Tracing population movement across eastern Africa and Eurasia through lithic technology during the late Pleistocene (End of MIS 6 to MIS 4)

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MaeGoder

Dr. Mae Goder, Max Planck Weizmann Center for Integrative Archaeology and Anthropology, Weizmann Institute of Science, Israel

Many archaeologists associate the appearance of Homo sapiens and modern behavior with the Middle Stone Age of Africa. Over the years numerous models have been developed to explain how and why modern humans left Africa and dispersed throughout the world. The majority of these models are based on skeletal and genetic data as well as climatic data, while paradoxically very few incorporate archaeological data.

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The Diatom Flora of Lake Kinneret (Israel) – Palaeolimnological evidence for Holocene climate change and human impact in the southeastern Mediterranean

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I am a member of the CRC 806 in project B3 as research assistant since 2011. Since September 2013 I am working on my PhD (funded by the German National Academic Foundation), in which I am analyzing changes of fossil diatom communities during the Holocene in sediment cores from Lake Kinneret (Israel; Southeastern Mediterranean) and Laguna de Medina (Spain, Western Mediterranean).

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