THE COLOR REFLECTANCE FEATURES OF THE SEDIMENTS IN MUD AREA ON THE INNER SHELF OF THE EAST CHINA SEA AND ITS PALEOCLIMATIC IMPLICATIONS FOR RECENT 2 ka

XU Taoyu; SHI Xuefa; LIU Shengfa; QIAO Shuqing; YANG Gang; WANG Guoqing; WANG Kunshan; WANG Xuchen

doi:10.3724/SP.J.1140.2012.06149

2012 Vol. 32, No. 6

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XU Taoyu, SHI Xuefa, LIU Shengfa, QIAO Shuqing, YANG Gang, WANG Guoqing, WANG Kunshan, WANG Xuchen. THE COLOR REFLECTANCE FEATURES OF THE SEDIMENTS IN MUD AREA ON THE INNER SHELF OF THE EAST CHINA SEA AND ITS PALEOCLIMATIC IMPLICATIONS FOR RECENT 2 ka[J]. Marine Geology & Quaternary Geology, 2012, 32(6): 149-158. doi: 10.3724/SP.J.1140.2012.06149

Citation:

XU Taoyu, SHI Xuefa, LIU Shengfa, QIAO Shuqing, YANG Gang, WANG Guoqing, WANG Kunshan, WANG Xuchen. THE COLOR REFLECTANCE FEATURES OF THE SEDIMENTS IN MUD AREA ON THE INNER SHELF OF THE EAST CHINA SEA AND ITS PALEOCLIMATIC IMPLICATIONS FOR RECENT 2 ka[J]. Marine Geology & Quaternary Geology, 2012, 32(6): 149-158. doi: 10.3724/SP.J.1140.2012.06149

THE COLOR REFLECTANCE FEATURES OF THE SEDIMENTS IN MUD AREA ON THE INNER SHELF OF THE EAST CHINA SEA AND ITS PALEOCLIMATIC IMPLICATIONS FOR RECENT 2 ka

1 Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China;
2 First Institute of Oceanography, State Oceanic Administration, Key Laboratory of State Oceanic Administration for Marine Sedimentology and Environmental Geology, Qingdao 266061, China;
3 China University of Geosciences(Wuhan), Wuhan 430074, China;
4 University of Massachusetts, Boston 02125, American

Received Date: 12 August 2012

Revised Date: 06 October 2012

Abstract

Abstract

A climatic proxy system is constructed on the basis of the color reflectance data of the core MZ01 using first derivative and factors analysis method, and a high-resolution climatic sequence is established with the support of AMS14C dating data for the past 2 ka.900AD is the key turning-point in the course of climate evolution.Climate became significantly cold with high-frequency but low amplitude temperature fluctuation right after 900AD.In the past 2 ka,the climate in East China has experienced four stages including a cold stage before 580AD,a warm stage between 580 and 900AD,a temperature fluctuation stage between 900 and 1460AD and a cold stage between 1460 and 1880AD.Each stage includes some secondary regional or global temperature fluctuations.
- mud area /
- color reflectance /
- East Asia monsoon /
- climate /
- inner shelf of the East China Sea

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References

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