Temperature evolution from the delta o-18 record of hani peat, northeast china, in the last 14000 years
文献类型：期刊论文
| 作者 | Hong Bing1,2; Liu CongQiang1; Lin QingHua1; Yasuyuki, Shibata3; Leng XueTian4; Wang Yu1; Zhu YongXuan1; Hong YeTang1 |
| 刊名 | Science in china series d-earth sciences
 |
| 出版日期 | 2009-07-01 |
| 卷号 | 52期号:7页码:952-964 |
| 关键词 | Holocene Abrupt climate change Peat Holocene megathermal 8.2 kyr event 4.2 kyr event Medieval warm period Little ice age |
| ISSN号 | 1006-9313 |
| DOI | 10.1007/s11430-009-0086-z |
| 通讯作者 | Liu congqiang(liucongqiang@vip.skleg.cn) |
| 英文摘要 | From the last deglaciation to the holocene, the greenland ice core (gisp2) delta o-18 records as well as the records of ice-rafted debris on the surface of the north atlantic have revealed a succession of sudden cooling events on the centennial to millennial scales. however, the temperature proxy records are rarely studied systematically and directly to ensure that this air temperature cooling pattern simultaneously existed in the east asian region, in addition to the repeated pattern occurring in the greater atlantic region. a peat cellulose delta o-18 temperature proxy record proximately existing for 14000 years was picked up from the hani peat in jilin province, china. it suggests by comparison that the sudden cooling events, such as the older dryas, inter-allerod, younger dryas, and nine ice-rafted debris events of the north atlantic, are almost entirely reiterated in the temperature signals of hani peat cellulose delta o-18. these cooling events show that the repeatedly occurring temperature cooling pattern not only appeared in the north atlantic region in the high latitudes, but also in the northwest pacific region in the middle latitudes. the climate change events marking the start of the holocene epoch, the holocene megathermal, the "8.2 kyr" event, the "4.2 kyr" event, the medieval warm period, and the little ice age are further discussed. the sensitivity response of hani peat cellulose delta o-18 to the land surface temperature and the reason for the age accuracy of peat cellulose c-14 are also discussed based on the characteristics of the peat bog environment. |
| WOS关键词 | ABRUPT CLIMATE-CHANGE ; ASIAN MONSOON ; ATLANTIC CLIMATE ; ISOTOPE COMPOSITION ; TREE-RINGS ; HOLOCENE ; PRECIPITATION ; OCEAN ; CIVILIZATION ; CELLULOSE |
| WOS研究方向 | Geology |
| WOS类目 | Geosciences, Multidisciplinary |
| 语种 | 英语 |
| WOS记录号 | WOS:000267687400006 |
| 出版者 | SCIENCE PRESS |
| URI标识 | http://www.irgrid.ac.cn/handle/1471x/2403087 |
| 专题 | 中国科学院大学 |
| 通讯作者 | Liu CongQiang |
| 作者单位 | 1.Chinese Acad Sci, Inst Geochem, State Key Lab Environm Geochem, Guiyang 550002, Peoples R China 2.Chinese Acad Sci, Grad Univ, Beijing 100049, Peoples R China 3.Natl Inst Environm Studies, Div Environm Chem, Tsukuba, Ibaraki 3050052, Japan 4.NE Normal Univ, Coll Urban & Environm Sci, Changchun 130024, Peoples R China |
| 推荐引用方式 GB/T 7714 | Hong Bing,Liu CongQiang,Lin QingHua,et al. Temperature evolution from the delta o-18 record of hani peat, northeast china, in the last 14000 years[J]. Science in china series d-earth sciences,2009,52(7):952-964. |
| APA | Hong Bing.,Liu CongQiang.,Lin QingHua.,Yasuyuki, Shibata.,Leng XueTian.,...&Hong YeTang.(2009).Temperature evolution from the delta o-18 record of hani peat, northeast china, in the last 14000 years.Science in china series d-earth sciences,52(7),952-964. |
| MLA | Hong Bing,et al."Temperature evolution from the delta o-18 record of hani peat, northeast china, in the last 14000 years".Science in china series d-earth sciences 52.7(2009):952-964. |
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来源：中国科学院大学
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