Our field data from the Upper Palaeolithic site of Al-Ansab 1 (Jordan) and from a pollen sequence in the Dead Sea elucidate the role that changing Steppe landscapes played in facilitating anatomically modern human populations to enter a major expansion and consolidation phase, known as the "Early Ahmarian", several millennia subsequent to their initial Marine Isotope Stage 4/3 migration from Africa, into the Middle East. The Early Ahmarian techno-cultural unit covers a time range between 45 ka-37 ka BP. With so far more than 50 sites found, the Early Ahmarian is the first fully Upper Palaeolithic techno-cultural unit exclusively and undisputedly related to anatomically modern human populations. In order to better understand the potentially attractive features of the Early Ahmarian environmental context that supported its persistence for over 8,000 years, we carried out a decennial research program in Jordan and in the Dead Sea. This included (1) a geoscientific and archaeological survey program in the Wadi Sabra (Jordan) with a particular focus on excavations at the Early Ahmarian site of Al-Ansab 1 alongside the detailed analysis of Quaternary sediments from the same area and (2) palaeobotanical research based on Quaternary lake deposits from the Dead Sea. Our pollen data from the Dead Sea indicate slow, low frequency vegetational variation with expanding Artemisia steppe, from 60 to 20 ka BP (MIS 3-2). Here, we see a reciprocal assimilation of southern and northern Levantine vegetation zones thereby enhancing a long-lasting south-to-north steppe corridor. The same integration process accelerated about 40 ka ago, when forested areas retreated in the Lebanese Mountains. The process then extended to encompass an area from Southern Lebanon to
In the analysis of archaeological relationships and processes, a uniform classification of the dataset is a fundamental requirement. To achieve this, a standardised taxonomic system, as well as consistent and valid criteria for the grouping of sites and assemblages, must be used. The Central European Late Palaeolithic (ca. 12,000-9700 cal BC) has a long research history and many regionally and temporally specific units-groups and cultures-are recognised. In this paper, we examine the complex taxonomic landscape of this period and critically analyse the use of typological, functional and economic criteria in the definition of selected groups. We subject three different archaeological taxonomic units, the Bromme culture from Denmark, the Fürstein group from Switzerland and the Atzenhof group from Germany, to particularly detailed scrutiny and highlight that the classificatory criteria used in their definition are inconsistent across units and most likely unsuitable for circumscribing past sociocultural units. We suggest a comprehensive re-examination of the overarching taxonomic system for the Late Palaeolithic, as well as a re-evaluation of the methodologies used to delineate sociocultural units in the Palaeolithic.
SrRuO 3 is a highly interesting material due to its anomalous-metal properties related with ferromagnetism and its relevance as conductive perovskite layer or substrate in heterostructure devices. We have used optical floating zone technique in an infrared image furnace to grow large single crystals of SrRuO 3 with volumes attaining several hundred mm 3 . Crystals obtained for optimized growth parameters exhibit a high ferromagnetic Curie temperature of 165 K and a low-temperature magnetization of 1.6 μ B at a magnetic field of 6 T. The high quality of the crystals is further documented by large residual resistance ratios of 75 and by crystal structure and chemical analyzes. With these crystals the magnetic anisotropy could be determined.
The Late Glacial, that is the period from the first pronounced warming after the Last Glacial Maximum to the beginning of the Holocene (c. 16,000-11,700 cal BP), is traditionally viewed as a time when northern Europe was being recolonized and Late Palaeolithic cultures diversified. These cultures are characterized by particular artefact types, or the co-occurrence or specific relative frequencies of these. In north-eastern Europe, numerous cultures have been proposed on the basis of supposedly different tanged points. This practice of naming new cultural units based on these perceived differences has been repeatedly critiqued, but robust alternatives have rarely been offered. Here, we review the taxonomic landscape of Late Palaeolithic large tanged point cultures in eastern Europe as currently envisaged, which leads us to be cautious about the epistemological validity of many of the constituent groups. This, in turn, motivates us to investigate the key artefact class, the large tanged point, using geometric morphometric methods. Using these methods, we show that distinct groups are difficult to recognize, with major implications for our understanding of patterns and processes of culture change in this period in north-eastern Europe and perhaps elsewhere.
Only a limited number of radiometric dates for the Final Palaeolithic and the first half of the Mesolithic are available from the southeastern Baltic. This paper presents eight new Late Pleistocene/Early Holocene radiocarbon accelerator mass spectrometry (14C AMS) ages of osseous artifacts housed at the Kaliningrad Regional Museum of History and Art. These artifacts include one piece of worked reindeer (Rangifer tarandus) antler, three axes of the so-called Lyngby type, one bone point, one uniserial harpoon, one so-called bâton percé antler shaft, and one slotted bone. All the samples were successfully dated and yielded five Late Pleistocene and three Early Holocene ages, including the hitherto earliest age for human occupation in the Eastern Baltic. The dates include not only a surprisingly early date for a bone point (for this region), but also some dates that contradict expected ages based on traditional typological assessment. Our study significantly adds to the still small number of existing absolutely dated artifacts from the region and proposes new ways of viewing the Final Palaeolithic and Early Mesolithic chronology in the southeastern Baltic.
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