The DOI matches its Crossref record; 45 of the 45 references it cites were found in a registry or an index.
A high-resolution stalagmite record of the Holocene East Asian monsoon from Mt Shennongjia, central China
Abstract
High-resolution oxygen isotope (δ 18 O) profiles of six stalagmites from Sanbao Cave in Hubei province, central China, established with 1413 oxygen isotope data and 65 230 Th ages, provide a continuous history of East Asian Summer Monsoon (EASM) intensity for the period from 13—0.2 thousand years before present (ky BP, relative to AD 1950). The δ 18 O record includes four distinct stages in the evolution of the EASM: (1) an abrupt transition (~11.5 ky BP) into the Holocene; (2) a period of gradual increase in monsoon intensity (11.5—9.5 ky BP); (3) the maximum humid period (9.5—6.5 ky BP); and (4) a period of gradual decline in monsoon intensity (6.5—0.2 ky BP). Comparison of Sanbao with regional records of comparable resolution reveals that the timing of the beginning and end of the Holocene Optimum (as defined by the minimum in δ 18 O) was similar in the Indian and East Asian monsoon systems. This supports the idea that shifts in the monsoon tied to shifts in the mean position of the Inter-Tropical Convergence Zone (ITCZ) may control monsoon intensity throughout the entire low-latitude region of Asia on orbital timescales. This observation also supports the idea that the fluctuations in δ 18 O recorded across southern Asia reflect broad changes in the monsoon, as opposed to local meteoric precipitation. The EASM records from Sanbao largely follow orbital-scale insolation changes, yet exhibit similar variability to Greenland ice core δ 18 O on millennial to centennial scales during the early to middle Holocene ( r = 0.94).
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Cites
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Self-citationMillennial- and orbital-scale changes in the East Asian monsoon over the past 224,000 years
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Self-citationHolocene Forcing of the Indian Monsoon Recorded in a Stalagmite from Southern Oman
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Cited by
Global biomass burning: a synthesis and review of Holocene paleofire records and their controls
Marlon, J. R., Bartlein, P. J., Daniau, A.-L., Harrison, S. P., Maezumi, S. Y., Power, M. J., Tinner, W., & Vanniére, B. (2013) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2012.11.029 · Cited by 438
Quantifying kinetic fractionation in Bunker Cave speleothems using Δ47
Kluge, T., & Affek, H. P. (2012) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2012.06.013 · Cited by 86
Metadata
- Authors
- Dong, J., Wang, Y., Cheng, H., Hardt, B., Edwards, R. L., Kong, X., Wu, J., Chen, S., Liu, D., Jiang, X., & Zhao, K.
- Venue
- The Holocene
- Publisher
- SAGE Publications
- Published
- 2010-02-25
- Volume
- 20
- Issue
- 2
- Pages
- 257-264
- ISSN
- 0959-6836 (ISSN-L)
- 1477-0911
- OpenAlex
- W2089177966
- Cited by
- 313
- References
- 45
- FWCI
- 8.48
- Type
- journal article
- Language
- en
- Open access
- closed
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- Dong, J., Wang, Y., Cheng, H., Hardt, B., Edwards, R. L., Kong, X., Wu, J., Chen, S., Liu, D., Jiang, X., & Zhao, K. (2010). A high-resolution stalagmite record of the Holocene East Asian monsoon from Mt Shennongjia, central China. The Holocene. https://doi.org/10.1177/0959683609350393
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