High resolution stalagmite δ18O records over the past 1000 years from Dongge Cave in Guizhou
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- Type
- article
- Published
- 2005-04-29
- Cited by
- 25
- References
- 31
- OpenAlex
- https://openalex.org/W102840713
- Semantic Scholar
- https://api.semanticscholar.org/CorpusID:128268184
Keywords
Stalagmite, Cave, Geology, δ18O, Physical geography
References
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- Feeding methane vents and gas hydrate deposits at south Hydrate Ridge
- Correlation between high-resolution climate records from a Nanjing stalagmite and GRIP ice core during the last glaciation
- A Role for the Tropical Pacific
- INTCAL98 Radiocarbon Age Calibration, 24,000–0 cal BP
- Cyclic rapid warming on centennial‐scale revealed by a 2650‐year stalagmite record of warm season temperature
- Persistent Solar Influence on North Atlantic Climate During the Holocene
- The δ18O variation of a stalagmite from Qixing Cave, Guizhou Province and indicated climate change during the Holocene
- Uranium and thorium isotopic and concentration measurements by magnetic sector inductively coupled plasma mass spectrometry
- Correlation between climate events in the North Atlantic and China during the last glaciation
- Response of climate to solar forcing recorded in a 6000-yearδ18O time-series of Chinese peat cellulose
- Coupled Land-Ocean-Atmosphere Processes and South Asian Monsoon Variability
- A high-resolution millennial record of the south asian monsoon from himalayan ice cores
- Evidence for solar forcing on the Indian monsoon during the last millennium
- Palaeoclimatic interpretation of high-resolution oxygen isotope profiles derived from annually lamin
- Spatial and temporal variability in the stable isotope systematics of modern precipitation in China: implications for paleoclimate reconstructions
- Correlation between Indian Ocean summer monsoon and North Atlantic climate during the Holocene
- Abrupt changes in the Asian southwest monsoon during the Holocene and their links to the North Atlantic Ocean
- A High-Resolution Absolute-Dated Late Pleistocene Monsoon Record from Hulu Cave, China
- Ocean circulation and climate during the past 120,000 years
Cited by
- Asian monsoon precipitation changes and the Holocene methane anomaly
- Transmission of oxygen isotope signals of precipitation-soil water-drip water and its implications in Liangfeng Cave of Guizhou, China
- Evaluation of the ability of the Chinese stalagmite δ 18 O to record the variation in atmospheric circulation during the second half of the 20th century
- Modern stalagmite oxygen isotopic composition and its implications of climatic change from a high-elevation cave in the eastern Qinghai-Tibet Plateau over the past 50 years
- Humid medieval warm period recorded by magnetic characteristics of sediments from Gonghai Lake, Shanxi, North China
- Summer monsoon precipitation variations in central China over the past 750 years derived from a high-resolution absolute-dated stalagmite
- Changes in extreme wet events in Southwestern China in 1960–2011
- Extreme drought changes in Southwest China from 1960 to 2009
- Centennial- to decadal-scale monsoon precipitation variability in the semi-humid region, northern China during the last 1860 years: Records from stalagmites in Huangye Cave
- High-precision 238U–234U–230Th disequilibrium dating of the recent past: a review
- Asian summer monsoon precipitation recorded by stalagmite oxygen isotopic composition in the western Loess Plateau during AD1875–2003 and its linkage with ocean-atmosphere system
- Temporal and spatial variations in hydro-geochemistry of cave percolation water and their implications for four caves in Guizhou, China
- Stable Carbon Isotope Variations in Cave Percolation Waters and their Implications in Four Caves of Guizhou, China
- Contextualizing human migration in different agro-ecological zones in ancient China
- Circulation background of climate patterns in the past millennium: Uncertainty analysis and re-reconstruction of ENSO-like state
- Natural and anthropogenic impacts on the Asian monsoon precipitation during the 20th century
- Recent advances on reconstruction of climate and extreme events in China for the past 2000 years
- Rapid retreat of the East Asian summer monsoon in the middle Holocene and a millennial weak monsoon interval at 9 ka in northern China
- Tree-ring δ18O inferred spring drought variability over the past 200 years in the Hengduan Mountains, Southwest China
- The Asian Summer Monsoon: Teleconnections and Forcing Mechanisms—A Review from Chinese Speleothem δ18O Records
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