<P style="MARGIN: 0cm 0cm 0pt; mso-pagination: widow-orphan; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-outline-level: 2" class=MsoNormal>ack; FONT-SIZE: 14pt; mso-font-kerning: 18.0pt; mso-bidi-font-weight: bold" lang=EN-US>ace="Times New Roman">The Last Glaciation Maximum in the Sea of Japan/East Sea pace prefix = o ns = "urn:schemas-microsoft-com:office:office" />p>p>

详细信息   

• 责任者：Liu Yanguang (Key Laboratory of Marine Sedimentology and Environmental Geology ; First Institute of Oceanography ; SOA ; Qingdao 266061 ; China) ; Zou Jianjun
• 刊名：Marine Geology & Quaternary Geology
• 出版年：2009
• 卷期：29(4)
• 关键词：末次冰期 ; last glacial age ; 日本海 ; Japan Sea
• 页码：p.53-63
• 图表：5 illus., 54 refs.
• 分类号：1400
• issnNo：ISSN0256-1492
• isbnNo：CN37-1117/P

摘要

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pt; mso-font-kerning: 0pt" lang=EN-US>ace="Times New Roman">Hemipelagic sediments in the Sea of Japan (pace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />place w:st="on">aceName w:st="on">EastaceName> aceType w:st="on">SeaaceType>place>) during the last glaciation maximum (LGM) were characterized by centimeter-to decimeter-scale alternations of organic-poor light-gray layers, organic-rich dark-gray layers and homogenous layers.pacerun: yes">&nbsp; In association with the sedimentary characteristics, the alkenone sea surface temperatures (Uk’37-SSTs) of the central and southern place w:st="on">aceName w:st="on">JapanaceName> aceType w:st="on">SeaaceType>place> were estimated and the results enabled us to understand the paleoceanographic evolutions in the study area during the LGM and its linkage with the East Asian monsoon (EAM). It was generally accepted that the ventilation of deep water was blocked during this period by the density stratification of the water column as a result of excessive EAM precipitation, the surface salinity was low and the bottom was filled with static, anoxic water.pacerun: yes">&nbsp; &nbsp;p>p>