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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
    In: Quaternary science reviews, Amsterdam [u.a.] : Elsevier, 1982, 28(2009), 15/16, Seite 1555-1567, 0277-3791
    In: volume:28
    In: year:2009
    In: number:15/16
    In: pages:1555-1567
    Description / Table of Contents: Lake Van is the fourth largest terminal lake in the world (volume 607 km3, area 3570 km2, maximum depth 460 m), extending for 130 km WSWENE on the Eastern Anatolian High Plateau, Turkey. The sedimentary record of Lake Van, partly laminated, has the potential to obtain a long and continuous continental sequence that covers several glacialinterglacial cycles (ca 500 kyr). Therefore, Lake Van is a key site within the International Continental Scientific Drilling Program (ICDP) for the investigation of the Quaternary climate evolution in the Near East (‘PALEOVAN’). As preparation for an ICDP drilling campaign, a site survey was carried out during the past years. We collected 50 seismic profiles with a total length of ~850 km to identify continuous undisturbed sedimentary sequences for potential ICDP locations. Based on the seismic results, we cored 10 different locations to water depths of up to 420 m. Multidisciplinary scientific work at positions of a proposed ICDP drill site included measurements of magnetic susceptibility, physical properties, stable isotopes, XRF scans, and pollen and spores. This core extends back to the Last Glacial Maximum (LGM), a more extended record than all the other Lake Van cores obtained to date. Both coring and seismic data do not show any indication that the deepest part of the lake (Tatvan Basin, Ahlat Ridge) was dry or almost dry during past times. These results show potential for obtaining a continuous undisturbed, long continental palaeoclimate record. In addition, this paper discusses the potential of "PALEOVAN" to establish new results on the dynamics of lake level fluctuations, noble gas concentration in pore water of the lake sediment, history of volcanism and volcanic activities based on tephrostratigraphy, and paleoseismic and earthquake activities.
    Type of Medium: Online Resource
    Pages: Ill., graph. Darst
    ISSN: 0277-3791
    Language: English
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  • 3
    ISSN: 1617-6278
    Keywords: Palaeoclimate ; Stable isotopes ; Eemian ; Early Weichselian ; Central Germany
    Source: Springer Online Journal Archives 1860-2000
    Topics: Archaeology , Biology
    Notes: Abstract This paper reviews the evidence from terrestrial palaeoenvironmental records in north-central Europe and, in particular, central Germany, which relates to the controversial proposition that there were strong climate oscillations during the last interglacial (oxygen isotope substage 5e). In contrast to the evidence from the GRIP ice core at Summit, Greenland, and a recent palaeoclimate reconstruction based on the pollen profile from Bispingen, Germany, the evaluation of the palaeobotanical and the stable isotope data presented here strongly suggests relatively stable temperature for most of the Eemian and with instability confined to the beginning and end of the interglacial. High amplitude temperature variations can be seen in both the Early Weichselian pollen and isotope records. It is argued that this pattern of climate development is applicable to most of continental north-central Europe.
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    Springer
    Vegetation history and archaeobotany 1 (1992), S. 69-74 
    ISSN: 1617-6278
    Keywords: Neolithic ; Central Germany ; Holocene ; Pedology
    Source: Springer Online Journal Archives 1860-2000
    Topics: Archaeology , Biology
    Notes: Abstract At present the central part of the Elbe-Saale area is characterized by subcontinental climatic conditions. Palynological investigations at Zöschen show that, even in pre-Neolithic times, the composition of the primeval forest in this part of Germany had its own distinctive features. On the basis of the palynological results, the existence of natural steppe Holocene is improbable, the region being covered by forests since ca. 9 500 B.P., i.e. the Preboreal. The appearance of anthropochores or culture dependent plants and the beginning of flood loam sedimentation as a result of soil erosion indicate human impact from ca. 6 000 B.P., i.e. the end of the older Atlantic. At Eilsleben changes of tree and shrub frequencies are combined with the occurrence of anthropogenic indicator herb species. These palynological features suggest agricultural expansion phases that are interrupted by regression phases in the early and middle Neolithic (ca. 6 500-2 500 B.P.).
    Type of Medium: Electronic Resource
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  • 5
    Publication Date: 2012-04-11
    Type: Conference or Workshop Item , NonPeerReviewed
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  • 6
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    Unknown
    AGU (American Geophysical Union)
    In:  Eos, Transactions American Geophysical Union, 92 (51). pp. 477-479.
    Publication Date: 2017-02-10
    Description: Sedimentary archives host a wealth of information that can be used to reconstruct paleoclimate as well as the tectonic and volcanic histories of specific regions. Long and continuous archives from the oceans have been collected in thousands of locations by scientific ocean drilling programs over the past 40 years. In contrast, suitable continental archives are rare because terrestrial environments are generally nondepositional and/or subject to erosion. Lake sediments provide ideal drilling targets to overcome this limitation if suitable lakes at key locations have existed continuously for a long time.
    Type: Article , NonPeerReviewed
    Format: text
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  • 7
    Publication Date: 2012-07-06
    Type: Conference or Workshop Item , NonPeerReviewed
    Format: text
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  • 8
    Publication Date: 2019-07-03
    Description: Lake Van is the fourth largest terminal lake in the world (volume 607 km(3), area 3570 km(2), maximum depth 460 m), extending for 130 km WSW-ENE on the Eastern Anatolian High Plateau, Turkey. The sedimentary record of Lake Van, partly laminated, has the potential to obtain a long and continuous continental sequence that covers several glacial-interglacial cycles (ca 500 kyr). Therefore, Lake Van is a key site within the International Continental Scientific Drilling Program (ICDP) for the investigation of the Quaternary climate evolution in the Near East ('PALEOVAN'). As preparation for an ICDP drilling campaign, a site survey was carried out during the past years. We collected 50 seismic profiles with a total length of similar to 850 km to identify continuous undisturbed sedimentary sequences for potential ICDP locations. Based on the seismic results, we cored 10 different locations to water depths of up to 420 m. Multidisciplinary scientific work at positions of a proposed ICDP drill site included measurements of magnetic susceptibility, physical properties, stable isotopes, XRF scans, and pollen and spores. This core extends back to the Last Glacial Maximum (LGM), a more extended record than all the other Lake Van cores obtained to date. Both coring and seismic data do not show any indication that the deepest part of the lake (Tatvan Basin, Ahlat Ridge) was dry or almost dry during past times. These results show potential for obtaining a continuous undisturbed, long continental palaeoclimate record. In addition, this paper discusses the potential of 'PALEOVAN' to establish new results on the dynamics of lake level fluctuations, noble gas concentration in pore water of the lake sediment, history of volcanism and volcanic activities based on tephrostratigraphy, and paleoseismic and earthquake activities. (C) 2009 Elsevier Ltd. All rights reserved.
    Type: Article , PeerReviewed
    Format: text
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  • 9
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    Unknown
    Deutsche Forschungsgemeinschaft
    In:  [Poster] In: IODP-ICDP Kolloquium, 09.03.-11.03.2010, Frankfurt, Main . IODP-ICDP Kolloquium 2010 Geozentrum Frankfurt : 9. - 11. März 2010 ; Goethe-Universität Frankfurt .
    Publication Date: 2012-02-23
    Type: Conference or Workshop Item , NonPeerReviewed
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  • 10
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    Unknown
    Copernicus
    In:  [Poster] In: EGU General Assembly 2011, 03.04.-08.04.2011, Vienna, Austria .
    Publication Date: 2012-07-06
    Description: EGU2011-1847-3 Lake Van is a lake by volume of 607 km3 and a maximum depth of 450 meters in a tectonically active zone in eastern Anatolia, Turkey. In summer 2010, Lake Van was the target of a deep drilling campaign (PaleoVan) in the frame of ICDP (International Continental Scientific Drilling Program). Two sites were drilled based on reflection seismic data collected during a seismic campaign in 2004. Here we present a first joint interpretation of the seismic and drilling data. Interpretation of seismic reflection data from lake reveals three physiographic provinces: a lacustrine shelf, a lacustrine slope, and a deep, relatively flat lake basin. The most prominent features of the lacustrine shelf and slope are prograding deltaic sequences, numerous unconformities, submerged channels, as well as closely spaced U- and/or V-shaped depressions, reflecting the variable lake level history of Lake Van. The seismic units of the shelf are dominantly composed of low-to-good continuity, variable amplitude reflections interpreted as fluvial deposits. The lake consists of three prominent basins (Tatvan, Deveboynu, and Northern Basins), separated by basement highs or ridges (Ahlat Ridge). The seismic units corresponding to these basins mainly consist of low to very high amplitude, well-stratified reflection patterns. Chaotic reflections are seen in parts of these basins. The Deveboynu Basin consists mainly of chaotic reflections. The Tatvan and Northern Basins are characterized by an alternating succession of well-stratified and chaotic reflecting layers. The chaotic seismic facies are interpreted as slump and slide deposits, which are probably the result of quick lake level fluctuations and/or earthquakes. The moderateto high amplitude, well-stratified facies seen in the deep parts of the basins away from the terrigenous sediment sources are interpreted as lacustrine deposits and tephra layers. The total sediment thickness in the deep parts of the lake is over 400 m. Prominent clinoforms indicate the initial flooding of Lake Van about 500 ka ago. The acoustic basement and the sediments lying on top of the basement in the southern part of the lake are disrupted by various intrusions and extrusions suggesting active volcanism. Synthetic seismograms calculated based on core logging, wire-line logging and check shot data will allow the correlation between seismic and drill data. This approach will allow extrapolating the stratigraphy from the wells to 3D-space by using the seismic data.
    Type: Conference or Workshop Item , NonPeerReviewed
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