, DOI: 10.1016/j.quascirev.2012.06.012
  Maintained by Andrea Miebach Spatial Temporal
• Thoma, B. (2017): Palaeoclimate Reconstruction in the Levant and on the Balkans. University Bonn, Meteorological Institute
  Maintained by Benno Thoma, Andreas Hense Spatial
• Chen, C. (2017): Dead Sea Pollen Reveal the Paleoenvironment of the Southern Levant during 147–89 ka from the Paleobotanical Perspective. University of Bonn
  Maintained by Andrea Miebach Spatial Temporal
• Miebach, A. (2017): Climate- and Human-Induced Vegetation Changes in Northwestern Turkey and the Southern Levant since the Last Glacial. University of Bonn
  Maintained by Andrea Miebach
• Chen, C., Litt, T. (2018): Dead Sea pollen provides new insights into the paleoenvironment of the southern Levant during MIS 6-5. Elsevier – In: Quaternary Science Reviews, Vol. 188, p: 15-27, DOI: 10.1016/j.quascirev.2018.03.029
  Maintained by Andrea Miebach Spatial Temporal
• Stolzenberger, S. (2017): On the Probabilistic Evaluation of Decadal and Paleoclimate Model Predictions. University of Bonn
  Maintained by Andrea Miebach