A5083268016- Geology and Paleoclimatology Research
- Geological and Geochemical Analysis
- Geomagnetism and Paleomagnetism Studies
- Paleontology and Stratigraphy of Fossils
- Geological formations and processes
- Geological and Geophysical Studies
- Evolution and Paleontology Studies
- earthquake and tectonic studies
- Pleistocene-Era Hominins and Archaeology
- Hydrocarbon exploration and reservoir analysis
- Geochemistry and Elemental Analysis
- Plant Diversity and Evolution
- Geochemistry and Geologic Mapping
- High-pressure geophysics and materials
- Aeolian processes and effects
- Groundwater and Isotope Geochemistry
- Geological Studies and Exploration
- Isotope Analysis in Ecology
- Methane Hydrates and Related Phenomena
- Climate change and permafrost
- Archaeology and ancient environmental studies
- Landslides and related hazards
- Remote Sensing and Land Use
- Plant Ecology and Soil Science
- Paleontology and Evolutionary Biology
Fuzhou University
2025
Guangdong Medical College
2025
Chinese Academy of Sciences
2015-2024
University of Chinese Academy of Sciences
2017-2024
Institute of Tibetan Plateau Research
2015-2024
Sun Yat-sen University
2020-2024
Fifth Affiliated Hospital of Sun Yat-sen University
2020-2024
Baidu (China)
2024
National Engineering Research Center for Wheat
2023
Jilin Agricultural University
2023
We present severe acute respiratory syndrome coronavirus 2 (SARS-CoV-2) real-time RT-PCR results of all and faecal samples from patients with disease 2019 (COVID-19) at the Fifth Affiliated Hospital Sun Yat-sen University, Zhuhai, China, throughout course their illness obligated quarantine period. Real-time was used to detect COVID-19 following recommended protocol (appendix p 1). Patients suspected SARS-CoV-2 were confirmed after two sequential positive tract sample results. Respiratory...
Abstract The way in which the NE Tibetan Plateau uplifted and its impact on climatic change are crucial to understanding evolution of development present geomorphology climate Central East Asia. This paper is not a comprehensive review current thinking but instead synthesises our past decades work together with number new findings. dating Late Cenozoic basin sediments tectonic demonstrates that rapid persistent rise this plateau began ~8 ± 1 Ma followed by stepwise accelerated at ~3.6 Ma,...
Knowledge of the topographic evolution Tibetan Plateau is essential for understanding its construction and influences on climate, environment, biodiversity. Previous elevations estimated from stable isotope records Lunpola Basin in central Tibet, which indicate a high plateau since at least 35 Ma, are challenged by recent discoveries low-elevation tropical fossils apparently deposited 25.5 Ma. Here, we use magnetostratigraphic radiochronologic dating to revise chronology elevation estimates...
The uplift of the Tibet Plateau (TP) during Miocene is crucial to understanding evolution Asian monsoon regimes and alpine biodiversity. However, northern (NTP) remains poorly investigated. We use pollen records montane conifers (Tsuga, Podocarpus, Abies, Picea) as a new paleoaltimetry construct two parallel midrange paleoelevation sequences in NTP at 1332 ± 189 m 433 m, respectively, Middle [~15 million years ago (Ma)]. Both midranges increased rapidly 3685 87 Late (~11 Ma) east, 3589 62 ~7...
Research Article| September 01, 2005 Late Cenozoic deformation and uplift of the NE Tibetan Plateau: Evidence from high-resolution magnetostratigraphy Guide Basin, Qinghai Province, China Xiaomin Fang; Fang 1Institute Plateau Research, Chinese Academy Science, P.O. Box 2871, Beilin North Str., Beijing 100085, China, National Laboratory Western China's Environmental Systems, Ministry Education College Resources Environment, Lanzhou University, Gansu 730000, Search for other works by this...
Phenological cold/warm events recorded in Chinese historical documents are used to reconstruct, at 10–30 years' resolution, winter half-year (October April) temperatures for the past 2000 years central region of eastern China. Because uneven spatial and temporal distribution phenological records, reconstruction regional mean temperature involves two steps: individual sites within calculation mean. For a single site, involves: identifying difference dates both modern records; establishing...
The Xining subbasin of the Longzhong basin holds longest continuous Cenozoic stratigraphic record at margin northeastern Tibetan Plateau. Despite a rich biostratigraphic content (including Xiejia mammal fauna), tectonic evolution is largely unconstrained. In this study we present stratigraphic, biostratigraphic, and magnetostratigraphic results that provide basis for reconstructing with respect to adjacent regions Magnetostratigraphic analysis from three red bed sections in indicates...
Abstract Plate-tectonic processes have long been thought to be the major cause of Cenozoic global carbon cycle, and cooling by uplift Tibetan Plateau through enhancing silicate weathering organic burial and/or obducted ophiolites during closure Neo-Tethys Ocean. However, imbalance resulting from accelerated CO2 consumption a relatively stable input volcanic degassing should depleted atmospheric within few million years; therefore, negative feedback mechanism must stabilized cycle. Here, we...
Significance We recovered the world’s thickest continuous loess record from southern margin of Taklimakan desert, a global-scale dust source area. The high-resolution grain size and flux records emission, reflecting histories aridity westerlies climate, indicate an extant dry desert area, stable land surface supporting deposition at least since ∼3.6 Ma, that global cooling, rather than Tibet uplift, modulated climate changes in inland Asia Ma. Moreover, our study may suggest potential...