Changes in climate and vegetation of central Guizhou in southwest China since the last glacial reflected by stalagmite records from Yelang Cave

Min Zhao, Hong Chun Li, Zai Hua Liu, Horng-Sheng Mii, Hai Long Sun, Chuan Chou Shen, Su Chen Kang

Research output: Contribution to journalArticle

15 Citations (Scopus)

Abstract

Two stalagmites (6-cm and 18-cm long) from Yelang Cave (26°2'28″N, 105°44'11″E) in central Guizhou of China have been dated by ICP-MS 230Th/U, 210Pb and AMS 14C dating methods. Low U but high Th contents in the young stalagmites were difficult to apply 230Th/U dating. Instead, AMS 14C dating solved the chronological problem of these stalagmites. Both stalagmites had fast growth rates during Holocene Optimum and the last 600years, but absent growth between 4 and 8ka. The δ18O record of Stalagmite 20120824-13 agrees well with the Dongge δ18O records on centennial or longer scales, showing dry climates during the Last Glacial Maximum (LGM) and Younger Dryas and wet climates during Holocene Optimum following the solar insolation trend. The summer monsoon strength decreased from 4.12ka to 1.5ka, but increased during the Medieval Warm Period to produce wet climates and abundant vegetation in the study area. The δ18O record during the last 600years exhibits strongly decadal variations. Twelve light δ18O excursions on decadal scales during the last 600years can be identified, agreeing with the local Dry-Wet index record. The Pacific Decadal Oscillation (PDO) strongly affects decadal variability of the moisture budget in the study area, with cold PDO (La Niña condition) in favor of stronger EASM and wet climates. The δ13C record indicates that natural vegetation in the study area was strongly destroyed by human activity after the reign of Emperor Yong Zheng (AD 1722-1735) of Qing Dynasty. Since then, the karst-desertification in central Guizhou has been strongly developed due to rapidly increased population and land-use.

Original languageEnglish
Pages (from-to)549-561
Number of pages13
JournalJournal of Asian Earth Sciences
Volume114
DOIs
Publication statusPublished - 2015 Dec 15

Fingerprint

stalagmite
Last Glacial
cave
vegetation
climate
Pacific Decadal Oscillation
accelerator mass spectrometry
Holocene
Medieval Warm Period
decadal variation
dating method
Younger Dryas
desertification
insolation
Last Glacial Maximum
karst
monsoon
human activity
moisture
land use

Keywords

  • AMS C dating
  • Central Guizhou
  • East Asian monsoon
  • Holocene
  • Late pleistocene
  • Pacific Decadal Oscillation
  • Stalagmite
  • δO and δC record

ASJC Scopus subject areas

  • Earth-Surface Processes
  • Geology

Cite this

Changes in climate and vegetation of central Guizhou in southwest China since the last glacial reflected by stalagmite records from Yelang Cave. / Zhao, Min; Li, Hong Chun; Liu, Zai Hua; Mii, Horng-Sheng; Sun, Hai Long; Shen, Chuan Chou; Kang, Su Chen.

In: Journal of Asian Earth Sciences, Vol. 114, 15.12.2015, p. 549-561.

Research output: Contribution to journalArticle

Zhao, Min ; Li, Hong Chun ; Liu, Zai Hua ; Mii, Horng-Sheng ; Sun, Hai Long ; Shen, Chuan Chou ; Kang, Su Chen. / Changes in climate and vegetation of central Guizhou in southwest China since the last glacial reflected by stalagmite records from Yelang Cave. In: Journal of Asian Earth Sciences. 2015 ; Vol. 114. pp. 549-561.
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