The environment in the Caucasus in the Upper Paleolithic (Late Pleistocene): Evidence from the small mammals from Dzudzuana cave, Georgia

Abstract

The MIS 3/2 transition (Denekamp interstadial and beginning of the LGM) is a crucial point in time for understanding adaptation of modern humans to climate. The Southern Caucasus is a unique place to study human ecology within this time period because it served as a refugium during the Last Glacial Maximum (LGM) and thus allows us to study how human populations responded to the climatic shifts during the Last Glacial. This study presents the results of the paleoecological analysis of Dzudzuana cave during the MIS 3/2 transition using small mammal community structure as a proxy for paleoenvironment.Of the four units in Dzudzuana (Units A through D), Unit C, divided into subunits C5 to C1, has been dated to 27–24 ka cal BP and the MIS 3/2 transition. Thus, Unit C allows for a diachronic analysis throughout this important time period. Small mammals were found primarily in subunit C2 and C1.Analysis of the small mammal assemblages of Dzudzuana subunits C2 and C1 confirm the paleoecological reconstruction obtained from macrobotanical remains, and suggest a refugium habitat during the last phase of MIS 3 and the onset of the LGM. Comparison with a contemporaneous site in the region (Satsurblia) suggests a high spatial-temporal mosaic habitat in the region. Small refugium areas within the Rioni River valley and its tributaries that enjoyed ameliorated climatic conditions and proximity to water resources may have promoted local human habitation.Furthermore, results suggest that the small mammal assemblages of Dzudzuana are non-analogue communities typical of European Denekamp assemblages, and provide a new datum point for the faunal remains during this time period.