贝加尔地区萨彦山东部Jom-Bolok火山谷湖泊古环境研究（英文）

作     者：Alexander SHCHETNIKOV Elena V. BEZRUKOVA 

作者机构：Institute of the Earth’s Crust SB Russian Academy of SciencesIrkutsk 664033Russia Vinogradov Institute of Geochemistry SB Russian Academy of SciencesIrkutsk 664033Russia Irkutsk State UniversityIrkutsk 664033Russia Institute of Archaeology and Ethnography SB Russian Academy of SciencesNovosibirsk 630090Russia 

出 版 物：《Journal of Geographical Sciences》 (地理学报（英文版）)

年 卷 期：2019年第29卷第11期

页      面：1823-1840页

核心收录：

学科分类：0709[理学-地质学] 07[理学] 0704[理学-天文学] 

基　　金：The Ministry of Education and Science of the Russian Federation,the State Assignment No.IX.130.3.1.(0350-2016-0026),No.IX.136.2.(0346-2016-0005) Russian Science Foundation,No.16-17-10079(geomorphology,pollen and isotopic studies) Russian Foundation for Basic Research,No.16-05-00586 The Project,No.074-02-2018-334 

主　　题：lake morphogenesis Holocene volcanism lava-dammed lakes environmental change 

摘      要：This article describes the lake basins of the Jom-Bolok volcanic region in the East Sayan (the largest manifestation of the Holocene eruptions in Central Asia).The geomorphological position,origins,aspects of the structure and development are reviewed considering its sedimentary filling.The limnic morphogenesis here develops under the conditions of contrasting relief,high energy of neotectonic and exogenous processes.We established that Lake Khara-Nur,formed as a result of lava-damming of the Jom-Bolok river valley,emerged in its present form approximately 6500 years ago.A complex record on the environment and climatic changes,acquired from its sediments,made it possible to determine for the first time in this region the long-term trends in the development of the Middle and Late Holocene mountain geosystems and also the distinction of several paleogeographic stages of the formation of the natural environment.An average geochemical record resolution for the bottom sediments of the lake was made uniquely for the East Siberian lake records and is equal to 35 years,while the palynological record approximates 110 years.