Hunter-gatherer mobility decisions and synchronous climate change in the Southern Andes: The early and middle Holocene occupations of ARQ-18, San Juan, Argentina (29.5°S)

2016 ◽  
Vol 422 ◽  
pp. 66-80 ◽  
Author(s):  
Erik Marsh ◽  
Valeria Cortegoso ◽  
Silvina Castro
2002 ◽  
Vol 17 (4) ◽  
pp. 15-1-15-12 ◽  
Author(s):  
Michael Staubwasser ◽  
Frank Sirocko ◽  
Pieter M. Grootes ◽  
Helmut Erlenkeuser

Boreas ◽  
2018 ◽  
Vol 47 (3) ◽  
pp. 897-909 ◽  
Author(s):  
Anna Šolcová ◽  
Libor Petr ◽  
Petra Hájková ◽  
Jan Petřík ◽  
Peter Tóth ◽  
...  

2009 ◽  
Vol 28 (27-28) ◽  
pp. 3246-3262 ◽  
Author(s):  
Gianluca Marino ◽  
Eelco J. Rohling ◽  
Francesca Sangiorgi ◽  
Angela Hayes ◽  
James L. Casford ◽  
...  

2016 ◽  
Vol 85 (2) ◽  
pp. 227-244 ◽  
Author(s):  
Laurent Lespez ◽  
Arthur Glais ◽  
José-Antonio Lopez-Saez ◽  
Yann Le Drezen ◽  
Zoï Tsirtsoni ◽  
...  

Numerous researchers discuss of the collapse of civilizations in response to abrupt climate change in the Mediterranean region. The period between 6500 and 5000 cal yr BP is one of the least studied episodes of rapid climate change at the end of the Late Neolithic. This period is characterized by a dramatic decline in settlement and a cultural break in the Balkans. High-resolution paleoenvironmental proxy data obtained in the Lower Angitis Valley enables an examination of the societal responses to rapid climatic change in Greece. Development of a lasting fluvio-lacustrine environment followed by enhanced fluvial activity is evident from 6000 cal yr BP. Paleoecological data show a succession of dry events at 5800–5700, 5450 and 5000–4900 cal yr BP. These events correspond to incursion of cold air masses to the eastern Mediterranean, confirming the climatic instability of the middle Holocene climate transition. Two periods with farming and pastural activities (6300–5600 and 5100–4700 cal BP) are evident. The intervening period is marked by environmental changes, but the continuous occurrence of anthropogenic taxa suggests the persistence of human activities despite the absence of archaeological evidence. The environmental factors alone were not sufficient to trigger the observed societal changes.


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