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Renata Perego

Researcher at University of Basel

Publications -  19
Citations -  355

Renata Perego is an academic researcher from University of Basel. The author has contributed to research in topics: Bronze Age & Biology. The author has an hindex of 8, co-authored 16 publications receiving 253 citations. Previous affiliations of Renata Perego include National Research Council & University of Milano-Bicocca.

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New AMS 14C dates track the arrival and spread of broomcorn millet cultivation and agricultural change in prehistoric Europe.

TL;DR: An extensive programme of AMS-dating of charred broomcorn millet grains from 75 prehistoric sites in Europe provides a new, high-resolution chronological framework for this key agricultural development that likely contributed to far-reaching changes in lifestyle in late 2nd millennium bc Europe.
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Lake evolution and landscape history in the lower Mincio River valley, unravelling drainage changes in the central Po Plain (N-Italy) since the Bronze Age

TL;DR: The Etruscan harbour of Forcello, in the lower valley of the Mincio River, northern Italy, was active between 540 and 390 BC, and stratigraphic investigations revealed that the settlement occupied a hill on the shore of a lake.
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Sedimentary evolution and persistence of open forests between the south-eastern Alpine fringe and the Northern Dinarides during the Last Glacial Maximum

TL;DR: In this paper, the authors present a paleoenvironmental reconstruction for the mountain fringe between the South Eastern Alps and the Northern Dinarides (NE-Italy/W-Slovenia) during the last glacial maximum.
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8800 years of high-altitude vegetation and climate history at the Rutor Glacier forefield, Italian Alps. Evidence of middle Holocene timberline rise and glacier contraction

TL;DR: In this article, the authors focused on records of timberline and glacier oscillations in the Rutor Glacier forefield (Western Italian Alps) in the last 8800 years, and adopted an integrative stratigraphic approach including proxies for glacier advance and timberline estimation, sedimentary events, and reconstructed temperatures.