Reply to Weiss: Tree-ring stable oxygen isotopes suggest an increase in Asian monsoon rainfall at 4.2 ka BP

. 2022 May 17 ; 119 (20) : e2204067119. [epub] 20220513

Jazyk angličtina Země Spojené státy americké Médium print-electronic

Typ dokumentu časopisecké články, práce podpořená grantem

Perzistentní odkaz   https://www.medvik.cz/link/pmid35561221

Bolin Centre for Climate Research Stockholm University 106 91 Stockholm Sweden

Centre for Ecological and Evolutionary Synthesis Department of Biosciences University of Oslo N 0316 Oslo Norway

Chinese Academy of Sciences Center for Excellence in Tibetan Plateau Earth Sciences Chinese Academy of Sciences Beijing 100101 China

Climatic Research Unit School of Environmental Sciences University of East Anglia Norwich NR4 7TJ United Kingdom

College of Earth and Environmental Sciences Lanzhou University Lanzhou 730000 China

Czech Globe Global Change Research Institute Czech Academy of Sciences 60300 Brno Czech Republic

Dendrosciences Group Swiss Federal Research Institute for Forest Snow and Landscape Research CH 8903 Birmensdorf Switzerland

Département des Sciences Fondamentales Université du Québec à Chicoutimi Chicoutimi QC G7H 2B1 Canada

Department of Geography Faculty of Science Masaryk University 61137 Brno Czech Republic

Department of Geography Johannes Gutenberg University 55099 Mainz Germany

Department of Geography Justus Liebig University D 35390 Giessen Germany

Department of Geography University of Cambridge CB2 3EN Cambridge United Kingdom

Department of History Stockholm University 106 91 Stockholm Sweden

Institute of Geography Friedrich Alexander University Erlangen Nürnberg 91058 Erlangen Germany

Key Laboratory of Desert and Desertification Northwest Institute of Eco Environment and Resources Chinese Academy of Sciences Lanzhou 730000 China

Key Laboratory of Virtual Geographic Environment of Ministry of Education School of Geography Science Nanjing Normal University Nanjing 210023 China

Laboratory of Tree Ring Research University of Arizona Tucson AZ 85721

Science and Innovation Department World Meteorological Organization CH 1211 Geneva Switzerland

State Key Laboratory of Lake Science and Environment Nanjing Institute of Geography and Limnology Chinese Academy of Sciences Nanjing 210008 China

Swedish Collegium for Advanced Study 752 38 Uppsala Sweden

Tree Ring Laboratory Lamont Doherty Earth Observatory of Columbia University Palisades NY 10964

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doi: 10.1073/pnas.2200796119 PubMed

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Yang B., et al. , Long-term decrease in Asian monsoon rainfall and abrupt climate change events over the past 6,700 years. Proc. Natl. Acad. Sci. U.S.A. 118, 10.1073/pnas.2102007118 (2021). PubMed DOI PMC

Walker M., et al. , Subdividing the Holocene Series/Epoch: Formalization of stages/ages and subseries/subepochs, and designation of GSSPs and auxiliary stratotypes. J. Quat. Sci. 34, 173–186 (2019).

Carolin S. A., et al. , Precise timing of abrupt increase in dust activity in the Middle East coincident with 4.2 ka social change. Proc. Natl. Acad. Sci. U.S.A. 116, 67–72 (2019). PubMed PMC

Cheng H., et al. , The climatic cyclicity in semiarid-arid central Asia over the past 500,000 years. Geophys. Res. Lett. 39, L01705 (2012).

Yang B., et al. , SI Appendix for Reply to Weiss. Zenodo. 10.5281/zenodo.6473441. DOI

Kathayat G., et al. , Evaluating the timing and structure of the 4.2 ka event in the Indian summer monsoon domain from an annually resolved speleothem record from Northeast India. Clim. Past 14, 1869–1879 (2018).

Kathayat G., et al. , The Indian monsoon variability and civilization changes in the Indian subcontinent. Sci. Adv. 3, e1701296 (2017). PubMed PMC

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