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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:气候和人类对全新世晚期和历史时期的Murav'ev Amursky半岛(俄罗斯远东)景观发展的影响

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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人口最稠密且工业发达的地区之一,并被包括在符拉迪沃斯托克(Blashoy)(大符拉迪沃斯托克)中。在大约150年前开始密集发展之前,该半岛的山区被针叶林覆盖,混合阔叶林仅限于沿海低地。在工业发展过程中,植被发生了显着变化。在中/晚全新世短期气候变化下,土著社区的景观演变和发展尤其令人关注。结果允许确定自然和人为因素在景观转化中的相对重要性。对Murav'inaya湾海岸的海洋和陆地序列的综合研究,为重建过去5950 cal的Murav'ev-Amursky半岛景观的变化奠定了基础。是的花粉和硅藻分析以及放射性碳年代测定可以洞悉中/晚全新世期间景观对气候波动的响应。沉积环境的变化基本上受日本海平面波动的控制,如Cherepashye湖的重建历史所说明的那样,形成的历史类似于2000 cal。年BP并更换了一个泻湖。在这一演变过程中的几个阶段显示出与海洋的联系程度存在差异。所获得的材料使得在Cherepakha-13工地诞生时就可以重建环境。该地点出现在与今天类似的气候条件下,并且海平面低于当前海平面(Zaisanovskaya考古文化)。 Lidovskaya和Yankovskaya考古文化的人们定居在比现在更高的气候下,海平面高于当今的海平面,沿海有红松阔叶林生长。在Yankovskaya和Krownovskaya文化时期,气候开始变凉,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,当女真人定居点出现在Murav'inaya湾时,沿海平原以红松阔叶红树林为主,混合林的成分比早期的森林植被差。此外,al木林在湖周围变得很普遍。在17至19世纪,针叶树种(尤其是红松)在半岛的植被中突然变得越来越重要。由于人类的密集活动,次生橡树林在20世纪变得广泛分布。 (C)2017爱思唯尔有限公司和INQUA。版权所有。

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