Bernd Wünnemann
Dados Biográficos
| ID | 5597985 |
|---|---|
| NOME | Bernd Wünnemann |
| PRENOMES | Bernd |
| SOBRENOME | Wünnemann |
| ASSINATURA | WÜNNEMANN B |
| AFILIAÇÕES | Freie Universität Berlin |
| ORCID | 0000-0002-7172-735X |
| VERIFICADO | Sim |
| TOTAL DE OBRAS | 19 |
| TOTAL DE CITAÇÕES | 17 |
| TOTAL COMO AUTOR | 19 |
| TOTAL COMO EDITOR | 0 |
| PRIMEIRO ANO DE PUBLICAÇÃO | 1995 |
| ANO MAIS RECENTE DE PUBLICAÇÃO | 2019 |
| ÍNDICE H | 3 |
Holocene climate and civilization
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
A Process- and Provenance-Based Attempt to Unravel Inconsistent Radiocarbon Chronologies in Lake Sediments
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
Early to mid-Holocene lake high-stand sediments at Lake Donggi Cona, northeastern Tibetan Plateau, China
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
Proxies for Quaternary monsoon reconstruction on the Tibetan Plateau
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
A study on Holocene foraminifera from the Aral Sea and West Siberian lakes and its implication for migration pathways
Lacustrine radiocarbon reservoir ages in Co Ngoin and Zigê Tangco, central Tibetan Plateau
Asian monsoon variability
Hydrological changes and Holocene climate variations in NW China, inferred from lake sediments of Juyanze palaeolake by factor analyses
Holocene climate variability in arid Asia
Holocene moisture evolution in arid central Asia and its out-of-phase relationship with Asian monsoon history
Withdrawn
Archaeology and climate
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
Modern pollen-based interpretations of mid-Holocene palaeoclimate (8500 to 3000 cal. BP) at the southern margin of the Tengger Desert, northwestern China
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
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
Archaeology and climate
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
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
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
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
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
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
Holocene moisture evolution in arid central Asia and its out-of-phase relationship with Asian monsoon history
Withdrawn
Hydrological changes and Holocene climate variations in NW China, inferred from lake sediments of Juyanze palaeolake by factor analyses
Holocene climate variability in arid Asia
Lacustrine radiocarbon reservoir ages in Co Ngoin and Zigê Tangco, central Tibetan Plateau
Asian monsoon variability
A study on Holocene foraminifera from the Aral Sea and West Siberian lakes and its implication for migration pathways
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
Early to mid-Holocene lake high-stand sediments at Lake Donggi Cona, northeastern Tibetan Plateau, China
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
Proxies for Quaternary monsoon reconstruction on the Tibetan Plateau
Potential of pollen and non-pollen palynomorph records from Tso Moriri (Trans-Himalaya, NW India) for reconstructing Holocene limnology and human–environmental interactions
A Process- and Provenance-Based Attempt to Unravel Inconsistent Radiocarbon Chronologies in Lake Sediments
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
Holocene climate and civilization
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)