Show simple item record

dc.contributor.authorSelvaraj, Kandasamy
dc.contributor.authorWei, Kuo-Yen
dc.contributor.authorLiu, Kon-Kee
dc.contributor.authorKao, Shuh-Ji
dc.contributor.author高树基
dc.date.accessioned2013-04-19T03:35:04Z
dc.date.available2013-04-19T03:35:04Z
dc.date.issued2012-03-22
dc.identifier.citationQUATERNARY SCIENCE REVIEWS,2012,37:48-60zh_CN
dc.identifier.issn0277-3791
dc.identifier.urihttp://dx.doi.org/10.1016/j.quascirev.2012.01.009
dc.identifier.uriWOS:000302444600004
dc.identifier.urihttps://dspace.xmu.edu.cn/handle/2288/15995
dc.description.abstractLittle information exists about centennial-scale climate variability on oceanic islands in the western Pacific where the East Asian monsoon (EAM) strongly influences the climate, mountain ecosystem and the society. In this study, we investigate a 168 cm long sediment core recovered from Emerald Peak Lake in subalpine NE Taiwan for the contents of grain size, total organic carbon (TOC), C/N ratio, and stable isotopes (delta C-13 and delta N-15) to reconstruct the monsoon climate and vegetation density during the late Holocene. Six radiocarbon (C-14) ages obtained on plant remains used for the chronology indicate that the sediment core has been accumulated since similar to 3770 cal BP with a mean sedimentation rate of 44.6 cm/ka. The sub-centennial resolution of our proxy records reveals strong fluctuations of the EAM and vegetation density for the past similar to 3770 cal BP. The greater contents of coarse and medium sediments with overall decreasing trends from 3770 to 2000 cal BP suggest an increasing fine sediment influx from the catchment likely due to an increasing lake water level. Although low TOC content, C/N ratio, and enriched delta C-13 values in bulk and fine sediments during this interval suggest a sparsely vegetated catchment, increasing trends of TOC content and C/N ratio together with decreasing trends of delta C-13 and delta N-15 values indicate a strengthening pattern of summer monsoon. This is in contrast to a decreasing monsoon strength inferred from Dongge Cave delta O-18 record at that time, supporting the idea of anti-phasing of summer EAM and Indian summer monsoon. Since 2000 cal BP, higher content of fine sediments with high TOC content and C/N ratio but relatively depleted delta C-13 and low delta N-15 values suggest a high but stable lake water level and dense C3 plants, consistent with a stronger summer monsoon in a wet climate. Within this general trend, we interpret a prominent change of proxy parameters in sediments from similar to 560 to 150 cal BP, as subtropical evidence for the Little Ice Age in NE Taiwan. By comparing our proxy records with other diverse land and marine records from southern China and adjoining marine realm, we demonstrate that the centennial to millennial-scale fluctuations of the summer EAM over the northeastern Taiwan during the late Holocene have been largely modulated by the tropical Pacific forcing through El Nino along with solar forcing. (C) 2012 Elsevier Ltd. All rights reserved.zh_CN
dc.description.sponsorshipNational Science Council of Taiwan [NSC 97-2629-M-001-025, NSC 99-2116-M-001-011]; National Science Foundation of China [41176059, 41121091]zh_CN
dc.language.isoenzh_CN
dc.publisherPERGAMON-ELSEVIER SCIENCE LTDzh_CN
dc.subjectTotal organic carbonzh_CN
dc.subjectC/N ratiozh_CN
dc.subjectStable isotopeszh_CN
dc.subjectEast Asian monsoonzh_CN
dc.subjectLate Holocenezh_CN
dc.subjectEmerald Peak Lakezh_CN
dc.subjectSubtropical Taiwanzh_CN
dc.titleLate Holocene monsoon climate of northeastern Taiwan inferred from elemental (C, N) and isotopic (delta C-13, delta N-15) data in lake sedimentszh_CN
dc.typeArticlezh_CN


Files in this item

Thumbnail

This item appears in the following Collection(s)

Show simple item record