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  • 1
    Call number: 9/S 90.0095(401)
    In: Special paper
    Description / Table of Contents: This volume is a key contribution to anyone interested in the Near East and its changing environments, climate change, natural hazards and lacustrine processes, salt diapirs, and age dating. It presents new data and syntheses by active researchers of the Dead Sea basin, one of the most historically, geologically and hydrologically interesting lake basins in the world. The Dead Sea holds a few records: its shores are at the lowest elevation on the continents and its water is among the most saline and dense in the world. It is a place where humans have interacted with harsh environments and rough landscapes for a very long time; this extremely arid lake basin is a challenge to modern societies. Some chapters cover natural hazards such as earthquakes and collapse sinkholes, floods, and flood-producing storms; others contribute to understanding the scarce water resources of surface and ground water in the area. Shore and lake depositional processes, the evolution of the lake water, and age dating methods also are presented and are used in reconstructing the lake levels and the Near East climate change in historical and prehistorical times. The interaction of people and their use of the shores and the fascination nineteenth century travelers had with the lake are also presented.
    Type of Medium: Series available for loan
    Pages: x, 253 S. Ill., graph. Darst., Kt.
    ISBN: 0813724015 , 978-0-8137-2401-0
    Series Statement: Special paper / Geological Society of America (GSA) 401
    Classification:
    Paleontology
    Location: Reading room
    Branch Library: GFZ Library
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  • 2
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    PANGAEA
    In:  Supplement to: Litt, Thomas; Ohlwein, Christian; Neumann, Frank Harald; Hense, Andreas; Stein, Mordechai (2012): Holocene climate variability in the Levant from the Dead Sea pollen record. Quaternary Science Reviews, 49, 95-105, https://doi.org/10.1016/j.quascirev.2012.06.012
    Publication Date: 2024-01-06
    Description: The Dead Sea, located at the deepest place on continent and between the subtropical Mediterranean zone and the desert, reflects in its water composition and levels, and sedimentary records the hydrological conditions in the southern Levant region. Temporal variations in rainfall and temperatures of the Holocene Levant are reconstructed here from pollen data recovered from a sediment core drilled at the Ein Gedi shore, applying a novel biome model based on Bayesian statistics. Our results suggest that the region was arid and warm in the early Holocene period (~10-6.5 ka cal BP), wetter and colder in the mid Holocene (6.3-3.3 ka cal BP), and drier and warmer in the late Holocene (~3.2 ka cal BP to present). These periods comprise multi-centennial climate cycles that are characterized by rapid changes in temperature and precipitation reflecting Sea Surface Temperature (SST) and atmospheric conditions over the Atlantic Ocean. The pollen record responds within a short time interval to the climate conditions and marks rapid shifts from Mediterranean to desert environmental conditions and back in the southern Levant region. We also evaluate our results in the light of possible disturbances of the natural vegetation, e.g. the possibility of forest decrease, since the Neolithic.
    Keywords: Acacia; AGE; Alnus; Anemone; Apiaceae; Arbutus; Artemisia; Asphodelus; Brassicaceae; Carpinus; Caryophyllaceae; Casuarina; Cedrus; Centaurea; Ceratonia; Cerealia-type; Chenopodiaceae; Cirsium-type; Cistus-type; Corylus; Crataegus; Cupressaceae; Cyperaceae; Dead Sea Basin, Israel; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSEn; Echium; Ein Gedi; Ephedra; Euphorbia; Fabaceae; Fraxinus; Geranium; Helianthemum; Herniaria-type; Hypericum; Juglans; Knautia; Lamiaceae; Laurus; Liguliflorae; Liliaceae; Lycopodium; Mentha-type; Mercurialis; Olea; Ostrya; Papaveraceae; Phillyrea; Phoenix; Pinus; Pistacia; Plantago; Plantago coronopus; Plantago lanceolata-type; Platanus; Poaceae; Polygonum; Polypodiaceae; Populus; Potentilla-type; Prunus; Quercus calliprinos-type; Quercus ithaburensis-type; Ranunculaceae; Rosaceae; Rubiaceae; Rumex; Salix; Sambucus; Sarcopoterium; Scabiosa; Scrophulariaceae; Symphytum; Tamarix; Thymelaea; Tubuliflorae; Typha angustifolia-type; Typha latifolia; Urtica; Varia; Vitis; Xanthium; Zizyphus; Zygophyllum
    Type: Dataset
    Format: text/tab-separated-values, 4640 data points
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  • 3
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    PANGAEA
    In:  Supplement to: Waldmann, Nicolas D; Torfstein, Adi; Stein, Mordechai (2010): Northward intrusions of low- and mid-latitude storms across the Saharo-Arabian belt during past interglacials. Geology, 38(6), 567-570, https://doi.org/10.1130/G30654.1
    Publication Date: 2024-01-03
    Description: The rain regime of the Levant during the late Quaternary was controlled primarily by Mediterranean cyclonic systems associated with North Atlantic climate shifts. Lake levels in the Dead Sea basin have been robust recorders of the regional hydrology and generally indicate highstand (wet) conditions throughout glacial intervals and lowstands (dry) during interglacials. However, sporadic deposition of travertines and speleothems occurred in the Negev Desert and Arava Valley during past interglacials, suggesting intrusions of humidity from southern sources probably in association with enhanced activity of mid-latitude Red Sea synoptic troughs and/or low-latitude tropical plumes. The southerly incursions of wetness were superimposed on the long-term interglacial Levantine arid conditions, as reflected by the current prevailing hyperaridity, and could have had an important impact on human migra- tion through the Red Sea-Dead Sea corridor.
    Keywords: DS-LL; Negev, Sinai Peninsula, Israel
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 4
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    In:  Supplement to: Miebach, Andrea; Chen, Chunzhu; Schwab, Markus J; Stein, Mordechai; Litt, Thomas (2017): Vegetation and climate during the Last Glacial high stand (ca. 28-22 ka BP) of the Sea of Galilee, northern Israel. Quaternary Science Reviews, 156, 47-56, https://doi.org/10.1016/j.quascirev.2016.11.013
    Publication Date: 2024-01-03
    Description: Despite ongoing discussions on hydroclimatic conditions in the southern Levant during the Last Glacial, detailed knowledge about the Levantine paleovegetation, which is an important indicator for the paleoclimate, is limited. To investigate the paleovegetation in northern Israel, we analyzed the pollen assemblage of a sediment core that was drilled at the Ohalo II archaeological site on the southwestern shore of the Sea of Galilee (Lake Kinneret). We refined the lithology and the age-depth model with the help of five new radiocarbon dates. The core comprises a continuous sediment profile of mainly laminated authigenic calcites and detrital material that deposited between ca. 28,000 and 22,500 years before present, when the Sea of Galilee rose above the modern lake level stand and temporarily merged with Lake Lisan, the precursor of the Dead Sea. The well-dated and high-resolution pollen record suggests that steppe vegetation with grasses, other herbs, and dwarf shrubs predominated in northern Israel during the investigated period. In contrast to the Holocene, there was no continuous vegetation belt of the Mediterranean biome in the vicinity of the Sea of Galilee. Mediterranean elements such as deciduous oaks only occurred in limited amounts and were probably patchily distributed. These results disagree with previous pollen-based hypotheses from the region that assumed the spread of Mediterranean forest during glacial periods. While the pollen data may indicate semiarid conditions in northern Israel and give no evidence of increased effective moisture, previous hydroclimatic studies suggested increased precipitation rates that are consistent with high lake levels (Sea of Galilee/Lake Lisan). Thus, we discuss factors influencing the pollen assemblage and the plant cover.
    Keywords: Acer; Adonis aestivalis-type; AGE; Age, comment; Alchemilla group; Alnus; Anagallis-type; Anemone coronaria; Apiaceae; Arboreal pollen; Artemisia; Asphodelus; Astragalus-type; Ballota-type; Betula; Bituminaria; Boraginaceae; Botryococcus; Brassicaceae; Caldesia parnassifolia; Campanulaceae; Caryophyllaceae; Castanea; Cedrus; Centaurea cyanus-type; Centaurea indeterminata; Centaurea jacea-type; Centaurea montana-type; Centaurea scabiosa-type; Cerealia-type; cf. Caldesia parnassifolia; cf. Campanulaceae; cf. Elaeagnus; cf. Euphorbia; cf. Parnassia palustris; cf. Populus; cf. Rhus group; cf. Ribes; cf. Scrophulariaceae; cf. Urticaceae; Chenopodiaceae; Cistus-type; Colchicum group; Convolvulus arvensis-type; Corylus; Cotinus; Cuscuta europaea-type; Cyperaceae; DEPTH, sediment/rock; Dinoflagellates; Dipsacaceae; Echinops; Ephedra distachya-type; Ephedra fragilis-type; Epilobium; Euphorbia; Fabaceae; Filipendula; Fraxinus; Galeopsis-type; Geranium; Haplophyllum; Hedera; Helianthemum-type; Helleborus foetidus-type; Helleborus niger-type; Helleborus viridis-type; Hippophae rhamnoides; Humulus-type; Hypericum; Ilex; Isoetes; Juglans; Juniperus; KIN2; Lemna; Liguliflorae; Liliaceae; Linum; Lycopodium; Lythrum; Malvaceae; Matthiola; Melampyrum; Mentha-type; Myriophyllum alterniflorum-type; Myriophyllum spicatum-type; Nitraria; Non arboreal pollen; Olea europaea; Onobrychis; Papaver rhoeas-type; Pediastrum; Phillyrea; Pimpinella-type; Pinus; Pistacia; Plantago; Platanus orientalis; Plumbaginaceae; Poaceae; Pollen, broken; Pollen, corroded; Pollen, crumpled; Pollen, total; Polygonaceae; Polygonum aviculare-type; Polypodiaceae; Potamogeton; Potentilla-type; Primulaceae; Prunus; Quercus calliprinos-type; Quercus ithaburensis-type; Ranunculaceae; Ranunculus lanuginosus-type; Rhamnaceae; Rhus group; Rosaceae; Rubiaceae; Rumex; Sagittaria-type; Salix; Salvia pratensis-type; Sample ID; Sample volume; Sarcopoterium spinosum-type; Saxifraga aizoides-type; Scrophulariaceae; Sea of Galilee, Israel; Solanaceae; Sorbus group; Sparganium-type; Spores, trilete; Staphylea; Symphytum; Tamarix; Thalictrum; Tilia; Trifolium-type; Tubuliflorae; Turgenia latifolia; Typha latifolia-type; Ulmus; Unknown pollen; Urticaceae; Urtica pilulifera-type; Varia; Vitis
    Type: Dataset
    Format: text/tab-separated-values, 8646 data points
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  • 5
    Publication Date: 2024-01-03
    Keywords: AGE; DS-LL; Level; Negev, Sinai Peninsula, Israel
    Type: Dataset
    Format: text/tab-separated-values, 182 data points
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  • 6
    Publication Date: 2024-01-03
    Keywords: AGE; DS-LL; Level; Negev, Sinai Peninsula, Israel
    Type: Dataset
    Format: text/tab-separated-values, 54 data points
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  • 7
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 382 (1996), S. 773-778 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] The lithosphere of the Arabian–Nubian shield was mainly formed during an interval of about 150 million years near the end of the Proterozoic aeon. The events recorded in the rocks of the shield indicate that an oceanic plateau, formed by the head of an upwelling mantle plume, ...
    Type of Medium: Electronic Resource
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  • 8
    Publication Date: 2007-02-09
    Print ISSN: 0939-6314
    Electronic ISSN: 1617-6278
    Topics: Archaeology , Biology
    Published by Springer
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  • 9
    Publication Date: 2011-11-01
    Description: A fundamental issue in the evolution of human culture concerns the route and conditions of anatomically modern hominids during the migration out of Africa. A particular question is, how could anatomically modern hominids cross the hyperarid Arabian deserts? Here we outline the evidence for significant presence of freshwater along the Red Sea shores during the last interglacial period. Freshwater caused an extensive recrystallization of coral reefs from aragonite to calcite, indicating uplift of the reefs through well-developed phreatic freshwater coastal aquifers. Applying novel open-system U-Th dating methodology to the calcitic corals, we dated the freshwater recrystallization to ca. 140 ka, consistent with other geological lines of evidence placing the migration of anatomically modern hominids out of Africa at the onset of the last interglacial.
    Print ISSN: 0091-7613
    Electronic ISSN: 1943-2682
    Topics: Geosciences
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  • 10
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