Titlebook: Archaeology of Piedra Museo Locality; An Open Window to th Laura Miotti,Monica Salemme,Darío Hermo Book 2022 Springer Nature Switzerland AG

LANCE

,Partners in Activism—Ivan and Lesley,ponent is deposited in Stratigraphic Unit 2 (. 8800–8400?cal. years BP). While the oldest assemblage of the site contains a significant record of extinct fauna—., ., and . sp., the two remaining assemblages are characterized by the strong presence of . (“guanaco”) remains, and in minor proportion rh

Stagger

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Connecting to Other Screens or Projectors,record a similar mean for δ.C, but there is a statistically significant difference in the δ.N, with higher values during the Middle Holocene. These δ.N variations would be a reflection of environmental changes occurring in the Central Plateau during this period.

巨頭

Everyday Conceptions of Emotionrce number of white hand stencils and paint remains. The third one corresponds to engraving events whose maximum age is the end of the middle Holocene. The fourth painting episode includes diverse expressions of hand reproductions in different colors.

Friction

expeditious

富足女人

Last Glacial Maximum, Late Glacial and Holocene of Patagoniaf the Patagonian landscape as we know it took place during this period. Moreover, the human colonization of Patagonia took place sometime after the Last Glacial Maximum and during the Late Glacial (ca. 18,000 to 10,000?years ago) and it was completed along the entire Early Holocene.

莊嚴(yán)

Geoarchaeology of Piedra Museo Localityve been affected by the fluctuations of the water table. The early occupations (late-glacial interval) of the rock shelter occurred when the sedimentation was dominant; instead, the later occupations (early-middle Holocene) occurred when soil-forming processes were prevalent.

修飾

Radiocarbon Chronology at the AEP-1 Rockshelter in Piedra Museo Locality: An Update and Discussion oal, i.e., 15–10?ka BP. They occurred when the sedimentation event was dominant in the rockshelter; instead, the latest occupations (Early-Middle Holocene) occurred when soil forming processes were dominant. On the basis of the curve calibration and the subsequent calculation of the probability sum o

使高興

Quaternary Fossil Vertebrates of Tierra del Fuego?and Southernmost Patagoniaveral species of Pampean herbivore megamammals expanded their distribution to reach the south of Patagonia and Tierra del Fuego. These herbivores were accompanied by their potential predators. This expansion of the distribution toward high latitudes can be attributed to environmental conditions that