Occupation of highland Central Asia: New evidence from Kurteke rockshelter, Eastern Pamir
Introduction
Research shows that the mountainous spine of Inner Asia has fostered human habitation for tens of thousands of years, with recent discoveries of Denisovans from the disparate ends of these interconnected ranges (Krause et al., 2010; Zhang et al., 2020), Neanderthals (Skov et al., 2022), Neanderthal/Denisovan hybrids (Slon et al., 2018), and Pleistocene examples of anatomically modern humans throughout (Ranov and Bubnova, 1961). The valleys of these mountains clearly fostered insular pockets of forests and megafaunal prey that drew people in throughout the latter half of the Pleistocene and during the Holocene. At the core of these interconnected chains of mountains, the Pamir Mountains, in particular, played a key role in human history, from the earliest human occupation of Eurasia through the formation the Silk Road (Good, 2013; Olivieri et al., 2019; Ranov and Carbonell, 1995; Vilade and Olivieri, 2002). The Pamirs sheltered some of the highest mountain passes of the ancient Silk Road (e.g., Bazar Dara), and some of the earliest mining towns in Eurasia formed in these high-alpine valleys (Bubnova, 2017; Bubnova, 2004, Bubnova, 2008). In recent years, excavations in caves within the Pamir range have produced the earliest evidence for productive economies in Central Asia proper, ornamental bone bead manufacture, and a complex array of lithic forms (Fedorchenko et al., 2020; Nishiaki et al., 2022; Taylor et al., 2021). Archaeological studies have recently shown that the Pamirs fostered a complex mix of agricultural systems in prehistory, serving as a corridor for the transmission of East Asian crops westward, as seen in recent discoveries of some of the oldest millet grains in West Asia (Yatoo et al., 2020) and the presence of early barley cultivation in western Tibet (Tang et al., 2021). Archaeobotanical data further suggest that the region served as a mixing zone for South Asian crops while they adapted to northern climates (Spengler et al., 2021; Tang et al., 2021).
Despite the clear archaeological significance, archaeological coverage of much of this region is exceedingly poor, and extant knowledge is based largely on 20th century Soviet scholarship performed before the development of many modern scientific techniques in archaeology. Based on previous research, some scholars have speculated that the Eastern Pamir could have been first inhabited during the Final Upper Paleolithic (20–12 ka BP) (Ranov and Khudjageldiev, 2005). However, archaeology from this period is largely represented by isolated artifacts without a reliable stratigraphic contexts (Ranov and Khudjageldiev, 2005). Artifacts recovered within stratigraphic sequence from the region can only be confidently dated as far back as the Early Holocene (Filimonova and Zhukov, 2020). Considering the unique preservation of archaeological material at many sites in the region, renewed field study using scientific techniques is essential for the development of an understanding of the chronology of early human activity. Here, we report the results of our ongoing research at the Kurteke rock shelter in the Eastern Pamir (Fig. 1) and explore its implications for an early highland occupation of the Pamirs during the Pleistocene/Holocene transition.
Section snippets
Regional background
Situated at the heart of Central Asia, the Pamir Mountains are located at the intersection between the Karakorum, Hindukush, Kunlun, and Tian Shan mountain ranges. The climate is largely arid, sitting in the rain shadow of the Himalaya, which blocks the eastern monsoonal front, an orographically determined climatic pattern that stretches deep into the past (Spate et al., 2022). While human impacts on the vegetation of the Pamirs also stretch back several millennia (Spate et al., 2022), there
Paleoclimatic framework
During the Last Glacial Maximum, the Pamir region was dry and cold, much colder than today (Lioubimtseva and Cole, 2006). According to pollen data, the Early Holocene began with an increase in humidity, and paleoclimatic data suggest that maximum temperatures were reached around 6.0–4.5 ka BP; drier conditions prevailed between 6.9 and 4.9 ka BP (Heinecke et al., 2018; Heinecke et al., 2017; Mischke et al., 2017). Intense glacial melt watered the valleys, resulting in wetter intervals between
Kurteke: location and history of study
The Kurteke rockshelter is located in the Eastern Pamir, 40 km southeast of the modern village of Murgab, at an absolute elevation of 3980 m asl (Fig. 1.1). The shelter is formed by a detached mass of rock in the valley of the Kurteke River, the rock is about 100 m long and 15–20 m high (Fig. 1.2); the archaeological site is associated with a small indent in the rock (12 m long with a width of 3.5 m).
Stratigraphy
In our reanalysis of the east wall of Ranov's excavations, we identified two stratigraphic units within a 0.84-m profile (Fig. 3). The upper unit (layer 1) is 0.63 m thick. We further divided it into five sublayers (1.1 to 1.5 downward). Sublayers 1.1, 1.3, and 1.5 are composed of a brownish sandy loam with fine gravel. Sublayers 1.2 and 1.4 were thin laminae found at depths of 10 and 35 cm below the modern surface, respectively. These layers appeared distinct due to occurrence of dry grass and
Discussion
The artifact assemblage recovered from the Kurteke rockshelter is characterized by volumetric knapping, resulting in microbladelet production; the tool kit contains bladelets with ventral retouch. Use-wear analysis suggests that two unretouched flakes were used on hard organic materials (bone or wood); an additional flake was used as a drill and a saw. Microblades appear to have been hafted (Fig. 6, Fig. 7), with one side showing traces of working of soft material (meat or skin), likely as part
Conclusion
In revisiting Kurteke, we were able to conduct archaeological investigations using methods not available to Ranov in the 1960s. Based on these analyses, we suggest a much earlier occupation than previously hypothesized. Cleaning and reanalysis of the former excavation profile revealed new material for scientific study, which shows changes in human-environmental relationships in the Pamir region, including paleoenvironmental data, faunal and floral remains, and aspects of material culture.
Formatting of funding sources
This study (ZooMS-analysis, palynological analysis, absolute dating in Golden valley laboratory) was supported by the Russian Scientific Foundation, Russia (grant number 19-78-10053), use-wear analysis was carried out under the financial supports of Russian Foundation for Basic Research, Russia (grant number 20-09-00387), techno-typological analysis of the lithic collection was carried out in the frame of the project RFBR #21-59-93002. Radiocarbon dating in the Poznan laboratory was supported
Author statement
S. Shnaider, S. Zhilich, L. Zotkina, K. Boxleitner, William T.T. Taylor, A. Chernonosov, L. Orlando, R. Spengler – wrote the manuscript, S. Shnaider, S. Shnaider, S. Zhilich, L. Zotkina, K. Boxleitner, S. Baranova, L. Tonasso-Calviere, L. Orlando, R. Spengler contributed data. All authors reviewed the manuscript.
Declaration of Competing Interest
This original research paper has not been published elsewhere and is not under consideration by any other journal. We do not foresee any conflict of interests in publishing this paper. Please contact the corresponding author if you require further information on this manuscript. We thank the editorial board for considering our manuscript for peer review.
Acknowledgements
A special thanks goes to Andrey I. Krivoshapkin (Insitute of Archaeology and Ethnography SB RAS, Novosibirsk, Russia), Masnav Navruzbekov and Maxim Filimonov (Institute of History, Archaeology Ethnography after A. Donish, Dushanbe, Tajikistan) for their support and essential help during the excavations. We also thank Maciej Krajcarz (Institute of Geological Sciences, Warsaw, Poland) for his support and valuable comments on the manuscript. We also want to dedicate this work to people of Murgab
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