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Holocene chemical weathering and climatic oscillations in north China: evidence from lacustrine sediments | |
Jin, ZD; Wu, JL; Cao, JJ; Wang, SM; Shen, J; Gao, NH; Zou, CJ | |
2004-09 | |
发表期刊 | BOREAS |
卷号 | 33期号:3页码:260-266 |
文章类型 | Article |
摘要 | Holocene lacustrine sediments from two isolated lakes in north China are investigated. Based on palaeoclimatic significance of independent proxies in lake sediments, Holocene chemical weathering, and hence climate change, has been reconstructed for dated sediment cores from Daihai Lake and Aibi Lake. During early to mid-Holocene, higher weathering intensity occurred in the Daihai catchment under warm and humid climate conditions, and this reached a maximum at similar to5 kyr BP. However, synchronous proxy shifts from the two widely separated, isolated lake sediments indicate that there was a cool climate event during the early to mid-Holocene transition. This is characterized by reduced weathering in each catchment, low delta(13)C and delta(18)O of authigenic carbonate, and by lake level fluctuations. These might correspond to a global cooling signal identified in lakes, oceans, mollusc sequences, and polar ice cores, typically centred between similar to8.0 and 8.5 kyr BP. Dry conditions were experienced in Greenland, the North Atlantic and surrounding regions, and in broad monsoonal regions including Daihai at this time. However, recent extensive evidences as well as our data from the Aibi Lake sediments show that cool but wet conditions occurred in the central Eurasian continent at this time. After similar to2.5 kyr BP, a significant shift of independent sediment proxies indicates the beginning of the Neoglaciation with a higher frequency of fluctuations, including both the Medieval Warm Period (MWP) and the Little Ice Age (LIA). Our continental records provide new evidence of the Holocene climate variability with global significance and highlight the different spatial nature of the response to oscillations associated with different climate patterns. |
学科领域 | Physical Geography ; Geology |
DOI | 10.1080/03009480410001280 |
关键词[WOS] | LAKE-SEDIMENTS ; LAST DEGLACIATION ; WARM PERIOD ; ICE-SHEET ; NEW-YORK ; EUROPE ; AGE ; VARIABILITY ; ISOTOPES ; RATIOS |
收录类别 | SCI ; SCIE |
语种 | 英语 |
WOS研究方向 | Geography, Physical ; Geosciences, Multidisciplinary |
WOS记录号 | WOS:000222997800007 |
出版者 | WILEY |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://ir.ieecas.cn/handle/361006/11987 |
专题 | 黄土与第四纪地质国家重点实验室(1985-2004) |
推荐引用方式 GB/T 7714 | Jin, ZD,Wu, JL,Cao, JJ,et al. Holocene chemical weathering and climatic oscillations in north China: evidence from lacustrine sediments[J]. BOREAS,2004,33(3):260-266. |
APA | Jin, ZD.,Wu, JL.,Cao, JJ.,Wang, SM.,Shen, J.,...&Zou, CJ.(2004).Holocene chemical weathering and climatic oscillations in north China: evidence from lacustrine sediments.BOREAS,33(3),260-266. |
MLA | Jin, ZD,et al."Holocene chemical weathering and climatic oscillations in north China: evidence from lacustrine sediments".BOREAS 33.3(2004):260-266. |
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