Xiaomin Fang

Biographic Data

ID	4021594
NAME	Xiaomin Fang
GIVEN NAMES	Xiaomin
FAMILY NAME	Fang
SIGNATURE	FANG X
AFFILIATIONS	Chinese Academy of Sciences
ORCID	0000-0003-2808-8836
VERIFIED	Yes
TOTAL WORKS	24
TOTAL CITATIONS	14
WORKS AS AUTHOR	24
WORKS AS EDITOR	0
FIRST PUBLICATION YEAR	2003
LATEST PUBLICATION YEAR	2024
H-INDEX	1

Aqueous M. oleifera leaf extract alleviates DSS-induced colitis in mice through suppression of inflammation
Open AccessShuai Zhang, Yanan Cao et al.ARTICLEJournal of Ethnopharmacology2024
Systematic boron isotope analysis on a Quaternary deep SG-1 core from the Qaidam Basin, NE Tibetan Plateau and its paleoclimate implication
Open AccessShengcheng Lu, Yunqi Ma et al.ARTICLEQuaternary International2022
Chronological and rock magnetic constraints on the transition of the Quaternary paleoclimate in the western Qaidam Basin, NE Tibetan Plateau
Open AccessWeilin Zhang, Tao Li et al.ARTICLEQuaternary Research2021
A closed Quaternary saline paleolake, currently still a lake and named Dalangtan after one of its largest sub-basins, has widely distributed sediments in the western Qaidam Basin, NE Tibetan Plateau. Lacustrine salt minerals and fine sediments from this paleolake provide an environmental record for investigating paleoclimatic evolution in the Asian interior. However, detailed continuous Pliocene–Quaternary paleoclimatic records are broadly lackin…
Characteristic grain-size component - A useful process-related parameter for grain-size analysis of lacustrine clastics
Open AccessYin Lu, Xiaomin Fang et al.ARTICLEQuaternary International2018
Variation of gypsum morphology along deep core SG-1, western Qaidam Basin (northeastern Tibetan Plateau) and its implication to depositional environments
Open AccessJiao Li, Minghui Li et al.ARTICLEQuaternary International2017
Altitudinal variations in the bulk organic carbon isotopic composition of topsoil in the Qilian Mountains area, NE Tibetan Plateau, and its environmental significance
Open AccessYan Zhao, Fuli Wu et al.ARTICLEQuaternary International2017
Late Plio-Pleistocene humidity fluctuations in the western Qaidam Basin (NE Tibetan Plateau) revealed by an integrated magnetic–palynological record from lacustrine sediments
Open AccessChristian Herb, Andreas Koutsodendris et al.ARTICLEQuaternary Research2015
Deciphering the climatic evolution of the Tibetan Plateau region during the Plio-Pleistocene is hampered by the lack of continuous archives and proxy datasets indicative of moisture availability. Here we assess the suitability of magnetic susceptibility (χ) measured on lacustrine sediments as a paleohydrological proxy based on material from drill core SG-1 (2.69–0.08 Ma) from the western Qaidam Basin. Our assessment is based on directly comparing…
Late Miocene–Quaternary rapid stepwise uplift of the NE Tibetan Plateau and its effects on climatic and environmental changes
Open AccessJijun Li, Xiaomin Fang et al.ARTICLEQuaternary Research2014
The way in which the NE Tibetan Plateau uplifted and its impact on climatic change are crucial to understanding the evolution of the Tibetan Plateau and the development of the present geomorphology and climate of Central and East Asia. This paper is not a comprehensive review of current thinking but instead synthesises our past decades of work together with a number of new findings. The dating of Late Cenozoic basin sediments and the tectonic geo…
Magnetic parameter variations in the Chaona loess/paleosol sequences in the central Chinese Loess Plateau, and their significance for the middle Pleistocene climate transition
Open AccessYougui Song, Xiaomin Fang et al.ARTICLEQuaternary Research2014
A high-resolution rock magnetic investigation was performed on the Chaona Quaternary loess/paleosol sequences in the Central Chinese Loess Plateau. Based on a newly developed independent unturned time scale and magnetic records, we reconstructed the history of the East Asia monsoons during the last 3 Ma and explored the middle Pleistocene climate transition (MPT). Rock magnetic results show that the loess layers are characterized by relatively hi…
Late Pliocene–Quaternary evolution of redox conditions in the western Qaidam paleolake (NE Tibetan Plateau) deduced from Mn geochemistry in the drilling core SG-1
Open AccessYibo Yang, Xiaomin Fang et al.ARTICLEQuaternary Research2013
Manganese (Mn) in lake sediments reacts strongly to changes of redox conditions. This study analyzed Mn concentrations in oxides, carbonates, and bulk phases of the calcareous lacustrine sediments of a 938.5-m-long core (SG-1) taken from the western Qaidam Basin, well dated from 2.77 Ma to 0.1 Ma. Comparisons of extractions from diluted hydrochloric acid, acetic acid and citrate"bicarbonate"dithionite demonstrate that variations of Mn concentrati…
Six million years of magnetic grain-size records reveal that temperature and precipitation were decoupled on the Chinese Loess Plateau during ~ 4.5–2.6 Ma
Open AccessJunsheng Nie, Yougui Song et al.ARTICLEQuaternary Research2013
Magnetic grain-size variations have been used as sensitive paleoclimate proxies to investigate the evolution of the East Asian summer monsoon, but their relationship with temperature and precipitation is not entirely clear. Here we find that two magnetic grain-size proxy records (χ ARM /χ LF and χ ARM /SIRM, where χ ARM , χ LF and SIRM are anhysteretic remanent magnetization susceptibility, magnetic susceptibility measured at 470 Hz and saturatio…
Evaporite minerals of the lower 538.5 m sediments in a long core from the Western Qaidam Basin, Tibet
Open AccessMinghui Li, Xiaomin Fang et al.ARTICLEQuaternary International2013
Over-representation of Picea pollen induced by water transport in arid regions
Open AccessFuli Wu, Xiaomin Fang et al.ARTICLEQuaternary International2013
Quaternary paleolake nutrient evolution and climatic change in the western Qaidam Basin deduced from phosphorus geochemistry record of deep drilling core SG-1
Yibo Yang, Xiaomin Fang et al.ARTICLEQuaternary International2013
Evolution of the arid climate in High Asia since ∼1 Ma
Jinbo Zan, Xiaomin Fang et al.ARTICLEQuaternary International2013
Environmental implications of the magnetic record in Pleistocene lacustrine sediments of the Qaidam Basin, NE Tibetan Plateau
Christian Herb, Weilin Zhang et al.ARTICLEQuaternary International2013
Magnetostratigraphy of deep drilling core SG-1 in the western Qaidam Basin (NE Tibetan Plateau) and its tectonic implications
Open AccessWeilin Zhang, Erwin Appel et al.ARTICLEQuaternary Research2012
The Qaidam Basin is the largest intermontane basin of the northeastern Tibetan Plateau and contains a continuous Cenozoic sequence of lacustrine sediments. A ~ 1000-m-deep drilling (SG-1) with an average core recovery of ~ 95% was carried out in the depocenter of the Chahansilatu playa (sub-depression) in the western Qaidam Basin, aimed to obtain a high-resolution record of the paleoenvironmental evolution and the erosion history. Stepwise altern…
Tibet forcing of mid-Pleistocene synchronous enhancement of East Asian winter and summer monsoons revealed by Chinese loess record
Open AccessWenxia Han, Xiaomin Fang et al.ARTICLEQuaternary Research2012
The mid-Pleistocene transition (MPT) of the global climate system, marked by a shift of previously dominant 41-ka cycles to lately dominant 100-ka cycles roughly in the mid-Pleistocene, is one of the fundamental enigma in the Quaternary climate evolution. The process and origin of the MPT remain of persistent interest and conjecture. Here we present high-resolution astronomically tuned magnetic susceptibility (MS) and grain‐size records from a co…
Magnetostratigraphy of sediments from the Yumu Shan, Hexi Corridor and its implications regarding the Late Cenozoic uplift of the NE Tibetan Plateau
Open AccessDongliang Liu, Maodu Yan et al.ARTICLEQuaternary International2011
Climate evolution and environmental response on the Tibetan Plateau
Open AccessAntje Schwalb, Brigitta Schütt et al.ARTICLEQuaternary International2010
Evaporite minerals and geochemistry of the upper 400m sediments in a core from the Western Qaidam Basin, Tibet
Open AccessMinghui Li, Xiaomin Fang et al.ARTICLEQuaternary International2010
Differences between East Asian and Indian monsoon climate records during MIS3 attributed to differences in their driving mechanisms
Open AccessWenxia Han, Xiaomin Fang et al.ARTICLEQuaternary International2010
Pedogenic response to millennial summer monsoon enhancements on the Tibetan Plateau
Open AccessXiaomin Fang, Lianqing Lü et al.ARTICLEQuaternary International2003
Winter half-year temperature reconstruction for the middle and lower reaches of the Yellow River and Yangtze River, China, during the past 2000 years
Quansheng Ge, Jie Zheng et al.ARTICLEThe Holocene2003Cited by: 14
Phenological cold/warm events recorded in Chinese historical documents are used to reconstruct, at 10–30 years' resolution, winter half-year (October to April) temperatures for the past 2000 years in the central region of eastern China. Because of the uneven spatial and temporal distribution of the phenological records, the reconstruction of the regional mean temperature involves two steps: reconstruction for individual sites within the region an…