The stable oxygen isotope ratio (δ18O) in precipitation is an integrated tracer of atmospheric
processes worldwide. Since the 1990s, an intensive effort has been dedicated to studying …

Oxygen isotope analyses of skeletal remains (18 O/16 O, δ 18 O) are a powerful tool for
exploring major themes in bioarchaeology (the study of biological archaeological remains) …

薛莲花, 赵侃, 崔英方, 梁怡佳, 杨少华, 汪永进. 近2000 年来东亚夏季风突变的落水洞高分辨率
石笋记录[J]. 第四纪研究, 2020, 40 (4): 973-984. doi: 10.11928/j. issn. 1001-7410.2020 …

The measurement and simulation of water vapor isotopic composition has matured rapidly
over the last decade, with long‐term data sets and comprehensive modeling capabilities …

The strong present-day Asian monsoons are thought to have originated between 25 and 22
million years (Myr) ago, driven by Tibetan–Himalayan uplift. However, the existence of older …

谭明. 环流效应: 中国季风区石笋氧同位素短尺度变化的气候意义——古气候记录与现代气候
研究的一次对话[J]. 第四纪研究, 2009, 29 (5): 851-862.引用本文: 谭明. 环流效应 …

Inter-annual variation in the ratio of 18 O to 16 O of precipitation (δ 18 O p) in the monsoon
regions of China (MRC, area approximately east of 100° E) has not yet been fully analyzed …

Variations in speleothem oxygen-isotope values (δ18O) result from a complicated interplay
of environmental controls and processes in the ocean, atmosphere, soil zone, epikarst, and …

Indian Summer Monsoon (ISM) precipitation during the twentieth century is characterized by
a biennial oscillation, such that ISM precipitation varied between singularly strong and weak …

• The sustained rate of increase over the past century in the combined radiative forcing from
the three well-mixed greenhouse gases carbon dioxide (CO2), methane (CH4), and nitrous …