Knowledge Management System Of Institute of Earth Environment, CAS
Eolian quartz flux to Lake Biwa, central Japan, over the past 145,000 years | |
Xiao, JL; Inouchi, Y; Kumai, H; Yoshikawa, S; Kondo, Y; Liu, TS; An, ZS | |
1997-07 | |
发表期刊 | QUATERNARY RESEARCH |
卷号 | 48期号:1页码:48-57 |
文章类型 | Article |
摘要 | Eolian quartz flux (EQF, g cm(-2) (10(3) yr)(-1)) to Lake Biwa, central Japan, provides direct information on variations of the East Asian winter monsoon, Lake Biwa sediments spanning the past ca, 145,000 yr are characterized by two main periods when EQF values were significantly greater than 5.50 g cm(-2) (10(3) yr)(-1), and two main intervals during which EQF values were lower, Two periods with EQF values >5.50 g cm(-2) (103 yr)(-1) occurred from ca. 145,000 to 125,000 and 73,000 to 13,000 yr B.P., while times of lower EQF values occurred from ca. 125,000 to 73,000 yr B.P. and around ca. 5500 yr B.P. Between ca. 125,000 and 73,000 yr B,P., three minimum EQF values and two intervening peaks of slightly higher EQF values are recorded. EQF increased markedly from ca. 73,000 to 13,000 yr B.P., whereas between ca. 53,000 and 20,000 yr B.P. the values recorded were relatively lower than those recorded during either the preceding or the subsequent episodes, The data imply that the East Asian winter monsoon strengthened during the periods when EQF values were high, and weakened during the intervals with low EQF values. The EQF record of Lake Biwa can be correlated with the grain-size record of the quartz fraction in Chinese loess and with the SPECMAP marine delta(18)O record, However, the EQF record apparently lags ca, 5000 yr behind the loess and delta(18)O records during stage 6/5 and 2/1 transitions and ca, 10,000 yr during stage 5/4 transition, These apparent lags could be due to problems with the chronology; alternatively, they may imply that the eolian quartz flux depended more on the extent of dust source regions than on wind intensity during these transitions. (C) 1997 University of Washington. |
学科领域 | Physical Geography ; Geology |
DOI | 10.1006/qres.1997.1893 |
关键词[WOS] | ATMOSPHERIC CIRCULATION ; NORTHERN HEMISPHERE ; MARINE-SEDIMENTS ; LOESS PLATEAU ; CENTRAL CHINA ; PACIFIC ; DEPOSITION ; HISTORY ; RECORDS ; CYCLES |
收录类别 | SCI ; SCIE |
语种 | 英语 |
WOS研究方向 | Geography, Physical ; Geosciences, Multidisciplinary |
WOS记录号 | WOS:A1997XQ62300005 |
出版者 | ACADEMIC PRESS INC JNL-COMP SUBSCRIPTIONS |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://ir.ieecas.cn/handle/361006/11922 |
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 | Xiao, JL,Inouchi, Y,Kumai, H,et al. Eolian quartz flux to Lake Biwa, central Japan, over the past 145,000 years[J]. QUATERNARY RESEARCH,1997,48(1):48-57. |
APA | Xiao, JL.,Inouchi, Y.,Kumai, H.,Yoshikawa, S.,Kondo, Y.,...&An, ZS.(1997).Eolian quartz flux to Lake Biwa, central Japan, over the past 145,000 years.QUATERNARY RESEARCH,48(1),48-57. |
MLA | Xiao, JL,et al."Eolian quartz flux to Lake Biwa, central Japan, over the past 145,000 years".QUATERNARY RESEARCH 48.1(1997):48-57. |
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