Karisa Terry
Central Washington University
14 Papers
57 Citations
Karisa Terry is an academic researcher from Central Washington University. The author has contributed to research in topics: Pleistocene & Upper Paleolithic. The author has an hindex of 7, co-authored 14 publications. Previous affiliations of Karisa Terry include Tokyo Metropolitan University.
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Papers
Radiocarbon dates, microblades and Late Pleistocene human migrations in the Transbaikal, Russia and the Paleo-Sakhalin-Hokkaido-Kuril Peninsula
TL;DR: In this article, the authors compare late Pleistocene archaeological 14C databases from the Transbaikal, Russia and the Paleo-Sakhalin-Hokkaido-Kuril Peninsula (PSHK) to the appearance and disappearance of microblade technology for evidence of human migration.
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The twilight of Paleolithic Siberia: Humans and their environments east of Lake Baikal at the late-glacial/Holocene transition
TL;DR: The Younger Dryas in Eastern Siberia and the Russian Far East was in many ways a watershed between Upper Paleolithic lifeways of the late Pleistocene and more settled Mesolithic traditions of the early Holocene as discussed by the authors.
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Emergence of a microlithic complex in the Transbaikal Region of southern Siberia
TL;DR: In this article, the authors trace the process of microlithization in the Transbaikal Region of southern Siberia using core reduction event-tree and morphometric analysis of cores and their by-products.
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Late Pleistocene Geology and Paleolithic Archaeology of the Shimaki Site, Hokkaido, Japan
TL;DR: In this paper, the authors assess geochronological, sedimentological, stratigraphic, and stone tool data from Shimaki, an Upper Paleolithic site in southeastern Hokkaido, Japan.
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Last Glacial Maximum Human Occupation of the Transbaikal, Siberia
Ian Buvit,Karisa Terry,Masami Izuho,Mikhail V. Konstantinov,Aleksander V. Konstantinov +4 more
- 06 Nov 2015
TL;DR: This paper analyzed the late Pleistocene radiocarbon chronology of the Transbaikal region of Siberia and concluded that humans inhabited the area during parts of the Last Glacial Maximum, but completely abandoned it between 24,800 and 22,800 cal yr BP.
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