首页> 外文期刊>Russian journal of Pacific geology >Record of Late Glacial-Holocene Paleogeographical Events in Ogranogenic Deposits of Matua Island (Central Kurils)
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Record of Late Glacial-Holocene Paleogeographical Events in Ogranogenic Deposits of Matua Island (Central Kurils)

机译:Matua Island(中央kurils)矿床晚期冰川 - 全新世古地图事件的记录

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摘要

The manifestation of paleoclimatic events since the latest Pleistocene recorded in paleosoils from the soil-pyroclastic covers of Matua Island in the Central Kurils is analyzed for the first time. Throughout this period, the landscape development occurred in conditions of volcanic activity. The studied sections are located under different types of vegetation. Spore and pollen analysis of buried and modern soils is performed. Age binding of the events is carried out on the basis of radiocarbon dating and tephrastratigraphy. Stages of landscape development, including pre- and post-caldera-forming eruptions of the Matua volcano and eruptive activity in the post-caldera period before and after the formation of the Sarychev Peak volcano are established. The interaction of volcanic and climatic factors in the development of the biotic components is determined.
机译:古叶病事件的表现为首次分析了中央Kurils的Matua岛的土壤 - 壁球菌覆盖物中的最新优质蛋白质。 在此期间,景观发展发生在火山活动的条件下。 研究的部分位于不同类型的植物下。 埋藏和现代土壤的孢子和花粉分析。 事件的年龄绑定是在Radiocarbon约会和TepharraThigraphy的基础上进行的。 景观发展的阶段,包括建立了Sarychev Peak Volcano之前和之后的Matua火山的爆发和火山火山爆发的预先和破产活动。 确定了火山和气候因子在生物组分发展中的相互作用。

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