Taoyu Xu, Xuefa Shi, Shengfa Liu, S. Qiao, Gang Yang, Guoqing Wang, Kunshan Wang, Xuchen Wang
{"title":"东海内陆架泥区沉积物颜色反射率特征及其近2ka古气候意义","authors":"Taoyu Xu, Xuefa Shi, Shengfa Liu, S. Qiao, Gang Yang, Guoqing Wang, Kunshan Wang, Xuchen Wang","doi":"10.3724/SP.J.1140.2012.06149","DOIUrl":null,"url":null,"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.","PeriodicalId":18188,"journal":{"name":"海洋地质与第四纪地质","volume":"32 1","pages":"149-158"},"PeriodicalIF":0.0000,"publicationDate":"2013-02-17","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"3","resultStr":"{\"title\":\"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\",\"authors\":\"Taoyu Xu, Xuefa Shi, Shengfa Liu, S. Qiao, Gang Yang, Guoqing Wang, Kunshan Wang, Xuchen Wang\",\"doi\":\"10.3724/SP.J.1140.2012.06149\",\"DOIUrl\":null,\"url\":null,\"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.\",\"PeriodicalId\":18188,\"journal\":{\"name\":\"海洋地质与第四纪地质\",\"volume\":\"32 1\",\"pages\":\"149-158\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2013-02-17\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"3\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"海洋地质与第四纪地质\",\"FirstCategoryId\":\"1089\",\"ListUrlMain\":\"https://doi.org/10.3724/SP.J.1140.2012.06149\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"海洋地质与第四纪地质","FirstCategoryId":"1089","ListUrlMain":"https://doi.org/10.3724/SP.J.1140.2012.06149","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
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
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.
期刊介绍:
Marine Geology and Quaternary Geology launched in 1981 is a bimonthly academic journal sponsored by Qingdao Institute of Marine Geology, China Geological Survey, and published by the Science Press, China.The journal aims to publish original, cutting-edge, and explorative scientific results in the field of marine geology and sea-land Quaternary geology. The journal focus on reporting the latest research achievements supported by National Natural Science Foundation Project, National Key Project and International Cooperation Project, with priority to the results in China seas, global ocean and three poles, and the comparative study results between offshore and land, regional and global scientific issues.