A5081239872- Geology and Paleoclimatology Research
- Geological formations and processes
- Pleistocene-Era Hominins and Archaeology
- Aeolian processes and effects
- Methane Hydrates and Related Phenomena
- Archaeology and ancient environmental studies
- Isotope Analysis in Ecology
- Cryospheric studies and observations
- earthquake and tectonic studies
- Plant Ecology and Soil Science
- Climate change and permafrost
- Tree-ring climate responses
- Urban Green Space and Health
- Coastal wetland ecosystem dynamics
- Planetary Science and Exploration
- Pacific and Southeast Asian Studies
- Geochemistry and Elemental Analysis
- Noise Effects and Management
- Climate variability and models
- Heavy metals in environment
- Geological and Geophysical Studies
- Geochemistry and Geologic Mapping
- Geomagnetism and Paleomagnetism Studies
- Crystallization and Solubility Studies
- Infection Control and Ventilation
Nanjing Institute of Geography and Limnology
2016-2025
Chinese Academy of Sciences
2016-2025
Chongqing University
2015-2025
Beijing Normal University
2022-2024
University of Chinese Academy of Sciences
2009-2024
State Key Laboratory of Lake Science and Environment
2021-2023
Institute of Earth Environment
2020-2023
Qinghai Normal University
2021-2022
Qinghai University
2022
East China Normal University
2021-2022
Paleolithic occupation of Tibet Human colonization the high-altitude Tibetan Plateau has generally been thought to have confined past few thousand years Holocene. Zhang et al. report an investigation Nwya Devu archaeological site in central Tibet, 4600 meters above sea level, with dates ∼40 30 ago (see Perspective by and Dennell). The yielded a range stone tools, indicating adaptive ability early modern humans harsh environment “roof world.” findings also suggest that people from Siberia may...
Abstract Zhuyeze palaeolake is a terminal lake situated in the arid northern China East Asian monsoon margin. In order to examine Holocene palaeoclimatic change margin, Qingtu Lake section (QTL) from sampled high resolution. Palaeoclimatic proxies such as grain size, carbonate, TOC, C/N and δ 13 C of organic matter, were analyzed; eleven 14 samples six optically stimulated luminescence (OSL) dated provide chronological control. We also investigated geomorphic features shorelines this area....
Organic carbon burial (OCB) in lakes, a critical component of the global cycle, surpasses that oceans, yet its response to warming and associated feedbacks remains poorly understood. Using well-dated biomarker sequence from southern Tibetan Plateau comprehensive analysis Holocene total organic variations lakes across region, here we demonstrate lake OCB significantly declined throughout Holocene, closely linked changes temperature seasonality. Process-based land surface model simulations...
Understanding the Holocene climate changes (especially moisture variation) and their mechanisms in semiarid–arid Central Asia (SCA) is very important, as water availability crucial for sustainable developments this area. This study presents chronostratigraphy of an aeolian sedimentary sequence from Bayanbulak Basin (Xinjiang, NW China), aiming to infer history SCA. Luminescence dating technique was selected construct age framework section. Since luminescence signal intensity quartz samples...
Abstract Mollisols are highly fertile soils and function as significant carbon reservoirs. However, determining their ages formation processes is challenging due to extensive pedoturbation, which undermines conventional dating methods. Here, we employed luminescence, a light‐sensitive property of minerals widely used in geological dating, investigate quantify soil mixing. We analyzed over 2,400 luminescence individual K‐feldspar grains from Mollisol profile Northeast China, for the first...
Abstract The evolution processes and forcing mechanisms of the Horqin dunefield in northern China are poorly understood. In this study, systematic OSL dating multiple sites is used together with pollen analysis a representative section order to reconstruct since Last Glacial Maximum (LGM). Our results show that there was extensive dune mobilization 25–10 ka, transition stabilization 10–8 considerable 8–3 episodes after 3 ka. Comparison dunefields during Holocene showed Asian monsoon...