supported by the National Natural Science Foundation of China(42325705 and 42230208);the Chinese Academy of Sciences(xbzg-zdsys-202217)。
Characterization of transport pathways and depositional changes in Mercury(Hg)and their connection to climatic and environmental changes on various time scales are crucial for better understanding the anthropogenic im...
supported by the National Natural Science Foundation of China(Grant No.41991252);the Strategic Priority Research Program(Grant No.XDB40000000);the International Partnership Program(Grant No.132B61KYSB20170005)of Chinese Academy of Sciences;the National Natural Science Foundation of China(Grant No.41888101);partly supported by the USA National Science Foundation(Grant Nos.0908792,1211299&1702816 to R.Lawrence EDWARDS and Hai CHENG);the 111 Program of China(Grant No.D19002);the Belt&Road Center for Climate and Environment Studies of IEECAS。
Evaluating anthropogenic impacts on regional vegetation changes during historical time is not only important for a better understanding of the Anthropocene but also valuable in improving the vegetation-climate models....
supported by the National Key Research and Development Program of China (Grant No. 2017YFA0603401);Shaanxi Science Fund for Distinguished Young Scholars (Grant No. 2018JC-023);Youth Innovation Promotion Association (Grant No. 2012295);West Light Foundation of Chinese Academy of Sciences;a part of The "Belt & Road" Project of the Institute of Earth Environment, Chinese Academy of Sciences
Application of X-ray fluorescence core-scanning(XRF-CS) on both marine and lake sediments has achieved remarkable results. However, its application has not been widely extended to the research on speleothems. In this ...
supported by the US National Science Foundation, project EAR-1600931
Speleothem carbonates are precipitated continuously from inorganic carbon dissolved in seepage water infiltrating from the land surface,that reflects a mixture of atmospheric CO_2,respired soil carbon,and epikarst sou...
supported by the National Natural Science Foundation of China(grants No.41290254 and 41372192);the State Key Laboratory of Loess and Quaternary Geology,and Chinese Academy of Science(International partnership Program,grant No.132B61KYS20160002)
The Westerlies is important in linking the Northem high latitude, North Atlantic and East Asian monsoon. The location and intensity of the Westerly jet can not only control the climate of central Asia (including nort...
supported by the National Natural Science Foundation of China(Grant Nos.41130102&41471162);the Fundamental Research Funds for the Central Universities(Grant Nos.LZUJBKY-2015-K09&LZUJBKY-2015-124);JC is partially supported by the Chinese Scholarship Council
The evolution of the East Asian summer monsoon (EASM) during the Holocene has long been of significant interest. Knowledge of past EASM variability not only increases our understanding of monsoon dynamics on a long ...
supported by the Open Project Program of State Key Laboratory of Geological Processes and Mineral Resources(Grant No.GPMR201201);National Natural Science Foundation of China(Grant No.41371216)
In-situ seasonalδ18O measurements of section 236.3-235.6 cm of speleothem HS4, from Qingjiang Valley of the Middle reaches of Yangtze River, China, were performed by an Secondary Ionization Mass Spectrometry (SIMS)...
funded by National Key Basic Research Development Program (Grant No. 2013CB956700);Orientation Project of Knowledge Innovation Program of Chinese Academy of Sciences (Grant No. kzcx2-yw-306);National Natural Science Foundation of China (Grant Nos. 41003054 and 90202003)
Monitoring and sampling of main plants, soil CO2, soil water, bedrock, spring water, drip water and its corresponding speleothem were performed at four cave systems of Guizhou, Southwest China, from April 2003 to May ...
Speleothems from Nerja Cave in southern Spain provide a record during interglacial period MIS5a. Period of speleothem deposition occurred from 70,000 90,000 yr ago. Oxygen (δ18O) and hydrogen (δD) isotope ratios of ...
A technique used to determine the authenticity of artifacts that compares the oxygen isotopic composition of speleothems to the carbonate included within the patina of unprovenanced artifacts is of questionable value....