Abstract
Ice-rich syncryogenic (termed “Ice Complex”) deposits are common in northern East Siberia and constitute the most important feature of the Quaternary geology of the region. The Ice Complex formed throughout the Late Pleistocene and not only contains an archive of paleoenvironmental proxies such as Pleistocene faunal remains, but also comprises a record of human habitation spanning ∼50,000 years, beginning with early MIS3. The development of syngenetic permafrost is an important variable in the formation of archaeological contexts in this depositional setting. Excavations of the Yana site complex in the lower Yana River area provide a unique opportunity to study archaeological finds preserved in Ice Complex deposits. Based on long-term field observations and dating results, we present important conclusions concerning the geology of the Yana sites. Taphonomic biases with potential to obscure the archaeological record are discussed. The thawing of frozen primary deposits has distorted depositional sequences, leading to the formation of secondary features and contexts, e.g., ice-wedge casts. Collapsed blocks of frozen sediment with undisturbed fragments of frozen layers containing artifacts and/or paleobiotic remains may become incorporated and refrozen into another depositional sequence and a source of misinterpretation and chronometric error. Furthermore, severe cryoturbation within the polygonal mounds warps the sediment in contact with the ice wedges; as a result, the contents of the sediment is uplifted with important consequences: 1) the hypsometric provenience of datable material is altered, creating chronometry problems; 2) in archaeology, there is an increased potential for misinterpretations with respect to dating, cultural classification, and human behavior; 3) transported material may form secondary concentrations at different hypsometric levels and thus bring further complications for its understanding; 4) in geology, the transportation of geochemical signatures may lead to erroneous interpretation of the geological potential of the area; 5) uplifted deposits contribute to increased Ice Complex thickness, which is thus not a direct function of sedimentation, but a combined result of sedimentation and redistribution of the deposits within an existing polygon deposit. Thus, the analysis of Ice Complex deposits during archaeological excavations at the Yana site complex has wider implications for Quaternary science.
Highlights
In the Northern hemisphere, permafrost underlies approximately 22.79 × 106 km2, or 23.9% of the exposed land surface
The structure and geocryology of Member 3 are highly germane to the present study, and below we present a detailed description based on the observations of the profiles in the Northern Point area (NP) area of the Yana site complex (Figures 6A,B)
Such concentrations are related to ice wedge casts during their initial formation; further development of these features may lead to full transformation of the primary in situ context to a secondary concentration of archaeological material similar to that investigated at the Zhokhov site in the New Siberian islands
Summary
In the Northern hemisphere, permafrost underlies approximately 22.79 × 106 km, or 23.9% of the exposed land surface. There is no alternative source for these secondary concentrations than the primary culture-bearing horizon in the central portion of T2, 7–8 m below the modern surface Such concentrations are related to ice wedge casts during their initial formation; further development of these features may lead to full transformation of the primary in situ context to a secondary concentration of archaeological material similar to that investigated at the Zhokhov site in the New Siberian islands (see, e.g., Pitul’ko, 1993; Pitulko et al, 2015b)
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