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Palaeogeographical evolution of the Atlantic coast of Pampa and Patagonia from the last glacial maximum to the Middle Holocene: PALAEOGEOGRAPHY OF PATAGONIA SINCE LGM
Abstract
We reconstruct the palaeogeographical evolution of the continental shelf in Patagonia for the period spanning the Last Glacial Maximum (approximately 24 000 calibrated years BP) to the Middle Holocene using a global sea level rise curve for this period and GLOBAL MAPPER 10 software (http://www.globalmapper.com). Our model provides new information for future palaeoenvironmental and palaeoclimatic reconstructions. We expect the model will be of assistance in studies designed to examine patterns of faunal and plant population expansion, dispersal, and migration in Pampa and Patagonia during the Late Glacial period (i.e. 15-10 ¹⁴C kyr BP).
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“The most dramatic changes occurred during the Late Pleistocene, when dry and cold weather and lower precipitation levels (ca. 100 mm) resulted in a sea-level drop of ca. 60 m below present day (Cione, Tonni, & Soibelzon 2003; Ponce et al. 2011; Quattrocchio et al. 2008; Zárate & Blasi 1991).”
From A maxent predictive model for hunter-gatherer sites in the southern pampas, argentina (2021) · cites this paper as Ponce et al. 2011
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Late Cenozoic Glaciations in Patagonia and Tierra del Fuego
Rabassa, J. (2008) · Developments in Quaternary Sciences · doi:10.1016/s1571-0866(07)10008-7 · Cited by 312
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Cited by
Sorted by citations
A maxent predictive model for hunter-gatherer sites in the southern pampas, argentina
Rafuse, D. J. (2021) · Open Quaternary · doi:10.5334/oq.97 · Cited by 17
Metadata
- Authors
- PONCE, J. F., RABASSA, J., CORONATO, A., & BORROMEI, A. M.
- Venue
- Biological Journal of the Linnean Society
- Publisher
- Oxford University Press (OUP)
- Published
- 2011-05-31
- Volume
- 103
- Issue
- 2
- Pages
- 363-379
- ISSN
- 0024-4066
- Cited by
- 186
- References
- 1
- Language
- en
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