Your browser doesn't support javascript.
loading
500-year climate cycles stacking of recent centennial warming documented in an East Asian pollen record.
Xu, Deke; Lu, Houyuan; Chu, Guoqiang; Wu, Naiqin; Shen, Caiming; Wang, Can; Mao, Limi.
Affiliation
  • Xu D; Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China.
  • Lu H; Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China.
  • Chu G; Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China.
  • Wu N; Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China.
  • Shen C; Key Laboratory of Plateau Lake Ecology and Global Change, Yunnan Normal University, Kunming, Yunnan 650092, China.
  • Wang C; 1] Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China [2] University of Chinese Academy of Sciences, Beijing 100049, China.
  • Mao L; State Key Laboratory of Paleobiology and Stratigraphy, Nanjing Institute of Geology and Paleontology, Chinese Academy of Sciences, Nanjing 210008, China.
Sci Rep ; 4: 3611, 2014 Jan 09.
Article in En | MEDLINE | ID: mdl-24402348
ABSTRACT
Here we presented a high-resolution 5350-year pollen record from a maar annually laminated lake in East Asia (EA). Pollen record reflected the dynamics of vertical vegetation zones and temperature change. Spectral analysis on pollen percentages/concentrations of Pinus and Quercus, and a temperature proxy, revealed ~500-year quasi-periodic cold-warm fluctuations during the past 5350 years. This ~500-year cyclic climate change occurred in EA during the mid-late Holocene and even the last 150 years dominated by anthropogenic forcing. It was almost in phase with a ~500-year periodic change in solar activity and Greenland temperature change, suggesting that ~500-year small variations in solar output played a prominent role in the mid-late Holocene climate dynamics in EA, linked to high latitude climate system. Its last warm phase might terminate in the next several decades to enter another ~250-year cool phase, and thus this future centennial cyclic temperature minimum could partially slow down man-made global warming.
Subject(s)

Full text: 1 Collection: 01-internacional Database: MEDLINE Main subject: Pollen / Climate Change / Documentation Country/Region as subject: Asia Language: En Journal: Sci Rep Year: 2014 Document type: Article Affiliation country:

Full text: 1 Collection: 01-internacional Database: MEDLINE Main subject: Pollen / Climate Change / Documentation Country/Region as subject: Asia Language: En Journal: Sci Rep Year: 2014 Document type: Article Affiliation country: