supported by the Second Tibetan Plateau Scientific Expedition and Research Program(STEP)(Grant No.2019QZKK0202);the National Natural Science Foundation of China(Grant Nos.42371159,42077415);the Program of Introducing Talents of Discipline to University(Grant No.BP0618001)。
The northern Tibetan Plateau is a climatically sensitive zone influenced by monsoon and westerly winds.In summer,water vapor transport can reach Qinghai Lake and the eastern section of the Qilian Mountains;in winter,w...
The Late Pleistocene littoral ridges of southern South America,especially those of the north of Argentinean Patagonia,contain remains of mollusk shells with bioerosion traces.Eleven sites from marine isotope stages(2 ...
As the world’s population has tripled(3x)since 1950,with another 50%increase expected by 2100,global annual carbon dioxide emissions growth rate has quadrupled(4x)since 1950 and global energy demand has quintupled(5x...
supported by the National Natural Science Foundation of China (Grant No. 41425003);the Strategic Priority Research Program of the Chinese Academy of Sciences (Grant No. XDA19070103);the Basic Research Project of Chinese Academy of Meteorological Sciences-Base Construction of Polar Atmospheric Sciences for Field Observation;the Scientific Research Foundation of the Key Laboratory of Cryospheric Sciences (Grant No. SKLCS-OP-2016-03)
Using high-resolution ice core and tree ring proxies for sea ice extent (SIE), we reconstructed a robust time series of autumn SIE over the Barents-Kara (B-K) sector of the Arctic from AD 1289-1993. After intercom...
We present here a simple and novel proposal for the modulation and rhythm of ice-ages and interglacials during the late Pleistocene. While the standard Milankovitch-precession theory fails to explain the long interval...
supported by the CAS Strategic Priority Research Program(Grant No.XDA05080801);the National Basic Research Program of China(Grant No.2010CB950104);the Chinese Academy of Sciences 100 Talents Project(Grant No.29082762);the National Natural Science Foundation of China(Grant No.40871091);Feng Shi was supported by the West Light Program for Talent Cultivation of Chinese Academy of Sciences and China Meteorological Administration Drought Research Fund(Grant Nos.IAM201213 and IAM201109);Lucien von Gunten was supported by the Swiss NSF(Grant No.PBBEP2-126056)
We present the first millennial-length gridded field reconstruction of annual temperature for China, and analyze the reconstruction for spatiotemporal changes and associated uncertainties, based on a network of 415 we...
The research is jointly supported by the Key Project of the National Natural Science Foundation of China(No.40332020);Prophase Special Research of Vital Projects in the Basic Research of the Ministry of Science and Technology of China(No.2001CCA01 800);International Geological Correlation Program(IGCP463/494).
The Cretaceous is among the most unusual eras in the geological past. Geoscience communities have been having great concerns with geological phenomena within this period, for example carbonate platforms and black shal...
the National Natural Science Foundation of China (Grant Nos. 49632070, 49972038) and by the Excellent Young Teachers Program of the Ministry of Education of China to the first author.
Based on reconstructions of paleogeography, paleoclimate and paleoceanography of the Chihsian, Wujiapingian, Anisian and Norian intervals in the eastern Tethys, the multiple intrinsic relationship and interaction amon...
Spelean stalagmite dating using thermal ionization mass spectrometry (TIMS) on the basis of U Th disequilibrium has contributed greatly to paleoclimatology, paleo environment, paleo oceanology, archaeology as well as ...
The δ18O value is mainly controlled by δ18O value of paleo-ocean water and the water skin temperature. The piston core HY4-901 is located at 14°49′N, 113°28′E, on the northern continental s...