5
views
0
recommends
+1 Recommend
0 collections
    0
    shares
      • Record: found
      • Abstract: found
      • Article: found
      Is Open Access

      The Late and Final Middle Palaeolithic of Central Europe and Its Contributions to the Formation of the Regional Upper Palaeolithic: a Review and a Synthesis

      , , ,
      Journal of Paleolithic Archaeology
      Springer Science and Business Media LLC

      Read this article at

      Bookmark
          There is no author summary for this article yet. Authors can add summaries to their articles on ScienceOpen to make them more accessible to a non-specialist audience.

          Abstract

          For decades, the relationship of pre-modern hominins to anatomically modern humans (AMH) and the transition from mode 3 to mode 4 industries remain topics of ongoing scientific debate. Over the last 20 years, different disciplines have added new data and much detail to these questions, highlighting the demographic and social and cultural complexity underlaying these major changes or turnovers in human evolution. As with most other regions outside Africa, archaeologists faced long-lasting discussions whether or not the central European archaeological record is to be understood as a regional transition from the Middle Palaeolithic (MP) to the Upper Palaeolithic (UP) or if it is characterised by the replacement of Neanderthal MP techno-complexes by industries of overall UP character imported by modern humans. These debates have been re-fuelled by the discoveries of new sites, of new hominin fossil remains and by aDNA studies pinpointing towards the arrival of AMH in Europe several millennia earlier than previously thought (Slimak et al.,  Science Advances, 8, eabj9496, 2022; Hajdinjak et al., Nature, 592, 253-257, 2021; Prüfer et al., Nature Ecology & Evolution, 5, 820–825, 2021). Together with new radiometric age-estimates and detailed archaeological site studies, these developments call to recapture the present knowledge of the Late (LMP) and Final Middle Palaeolithic (FMP) of central Europe, viewed from the perspective of lithic technology and typology, raw material exploitation and land-use strategies. We will review and characterise this record as it represents the demographic and cultural substrate that AMH had met and will discuss to which degree this substrate contributed to the formation of the central European UP.

          Related collections

          Most cited references180

          • Record: found
          • Abstract: found
          • Article: not found
          Is Open Access

          THE INTCAL20 NORTHERN HEMISPHERE RADIOCARBON AGE CALIBRATION CURVE (0–55 CAL kBP)

          Radiocarbon ( 14 C) ages cannot provide absolutely dated chronologies for archaeological or paleoenvironmental studies directly but must be converted to calendar age equivalents using a calibration curve compensating for fluctuations in atmospheric 14 C concentration. Although calibration curves are constructed from independently dated archives, they invariably require revision as new data become available and our understanding of the Earth system improves. In this volume the international 14 C calibration curves for both the Northern and Southern Hemispheres, as well as for the ocean surface layer, have been updated to include a wealth of new data and extended to 55,000 cal BP. Based on tree rings, IntCal20 now extends as a fully atmospheric record to ca. 13,900 cal BP. For the older part of the timescale, IntCal20 comprises statistically integrated evidence from floating tree-ring chronologies, lacustrine and marine sediments, speleothems, and corals. We utilized improved evaluation of the timescales and location variable 14 C offsets from the atmosphere (reservoir age, dead carbon fraction) for each dataset. New statistical methods have refined the structure of the calibration curves while maintaining a robust treatment of uncertainties in the 14 C ages, the calendar ages and other corrections. The inclusion of modeled marine reservoir ages derived from a three-dimensional ocean circulation model has allowed us to apply more appropriate reservoir corrections to the marine 14 C data rather than the previous use of constant regional offsets from the atmosphere. Here we provide an overview of the new and revised datasets and the associated methods used for the construction of the IntCal20 curve and explore potential regional offsets for tree-ring data. We discuss the main differences with respect to the previous calibration curve, IntCal13, and some of the implications for archaeology and geosciences ranging from the recent past to the time of the extinction of the Neanderthals.
            Bookmark
            • Record: found
            • Abstract: not found
            • Article: not found

            Irregular glacial interstadials recorded in a new Greenland ice core

              Bookmark
              • Record: found
              • Abstract: found
              • Article: not found

              The landscape of Neandertal ancestry in present-day humans

              Analyses of Neandertal genomes have revealed that Neandertals have contributed genetic variants to modern humans 1–2 . The antiquity of Neandertal gene flow into modern humans means that regions that derive from Neandertals in any one human today are usually less than a hundred kilobases in size. However, Neandertal haplotypes are also distinctive enough that several studies have been able to detect Neandertal ancestry at specific loci 1,3–8 . Here, we have systematically inferred Neandertal haplotypes in the genomes of 1,004 present-day humans 12 . Regions that harbor a high frequency of Neandertal alleles in modern humans are enriched for genes affecting keratin filaments suggesting that Neandertal alleles may have helped modern humans adapt to non-African environments. Neandertal alleles also continue to shape human biology, as we identify multiple Neandertal-derived alleles that confer risk for disease. We also identify regions of millions of base pairs that are nearly devoid of Neandertal ancestry and enriched in genes, implying selection to remove genetic material derived from Neandertals. Neandertal ancestry is significantly reduced in genes specifically expressed in testis, and there is an approximately 5-fold reduction of Neandertal ancestry on chromosome X, which is known to harbor a disproportionate fraction of male hybrid sterility genes 20–22 . These results suggest that part of the reduction in Neandertal ancestry near genes is due to Neandertal alleles that reduced fertility in males when moved to a modern human genetic background.
                Bookmark

                Author and article information

                Contributors
                Journal
                Journal of Paleolithic Archaeology
                J Paleo Arch
                Springer Science and Business Media LLC
                2520-8217
                December 2022
                November 18 2022
                : 5
                : 1
                Article
                10.1007/s41982-022-00126-8
                31e118b0-02aa-4a6f-af1f-f9d5caf16d83
                © 2022

                https://creativecommons.org/licenses/by/4.0

                https://creativecommons.org/licenses/by/4.0

                History

                Comments

                Comment on this article