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Bernd Wünnemann

Dados Biográficos

ID5597985
NOMEBernd Wünnemann
PRENOMESBernd
SOBRENOMEWünnemann
ASSINATURAWÜNNEMANN B
AFILIAÇÕESFreie Universität Berlin
ORCID0000-0002-7172-735X
VERIFICADOSim
TOTAL DE OBRAS19
TOTAL DE CITAÇÕES17
TOTAL COMO AUTOR19
TOTAL COMO EDITOR0
PRIMEIRO ANO DE PUBLICAÇÃO1995
ANO MAIS RECENTE DE PUBLICAÇÃO2019
ÍNDICE H3
  • Holocene climate and civilization

    Open Access•Bahadur Singh Kotlia, Bernd Wünnemann•ARTICLE•Quaternary International•2019

  • A long arid interlude in the Indian summer monsoon during ∼4,350 to 3,450 cal. yr BP contemporaneous to displacement of the Indus valley civilization

    Open Access•Som Dutt, Anil K Gupta et al.•ARTICLE•Quaternary International•2018

  • A Process- and Provenance-Based Attempt to Unravel Inconsistent Radiocarbon Chronologies in Lake Sediments

    Open Access•Gregori Lockot, Arne Ramisch et al.•ARTICLE•Radiocarbon•2015•Citada por: 3•Referências: 49

    Aquatic macrophytes from a lacustrine environment are highly prone to a reservoir effect, resulting in an overestimation of age. This is often caused by the incorporation of dissolved carbon (CO 2 and HCO 3 – ) through photosynthesis from lake waters that have a different 14 C activity than the atmosphere. The atmosphere-water disparity is often produced by a mixing of carbon between the water body and its terrestrial surroundings, a process high…

  • Potential of pollen and non-pollen palynomorph records from Tso Moriri (Trans-Himalaya, NW India) for reconstructing Holocene limnology and human–environmental interactions

    Open Access•Christian Leipe, Dieter Demske et al.•ARTICLE•Quaternary International•2014

  • Early to mid-Holocene lake high-stand sediments at Lake Donggi Cona, northeastern Tibetan Plateau, China

    Open Access•Elisabeth Dietze, Bernd Wünnemann et al.•ARTICLE•Quaternary Research•2013

    Lake high-stand sediments are found in three onshore terraces at Lake Donggi Cona, northeastern Tibetan Plateau, and reveal characteristics of hydrological changes on lake shorelines triggered by climate change, geomorphological processes, and neo-tectonic movements. The terraces consist of fluvial–alluvial to littoral-lacustrine facies. End-member modeling of grain-size distributions allowed quantification of sediment transport processes and rel…

  • Basin morphology and seismic stratigraphy of Lake Kotokel, Baikal region, Russia

    Open Access•Yongzhan Zhang, Bernd Wünnemann et al.•ARTICLE•Quaternary International•2013

  • Proxies for Quaternary monsoon reconstruction on the Tibetan Plateau

    Open Access•Steffen Mischke, Bernd Wünnemann et al.•ARTICLE•Quaternary International•2013

  • Reply to “Comment on a study on Holocene foraminifera from the Aral Sea and West Siberian lakes and its implication for migration pathways” by S.A. Gusskov, Y.V. Kuzmin, E.Y. Zhakov

    Open Access•Frank Riedel, Annette Kossler et al.•ARTICLE•Quaternary International•2012

  • A study on Holocene foraminifera from the Aral Sea and West Siberian lakes and its implication for migration pathways

    Open Access•Frank Riedel, Annette Kossler et al.•ARTICLE•Quaternary International•2011

  • Lacustrine radiocarbon reservoir ages in Co Ngoin and Zigê Tangco, central Tibetan Plateau

    Open Access•Yanhong Wu, Shijie Li et al.•ARTICLE•Quaternary International•2010

  • Asian monsoon variability

    Open Access•Bernd Wünnemann, Bahadur Kotlia et al.•ARTICLE•Quaternary International•2010

  • Hydrological changes and Holocene climate variations in NW China, inferred from lake sediments of Juyanze palaeolake by factor analyses

    Open Access•Kai Hartmann, Bernd Wünnemann•ARTICLE•Quaternary International•2009

  • Holocene climate variability in arid Asia

    Open Access•Fahu Chen, Jonathan Holmes et al.•ARTICLE•Quaternary International•2009

  • Holocene moisture evolution in arid central Asia and its out-of-phase relationship with Asian monsoon history

    Open Access•Fahu Chen, Zicheng Yu et al.•ARTICLE•Quaternary Science Reviews•2008

  • Withdrawn

    Open Access•Mei-lin Yang, Fa-hu Chen et al.•ARTICLE•Quaternary International•2008

  • Archaeology and climate

    Open Access•Nikolaus G O Boroffka, Nikolaus Boroffka et al.•ARTICLE•Geoarchaeology•2006•Citada por: 4

    New archaeological and geomorphologic data collected adjacent to the Aral Sea show lake‐level stands during the late Pleistocene and the past 5000 years. On the northern and southern shores, archaeological sites from the Palaeolithic through the Late Middle Ages contain evidence of various cultures and economies. Changes in settlement activity during the mid‐Holocene are related to several major lake‐level oscillations. Some of them, especially t…

  • A general cooling trend on the central Tibetan Plateau throughout the Holocene recorded by the Lake Zigetang pollen spectra

    Open Access•Ulrike Herzschuh, Katja Winter et al.•ARTICLE•Quaternary International•2006•Citada por: 6•Referências: 41

  • Modern pollen-based interpretations of mid-Holocene palaeoclimate (8500 to 3000 cal. BP) at the southern margin of the Tengger Desert, northwestern China

    Open Access•Yuzhen Ma, Hucai Zhang et al.•ARTICLE•The Holocene•2004•Citada por: 4•Referências: 2

    The focus of this paper is on the reconstruction of the mid-Holocene climatic changes based on the pollen records contained in a 6.2 m thick section in the southern part of the Tengger Desert, northwestern China. To understand the modem analogues of the mid-Holocene changes, modem pollen spectra across different vegetation zones from the Qilian Mountains to the lowland Tengger Desert were studied first. Four pollen combinations were identified, c…

  • Lake Evolution in the Tengger Desert, Northwestern China, during the Last 40,000 Years

    Open Access•Hans‐Joachim Pachur, Hans-Joachim Pachur et al.•ARTICLE•Quaternary Research•1995

    Climatic changes inferred from lacustrine deposits and lake-level fluctuations in northwestern and central China are mainly based on paleoclimatic records from the Tibetan Plateau, while there is still a lack of data relating to the semiarid/arid desert regions of Inner Mongolia. In the Tengger Desert, different paleolake levels at Baijian Hu are documented by six paleoshorelines and stratified lake carbonates. The highest lake level occurred ca.…

  • A general cooling trend on the central Tibetan Plateau throughout the Holocene recorded by the Lake Zigetang pollen spectra

    Open Access•Ulrike Herzschuh, Katja Winter et al.•ARTICLE•Quaternary International•2006•Citada por: 6•Referências: 41

  • Archaeology and climate

    Open Access•Nikolaus G O Boroffka, Nikolaus Boroffka et al.•ARTICLE•Geoarchaeology•2006•Citada por: 4

    New archaeological and geomorphologic data collected adjacent to the Aral Sea show lake‐level stands during the late Pleistocene and the past 5000 years. On the northern and southern shores, archaeological sites from the Palaeolithic through the Late Middle Ages contain evidence of various cultures and economies. Changes in settlement activity during the mid‐Holocene are related to several major lake‐level oscillations. Some of them, especially t…

  • Modern pollen-based interpretations of mid-Holocene palaeoclimate (8500 to 3000 cal. BP) at the southern margin of the Tengger Desert, northwestern China

    Open Access•Yuzhen Ma, Hucai Zhang et al.•ARTICLE•The Holocene•2004•Citada por: 4•Referências: 2

    The focus of this paper is on the reconstruction of the mid-Holocene climatic changes based on the pollen records contained in a 6.2 m thick section in the southern part of the Tengger Desert, northwestern China. To understand the modem analogues of the mid-Holocene changes, modem pollen spectra across different vegetation zones from the Qilian Mountains to the lowland Tengger Desert were studied first. Four pollen combinations were identified, c…

  • A Process- and Provenance-Based Attempt to Unravel Inconsistent Radiocarbon Chronologies in Lake Sediments

    Open Access•Gregori Lockot, Arne Ramisch et al.•ARTICLE•Radiocarbon•2015•Citada por: 3•Referências: 49

    Aquatic macrophytes from a lacustrine environment are highly prone to a reservoir effect, resulting in an overestimation of age. This is often caused by the incorporation of dissolved carbon (CO 2 and HCO 3 – ) through photosynthesis from lake waters that have a different 14 C activity than the atmosphere. The atmosphere-water disparity is often produced by a mixing of carbon between the water body and its terrestrial surroundings, a process high…

  • Lake Evolution in the Tengger Desert, Northwestern China, during the Last 40,000 Years

    Open Access•Hans‐Joachim Pachur, Hans-Joachim Pachur et al.•ARTICLE•Quaternary Research•1995

    Climatic changes inferred from lacustrine deposits and lake-level fluctuations in northwestern and central China are mainly based on paleoclimatic records from the Tibetan Plateau, while there is still a lack of data relating to the semiarid/arid desert regions of Inner Mongolia. In the Tengger Desert, different paleolake levels at Baijian Hu are documented by six paleoshorelines and stratified lake carbonates. The highest lake level occurred ca.…

  • Modern pollen-based interpretations of mid-Holocene palaeoclimate (8500 to 3000 cal. BP) at the southern margin of the Tengger Desert, northwestern China

    Open Access•Yuzhen Ma, Hucai Zhang et al.•ARTICLE•The Holocene•2004•Citada por: 4•Referências: 2

    The focus of this paper is on the reconstruction of the mid-Holocene climatic changes based on the pollen records contained in a 6.2 m thick section in the southern part of the Tengger Desert, northwestern China. To understand the modem analogues of the mid-Holocene changes, modem pollen spectra across different vegetation zones from the Qilian Mountains to the lowland Tengger Desert were studied first. Four pollen combinations were identified, c…

  • Archaeology and climate

    Open Access•Nikolaus G O Boroffka, Nikolaus Boroffka et al.•ARTICLE•Geoarchaeology•2006•Citada por: 4

    New archaeological and geomorphologic data collected adjacent to the Aral Sea show lake‐level stands during the late Pleistocene and the past 5000 years. On the northern and southern shores, archaeological sites from the Palaeolithic through the Late Middle Ages contain evidence of various cultures and economies. Changes in settlement activity during the mid‐Holocene are related to several major lake‐level oscillations. Some of them, especially t…

  • A general cooling trend on the central Tibetan Plateau throughout the Holocene recorded by the Lake Zigetang pollen spectra

    Open Access•Ulrike Herzschuh, Katja Winter et al.•ARTICLE•Quaternary International•2006•Citada por: 6•Referências: 41

  • Holocene moisture evolution in arid central Asia and its out-of-phase relationship with Asian monsoon history

    Open Access•Fahu Chen, Zicheng Yu et al.•ARTICLE•Quaternary Science Reviews•2008

  • Withdrawn

    Open Access•Mei-lin Yang, Fa-hu Chen et al.•ARTICLE•Quaternary International•2008

  • Hydrological changes and Holocene climate variations in NW China, inferred from lake sediments of Juyanze palaeolake by factor analyses

    Open Access•Kai Hartmann, Bernd Wünnemann•ARTICLE•Quaternary International•2009

  • Holocene climate variability in arid Asia

    Open Access•Fahu Chen, Jonathan Holmes et al.•ARTICLE•Quaternary International•2009

  • Lacustrine radiocarbon reservoir ages in Co Ngoin and Zigê Tangco, central Tibetan Plateau

    Open Access•Yanhong Wu, Shijie Li et al.•ARTICLE•Quaternary International•2010

  • Asian monsoon variability

    Open Access•Bernd Wünnemann, Bahadur Kotlia et al.•ARTICLE•Quaternary International•2010

  • A study on Holocene foraminifera from the Aral Sea and West Siberian lakes and its implication for migration pathways

    Open Access•Frank Riedel, Annette Kossler et al.•ARTICLE•Quaternary International•2011

  • Reply to “Comment on a study on Holocene foraminifera from the Aral Sea and West Siberian lakes and its implication for migration pathways” by S.A. Gusskov, Y.V. Kuzmin, E.Y. Zhakov

    Open Access•Frank Riedel, Annette Kossler et al.•ARTICLE•Quaternary International•2012

  • Early to mid-Holocene lake high-stand sediments at Lake Donggi Cona, northeastern Tibetan Plateau, China

    Open Access•Elisabeth Dietze, Bernd Wünnemann et al.•ARTICLE•Quaternary Research•2013

    Lake high-stand sediments are found in three onshore terraces at Lake Donggi Cona, northeastern Tibetan Plateau, and reveal characteristics of hydrological changes on lake shorelines triggered by climate change, geomorphological processes, and neo-tectonic movements. The terraces consist of fluvial–alluvial to littoral-lacustrine facies. End-member modeling of grain-size distributions allowed quantification of sediment transport processes and rel…

  • Basin morphology and seismic stratigraphy of Lake Kotokel, Baikal region, Russia

    Open Access•Yongzhan Zhang, Bernd Wünnemann et al.•ARTICLE•Quaternary International•2013

  • Proxies for Quaternary monsoon reconstruction on the Tibetan Plateau

    Open Access•Steffen Mischke, Bernd Wünnemann et al.•ARTICLE•Quaternary International•2013

  • Potential of pollen and non-pollen palynomorph records from Tso Moriri (Trans-Himalaya, NW India) for reconstructing Holocene limnology and human–environmental interactions

    Open Access•Christian Leipe, Dieter Demske et al.•ARTICLE•Quaternary International•2014

  • A Process- and Provenance-Based Attempt to Unravel Inconsistent Radiocarbon Chronologies in Lake Sediments

    Open Access•Gregori Lockot, Arne Ramisch et al.•ARTICLE•Radiocarbon•2015•Citada por: 3•Referências: 49

    Aquatic macrophytes from a lacustrine environment are highly prone to a reservoir effect, resulting in an overestimation of age. This is often caused by the incorporation of dissolved carbon (CO 2 and HCO 3 – ) through photosynthesis from lake waters that have a different 14 C activity than the atmosphere. The atmosphere-water disparity is often produced by a mixing of carbon between the water body and its terrestrial surroundings, a process high…

  • A long arid interlude in the Indian summer monsoon during ∼4,350 to 3,450 cal. yr BP contemporaneous to displacement of the Indus valley civilization

    Open Access•Som Dutt, Anil K Gupta et al.•ARTICLE•Quaternary International•2018

  • Holocene climate and civilization

    Open Access•Bahadur Singh Kotlia, Bernd Wünnemann•ARTICLE•Quaternary International•2019

Geology and Paleoclimatology Research (18 obras) · Holocene (17 obras) · Geology (16 obras) · Physical geography (15 obras) · Paleontology (14 obras) · Geography (13 obras) · Oceanography (10 obras) · Geological formations and processes (8 obras) · Climate change (7 obras) · Monsoon (7 obras)

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