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Quaternary studies in Korea Ⅱ: Contents and characteristics of paleoclimatology/paleoceanography study in and around Korea

机译:韩国第四纪研究Ⅱ:韩国及周边地区的古气候学/古海洋学研究的内容和特征

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This volume was planned by a "subcommittee on paleoclimate and paleoceanography" after the fall 2012 meeting of the Geological Society of Korea. The subcommittee is one of several belonging to the Geological Society of Korea and is composed mainly of Korean members who work on Quaternary terrestrial and ocean sciences in and around the Korean Peninsula. Similar to Quaternary Studies in Korea Ⅰ (Volume 176-177, 2008), Volume Ⅱ contains the initial findings and reviews of studies spanning the Korean Peninsula and its surrounding seas. The Korean Peninsula, located in the east Eurasian continental margin, is influenced by the East Asian monsoon system. The surrounding seas, such as the Yellow Sea, South Sea, and East Sea, were influenced by currents and gyres during the Quaternary. As a result, the paleo-records obtained from proxies from lake, wetland, and marine environments aid our understanding of the East Asian monsoon system and the variability of paleo-currents (e.g., the Tsushima Warm Current, TWC) in the East Sea. To disseminate and advance fundamental research on the Quaternary, the publication of Quaternary Studies in Korea Ⅱ is planned in a series of volumes, which will illustrate the quality and diversity of Quaternary studies in Korea. A total of 19 papers are illustrated in this volume and each data of papers is originated in and around the Korean Peninsula. The following studies appear in Volume Ⅱ.
机译:该卷是由韩国地质学会2012年秋季会议之后的“古气候和古海洋学小组委员会”计划的。该小组委员会是韩国地质学会的数个委员会之一,主要由从事朝鲜半岛及其周围第四纪陆生和海洋科学工作的韩国成员组成。与《朝鲜第四纪研究》(第176-177卷,2008年)类似,《第二纪》包含了对朝鲜半岛及其周围海域的研究的初步发现和回顾。朝鲜半岛位于欧亚大陆东部边缘,受东亚季风系统的影响。第四纪期间,洋流和旋流影响了周围的海洋,例如黄海,南海和东海。结果,从湖泊,湿地和海洋环境的代理获得的古记录有助于我们了解东亚季风系统和东海古流(例如对马暖流,TWC)的变化性。为了传播和促进第四纪的基础研究,计划在第二卷中出版《第二纪韩国研究》,以阐明韩国第四纪研究的质量和多样性。此卷共展示了19篇论文,每篇论文的数据都起源于朝鲜半岛及其周围地区。以下研究载于第二卷。

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  • 来源
    《Quaternary International》 |2014年第10期|1-3|共3页
  • 作者单位

    Geological Research Division, Korea Institute of Geoscience and Mineral Resources, 124 Gwahang-no, Yuseong-gu, Daejeon 305-350, Republic of Korea;

    Marine Environments and Conservation Research Division, Korea Institute of Ocean Science and Technology, 1270 Sa 2dong, Ansan 426-744, Republic of Korea;

    Department of Geography, Memorial University, St. John's NL A1B 3X9, Canada;

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