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  • 2020-2024  (7)
  • 2015-2019  (26)
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  • 1
    Keywords: Life sciences. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (392 pages)
    Edition: 1st ed.
    ISBN: 9783510655359
    DDC: 371
    Language: English
    Note: Cover -- Title -- Copyright -- Preface -- The Authors -- Table of Contents -- Chapter 1 African Research -- 1.1 Millennial spaces have always structured the African continent -- 1.1.1 Genetics, archaeology and geography -- 1.1.2 The genetic narrative -- 1.1.3 The role of archaeology -- 1.1.4 The build of the African continent -- 1.1.5 Longstanding contexts -- 1.1.6 The centre of Africa, void of Pleistocene humans -- 1.1.7 The volatile bow around the centre -- 1.1.8 The self-sufficient subcontinent to the south -- 1.1.9 The patchy east -- 1.1.10 Sahara Desert and Nile Valley -- 1.1.11 Remote margins: Atlas Mountains, Niger Inland Delta, Namib desert: oblivion and loss -- 1.2 Palaeoanthropological background -- 1.2.1 Early hominins -- 1.2.2 Origin of Homo and first expansions out of Africa -- 1.2.3 Archaic Homo sapiens in Africa -- 1.2.4 Anatomically modern humans -- 1.2.5 Biocultural evolution of Homo sapiens -- 1.3 Ethiopian lakes as paleoenvironmental and palaeoclimate archives -- 1.3.1 Regional setting of the Chew Bahir basin -- 1.3.2 Materials and Methods used for the analysis of the Chew Bahir record -- 1.3.3 Palaeoecological results based on the Chew Bahir record -- 1.3.4 Conclusion from a palaeoecological point of view -- 1.4 The role of tropical highlands in the dispersal of Homo sapiens -- 1.4.1 Introduction -- 1.4.2 Environmental background -- 1.4.3 The Middle Stone Age archaeological record -- 1.4.4 The earliest evidence of high-altitude occupation -- 1.4.5 The influence of climate in the dispersal of Homo sapiens from Africa -- 1.4.6 Conclusion -- 1.5 Ephemeral but not remote - Insights into the Late Pleistocene of North-East Africa -- 1.5.1 Introduction -- 1.5.2 Regional context -- 1.5.3 Environmental and climatological setting -- 1.5.4 Late Pleistocene record from Sodmein Cave. , 1.5.5 Open-air sites in Sodmein area and Wadi Qena area -- 1.5.6 Reconstructing the Late Pleistocene environment of the Eastern Desert -- 1.5.7 Re-occupation model of the Sahara after the hyper-arid Pleistocene -- 1.5.8 Conclusion -- 1.6 Hunter-gatherer mobility: Anthropological models of the first African frontier -- 1.6.1 Introduction -- 1.6.2 Frontiers of rationalism and colonial expansionism -- 1.6.3 The internal African frontier and the first African frontier -- 1.6.4 Fission and fusion pattern -- 1.6.5 The effects of nested developmental cycles -- 1.6.6 The Changing Composition Group Model -- 1.6.7 Modelling marriage rules -- 1.6.8 Conclusion -- 1.7 Summary -- 1.8 References -- Chapter 2 Middle East/Levant -- 2.1 The southern Levant as migration corridor and barrier -- 2.1.1 Physiographic and geologic settings -- 2.1.2 Climate -- 2.1.3 Present-day vegetation -- 2.1.4 Vegetation history: Dry or wet glacial in the Levant? -- 2.1.5 Lake-level history: increased glacial wetness or decreased evaporation? -- 2.2 The palaeoenvironment of the southern Levant during the last interglacial- glacial cycle -- 2.2.1 Vegetation history -- 2.2.2 Climate reconstruction -- 2.2.3 Biome modelling -- 2.2.4 Regional synthesis and implications for hominids -- 2.3 The Levantine Upper Palaeolithic seen from the Wadi Sabra archaeological and environmental record -- 2.3.1 Human migration crossed the latitudes -- 2.3.2 Various biomes share the Middle East -- 2.3.3 Environment, culture and human migration related -- 2.3.4 Middle Palaeolithic -- 2.3.5 Upper Palaeolithic -- 2.3.6 Early phase: only Lower Wadi Sabra occupied by humans -- 2.3.7 Evolved phase: occasional human visits to the Upper Wadi Sabra -- 2.3.8 Late phase: a human refuge in arid times? -- 2.3.9 The onset of the Epipalaeolithic: Wadi Sabra as marginal habitat. , 2.3.10 Geomorphological and sedimentological setting of the archaeological sites in the Wadi Sabra -- 2.3.11 Conclusion -- 2.4 Summary -- 2.5 References -- Chapter 3 South-Eastern Europe -- 3.1 South-Eastern Europe: The gateway for human migration towards Europe? -- 3.1.1 Physiographic and geological setting, climate and present-day vegetation -- 3.1.2 Outline and investigations presented in this chapter -- 3.2 Early Homo sapiens in South-East Europe: the evidence from Apidima Cave A -- 3.2.1 Homo sapiens: evolution and dispersal -- 3.2.2 The site of Apidima -- 3.3 Orbital and millennial climate oscillations and environment evolution in the Marmara-Balkan migration route since the Last Glacial -- 3.4 The speleothem record of the Mediterranean and Balkan region -- 3.4.1 The last glacial's speleothem record in the wider Mediterranean region -- 3.4.2 Rapid climate change at the transition from Neanderthals to modern humans -- 3.4.3 Towards process-understanding of environmental change during last glacial's D-O cycles -- 3.5 Palaeoclimatic evolution in Central and South-Eastern Europe during the last glacial based on aeolian sediments -- 3.5.1 The Banat - a geoarchaeological key area -- 3.5.2 The palaeoclimatic archive of the Middle Danube loess deposits -- 3.5.3 The palaeoclimatic archive of the Lower Danube loess deposits -- 3.5.4 Supraregional and global implications -- 3.6 Chronological constraints from tephra in South-Eastern European loess records -- 3.6.1 State-of-art of tephrochronological research in South-Eastern European loess -- 3.6.2 The Campanian Ignimbrite/Y-5 tephra (CI) -- 3.6.3 The so-called L2 tephra -- 3.6.4 The Bag tephra -- 3.6.5 Other prominent tephra layers -- 3.6.6 The Carpathian tephras -- 3.6.7 Outlook -- 3.7 The Upper Paleolithic in the Carpathian Basin: The European heart of Our Way to Europe. , 3.7.1 The early Upper Palaeolithic of the Carpathian Basin: Patterns of disorder -- 3.7.2 Ideas in motion: The technological approach and the contribution to human dispersal -- 3.7.3 Discussion: No clear direction -- 3.7.4 Conclusions: A weak vanguard -- 3.8 Summary -- 3.9 References -- Chapter 4 Population dynamics, mobility and human-environment interaction from the Palaeolithic to the Neolithic - a view from Central Europe to the world -- 4.1 Representations of demographic dynamics -- 4.1.1 Three types of representation -- 4.1.2 Relationship between the dominant and the segmentary representation -- 4.1.3 Comparison of interpretations -- 4.1.4 Stages and oscillations -- 4.1.5 Biological patterns -- 4.1.6 Vertical social differentiation -- 4.1.7 The fallacy of the so-called Malthusian trap -- 4.1.8 The fallacy of exhausting the environmental carrying capacity -- 4.1.9 Conclusion -- 4.2 Population dynamics of the Palaeolithic -- 4.2.1 Demographic estimates -- 4.2.2 The Cologne Protocol - approaching prehistoric demography -- 4.2.3 Upscaling - mind the gap -- 4.2.4 Diachronic population dynamics during the Upper and Final Palaeolithic of Europe -- 4.2.5 A spatially explicit, regional perspective on population dynamics -- 4.2.6 Demographic developments at global scale -- 4.2.7 Conclusion -- 4.3 Human-environment interaction -- 4.3.1 Cultural connectivity -- 4.3.2 A multisphere perspective on population dynamics, human-environment interaction and mobility in prehistoric Central Europe -- 4.3.3 Lithosphere/reliefsphere and population dynamics -- 4.3.4 Pedosphere and population dynamics -- 4.3.5 Pedosphere and human occupation during the Upper Palaeolithic -- 4.3.6 Terrestrial Hydrosphere and population dynamics -- 4.3.7 Biosphere and population dynamics -- 4.3.8 Biosphere, atmosphere and population dynamics -- 4.3.9 Fire and population dynamics. , 4.3.10 Conclusion -- 4.4 Summary -- 4.5 References -- Chapter 5 The Westernmost Mediterranean -- 5.1 Introduction -- 5.2 Palaeoecology and human settlement pattern (50-5 ka) -- 5.2.1 Geoarchives and palaeoenvironment -- 5.2.2 Human settlement pattern -- 5.3 Key Sites in Andalusia and the Eastern Rif -- 5.3.1 Sites in Andalusia -- 5.3.3 Sites in the Eastern Rif -- 5.4 On the Relevance of Borders - The Strait of Gibraltar and the Ebro Frontier Model -- 5.4.1 The Strait of Gibraltar - Bridge or Barrier -- 5.4.2 The Ebro Frontier Model - 20 years after -- 5.5 Summary -- 5.6 References -- Chapter 6 Modelling Human Dispersal in Space and Time -- 6.1 Introduction -- 6.2 Model Framework -- 6.2.1 Human Existence Potential -- 6.2.2 Human Mobility Model -- 6.2.3 Constrained Random Walk Model -- 6.3 Archaeological data -- 6.4 Human existence potential and kinematic applications -- 6.4.1 Probability of human existence: Aurignacian -- 6.4.2 Probability of human existence: Last Glacial Maximum -- 6.5 Impact of regional climate on human dispersal -- 6.6 Dynamic simulation of our way to Europe -- 6.7 Impact of the Heinrich Event 4 on human population in the Iberian Peninsula -- 6.8 Summary -- 6.9 References -- Chapter 7 Methods -- 7.1 Scientific Drilling -- 7.2 Palaeomagnetism and environmental magnetism -- 7.3 Varve chronology -- 7.4 Radiocarbon dating -- 7.5 Pollen dating and flow cytometry -- 7.6 Luminescence dating -- 7.7 U-Th dating of carbonates -- 7.8 Stable isotopes in speleothems as palaeoclimatic indicators -- 7.9 Pollen analysis -- 7.10 Black carbon analyses -- 7.11 Laboratory analysis of Loess palaeosol sequences -- 7.12 Palaeoclimate reconstructions based on botanical-climatological transfer functions -- Chapter 8 Epilogue: School needs science! - Approaches to Model and Promote Comparative Competences in Geography Education -- 8.1 Introduction. , 8.2 Theoretical approaches to comparison.
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  • 2
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    PANGAEA
    In:  Supplement to: Pickarski, Nadine; Kwiecien, Ola; Djamali, Morteza; Litt, Thomas (2015): Vegetation and environmental changes during the last interglacial in eastern Anatolia (Turkey): a new high-resolution pollen record from Lake Van. Palaeogeography, Palaeoclimatology, Palaeoecology, 435, 145-158, https://doi.org/10.1016/j.palaeo.2015.06.015
    Publication Date: 2023-01-13
    Description: A high-resolution multi-proxy record from Lake Van, eastern Anatolia, derived from a lacustrine sequence cored at the 357 m deep Ahlat Ridge (AR), allows a comprehensive view of paleoclimate and environmental history in the continental Near East during the last interglacial (LI). We combined paleovegetation (pollen), stable oxygen isotope (d18Obulk) and XRF data from the same sedimentary sequence, showing distinct variations during the period from 135 to 110 ka ago leading into and out of full interglacial conditions. The last interglacial plateau, as defined by the presence of thermophilous steppe-forest communities, lasted ca. 13.5 ka, from ~129.1-115.6 ka BP. The detailed palynological sequence at Lake Van documents a vegetation succession with several climatic phases: (I) the Pistacia zone (ca. 131.2-129.1 ka BP) indicates summer dryness and mild winter conditions during the initial warming, (II) the Quercus-Ulmus zone (ca. 129.1-127.2 ka BP) occurred during warm and humid climate conditions with enhanced evaporation, (III) the Carpinus zone (ca. 127.2-124.1 ka BP) suggest increasingly cooler and wetter conditions, and (IV) the expansion of Pinus at ~124.1 ka BP marks the onset of a colder/drier environment that extended into the interval of global ice growth. Pollen data suggest migration of thermophilous trees from refugial areas at the beginning of the last interglacial. Analogous to the current interglacial, the migration documents a time lag between the onset of climatic amelioration and the establishment of an oak steppe-forest, spanning 2.1 ka. Hence, the major difference between the last interglacial compared to the current interglacial (Holocene) is the abundance of Pinus as well as the decrease of deciduous broad-leaved trees, indicating higher continentality during the last interglacial. Finally, our results demonstrate intra-interglacial variability in the low mid-latitudes and suggest a close connection with the high-frequency climate variability recorded in Greenland ice cores.
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 3
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    PANGAEA
    In:  Supplement to: Pickarski, Nadine; Kwiecien, Ola; Langgut, Dafna; Litt, Thomas (2015): Abrupt climate and vegetation variability of eastern Anatolia during the last glacial. Climate of the Past, 11(11), 1491-1505, https://doi.org/10.5194/cp-11-1491-2015
    Publication Date: 2023-01-13
    Description: Detailed analyses of the Lake Van pollen, Ca/K ratio and stable oxygen isotope record allow the identification of millennial-scale vegetation and environmental changes in eastern Anatolia throughout the last glacial (~75-15 ka BP). The climate within the last glacial was cold and dry, with low arboreal pollen (AP) levels. The driest and coldest period corresponds to Marine Isotope Stage (MIS) 2 (~28-14.5 ka BP) dominated by the highest values of xerophytic steppe vegetation. Our high-resolution multi proxy record shows rapid expansions and contractions of tree populations that reflects variability in temperature and moisture availability. This rapid vegetation and environmental changes can be linked to the stadial-interstadial pattern of the Dansgaard-Oeschger (DO) events as recorded in the Greenland ice cores. Periods of reduced moisture availability were characterized by enhanced xerophytic species and high terrigenous input from the Lake Van catchment area. Furthermore, comparison with the marine realm reveals that the complex atmosphere-ocean interaction can be explained by the strength and position of the westerlies, which is responsible for the supply of humidity in eastern Anatolia. Influenced by diverse topography of the Lake Van catchment, larger DO interstadials (e.g. DO 19, 17-16, 14, 12 and 8) show the highest expansion of temperate species within the last glacial. However, Heinrich events (HE), characterized by highest concentrations of ice-rafted debris (IRD) in marine sediments, are identified in eastern Anatolia by AP values not lower and high steppe components not more abundant than during DO stadials. In addition, this work is a first attempt to establish a continuous microscopic charcoal record over the last glacial in the Near East, which documents an initial immediate response to millennial-scale climate and environmental variability and enables us to shed light on the history of fire activity during the last glacial.
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 4
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    PANGAEA
    In:  European Pollen Database (EPD)
    Publication Date: 2023-06-27
    Keywords: Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; EPD; Lake Van, Turkey; Lithology/composition/facies; PCUWI; Piston corer, UWITEC; VAN04-2
    Type: Dataset
    Format: text/tab-separated-values, 27 data points
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  • 5
    Publication Date: 2023-06-27
    Keywords: AGE; Age, comment; Age, maximum/old; Age, minimum/young; COMPCORE; Composite Core; Eastern Anatolian high plateau, Turkey; Lake_Van; Pollen assemblage; Pollen zone; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 40 data points
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  • 6
    Publication Date: 2023-06-27
    Keywords: AGE; COMPCORE; Composite Core; DEPTH, sediment/rock; Eastern Anatolian high plateau, Turkey; Lake_Van; Mass spectrometer DeltaPlusXL coupled to a Gasbench II; Sample code/label; δ18O, bulk carbonate
    Type: Dataset
    Format: text/tab-separated-values, 98 data points
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  • 7
    Publication Date: 2023-06-27
    Keywords: AGE; Calcium/Potassium ratio; COMPCORE; Composite Core; DEPTH, sediment/rock; Eastern Anatolian high plateau, Turkey; Lake_Van; X-ray fluorescence core scanner (XRF) III, Bremen
    Type: Dataset
    Format: text/tab-separated-values, 383 data points
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  • 8
    Publication Date: 2023-06-27
    Keywords: AGE; COMPCORE; Composite Core; DEPTH, sediment/rock; Eastern Anatolian high plateau, Turkey; Lake_Van; Mass spectrometer DeltaPlusXL coupled to a Gasbench II; Sample code/label; δ18O, bulk carbonate
    Type: Dataset
    Format: text/tab-separated-values, 400 data points
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  • 9
    Publication Date: 2023-06-27
    Keywords: AGE; Calcium/Potassium ratio; COMPCORE; Composite Core; DEPTH, sediment/rock; Eastern Anatolian high plateau, Turkey; Lake_Van; X-ray fluorescence core scanner (XRF) III, Bremen
    Type: Dataset
    Format: text/tab-separated-values, 1772 data points
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  • 10
    Publication Date: 2023-06-27
    Keywords: AGE; Age, comment; Age, maximum/old; Age, minimum/young; COMPCORE; Composite Core; Eastern Anatolian high plateau, Turkey; Lake_Van; Pollen assemblage; Pollen zone; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 40 data points
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