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首页> 外文期刊>Quaternary International >Climatic and human impacts on landscape development of the Murav'ev Amursky Peninsula (Russian South Far East) in the Middle/Late Holocene and historical time
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Climatic and human impacts on landscape development of the Murav'ev Amursky Peninsula (Russian South Far East) in the Middle/Late Holocene and historical time

机译:对Murav'ev Amssky半岛(俄罗斯南远东)在中/晚全新女和历史时期的气候和人类影响

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摘要

The Murav'ev-Amursky Peninsula is one of the most densely populated and industrially developed regions in the Russian Far East and is included in Bolshoy (Greater) Vladivostok. Before its intensive development began approximately 150 years ago, the mountainous portion of the peninsula was covered by coniferous forests, with mixed broadleaved forests confined to the coastal lowlands. Vegetation was notably transformed during industrial development. The landscape evolution and development of native communities under Middle/Late Holocene short-time climate changes are of particular interest. The results allow the relative importance of natural and anthropogenic factors in landscape transformation to be determined. Integrated studies of marine and terrestrial sequences on the Murav'inaya Bay coasts form the foundation for reconstructing changes in the Murav'ev-Amursky Peninsula landscapes over the last 5950 cal. Yrs. Pollen and diatom analyses as well as radiocarbon dating provide insight into the landscape response to climate fluctuations during the Middle/Late Holocene. Changes in the depositional environments were essentially controlled by fluctuations in the level of the Sea of Japan, as illustrated by the reconstructed history of Cherepashye Lake, which formed similar to 2000 cal. Yr BP and replaced a lagoon. Several stages in this evolution show variations in the degree of connection with the sea. The materials obtained made it possible to reconstruct the environments at the time when site Cherepakha-13 came into being. The site appeared under climatic conditions similar to those of today, and the sea level was below the present sea level (Zaisanovskaya archeological culture). The people of the Lidovskaya and Yankovskaya archeological cultures settled under a climate warmer than that at present, with a sea level above the present-day sea level, and broadleaved forests with Korean pine grew on the coast. During the Yankovskaya and Krownovskaya cultural period, the climate began to cool and the sea level dropped. These changes led to deterioration of living conditions of these people. In the 13th century, when a Jurchen settlement appeared at Murav'inaya Bay, the coastal plain was dominated by Korean pine-broadleaved forests, and mixed forests were poorer in composition than the earlier forest vegetation. Additionally, alder woodlands became widespread around the lake. In the 17th to 19th centuries, coniferous tree species (and Korean pine in particular) abruptly gained in importance in the vegetation of the peninsula. Secondary oak forests became widely distributed in the 20th century due to intensive human activities. (C) 2017 Elsevier Ltd and INQUA. All rights reserved.
机译:Murav'ev-Amursky半岛是俄罗斯远东地区最稠密和工业发达的地区之一,被列入Bolshoy(更大)vladivostok。在其密集发展开始于大约150年前,半岛的山区部分被针叶林覆盖,混合阔叶林被限制在沿海低地。在工业发展期间植被尤其变化。中/晚全新事短时间气候变化下的天然社区的景观演变与发展特别令人兴趣。结果允许确定景观转化中的天然和人为因素的相对重要性。 Murav'Inaya湾海岸海洋和陆地序列的综合研究形成了在过去5950年CAL中Murav'ev-Amursky半岛景观中的重建变化的基础。 yrs。花粉和硅藻分析以及RadioCarbon约会的洞察力在中/晚全新世期间对气候波动的景观响应提供了深入。沉积环境的变化基本上受日本海平面的波动的控制,如湖泊的重建史如图所示,它与2000 Cal相似。 YR BP并更换了泻湖。该演进中的几个阶段显示了与海洋的连接程度的变化。所获得的材料使得当时Cherepakha-13正在进行时,可以重建环境。该遗址在类似于今天的气候条件下出现,海平面低于目前的海平面(Zaisanovskaya考古文化)。 Lidovskaya和yankovskaya考古文化的人民在气候温暖的情况下,目前的气候升温,海拔高于本日海平面,宽阔的森林与韩国杉木在海岸上增长。在Yankovskaya和Krownovskaya文化期间,气候开始凉爽,海平面下降。这些变化导致这些人的生活条件恶化。在13世纪,当Murav'Inaya湾出现Jurchen Sollement时,沿海平原占据了韩国宽阔的森林,而混合森林的组成较差,而不是早期的森林植被。此外,艾尔林地在湖边普遍普遍。在17日至19世纪,针叶树种类(特别是朝鲜松树)在半岛植被中突然获得。由于密集的人类活动,二次橡木森林在20世纪被广泛分布。 (c)2017年elestvier有限公司和诊断。版权所有。

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