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Xianfeng Wang

Researcher at Nanyang Technological University

Publications -  110
Citations -  11945

Xianfeng Wang is an academic researcher from Nanyang Technological University. The author has contributed to research in topics: Stalagmite & Monsoon. The author has an hindex of 39, co-authored 98 publications receiving 9796 citations. Previous affiliations of Xianfeng Wang include Lamont–Doherty Earth Observatory & Chinese Academy of Sciences.

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Spectral analysis of a 1000-year stalagmite lamina-thickness record from Shihua Cavern, Beijing, China, and its climatic significance

TL;DR: In this paper, moving spectral analysis is used to analyse a stalagmite lamina thickness record to study climate change, which provides a high-resolution geological record of climate change.
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Strong coupling of Asian Monsoon and Antarctic climates on sub-orbital timescales

TL;DR: It is found that the weakest monsoon closely associated with the warmest Antarctic event always occurred during the Terminations, which suggests that millennial-scale events play a key role in driving the deglaciation through positive feedbacks associated with enhanced upwelling and increasing CO2.
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Oxygen isotope precipitation anomaly in the North Atlantic region during the 8.2 ka event

TL;DR: In this paper, an annual laminated stalagmite from northern Spain recorded two outstanding oxygen isotope (δ18O) pulses during the 8.2 ka event, most probably generated by the drainage of proglacial lakes Agassiz and Ojibway.
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Cyclic sedimentation in Brazilian caves: Mechanisms and palaeoenvironmental significance

TL;DR: The palaeoenvironmental meaning and chronology of these three processes were studied in both semi-arid Campo Formoso and subhumid Lagoa Santa areas through 230 Th dating and stratigraphical analyses.
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The Blake geomagnetic excursion recorded in a radiometrically dated speleothem

TL;DR: For the first time, the Blake geomagnetic excursion was recorded in a stalagmite which was dated using the uranium-series dis equilibrium techniques as mentioned in this paper, and the age of the event was estimated to be between 116.5 ± 0.7 kyr and 112.0 ± 1.9 kyr.