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首页> 外文期刊>Quaternary International >Neolithic and Aeneolithic Environments in the Central Primor'ye Region (the Bol'shaya Ussurka Valley), the Russian Far East
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Neolithic and Aeneolithic Environments in the Central Primor'ye Region (the Bol'shaya Ussurka Valley), the Russian Far East

机译：俄罗斯远东中部普里默里地区（博尔沙雅乌苏尔卡山谷）的新石器时代和新石器时代环境

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摘要

Holocene climates and environmental changes in the Russian Primor'ye are still insufficiently documented in comparison with the more southerly Far East Asian areas. Systematic field investigations performed during the last years in the central Primor'ye Region adjacent to Manchuria have produced a new and most fascinating picture on the local cultural development between 9th and 3rd Mill. BP. Multiproxy palaeoecology records from the key stratified archaeological sites in the Bol'shaya Ussurka (Iman) River basin display marked environmental shifts witnessed by the contextual geological and pollen evidence from the occupations loci believed to reflect the early prehistoric formation in these woodland territories during the early and mid-Holocene. The reconstructed vegetation history shows a good correlation of the Neolithic appearance in the Iman Basin with the mapped trend of a regional climate amelioration characterized by increased temperature and humidity rates, culminating in the Holocene Climatic Optimum (9-6 ka BP), and the subsequent cultural diversification and progress during the late Neolithic and Aeneolithic (Palaeo-Metal) periods. Changes in the regional vegetation cover extrapolated from pollen sequences, C-14-dated to ca. 4500-3500 cal. BP, are likely linked to anthropogenic pressure to the pristine environment with the site-vicinity taiga clearance for new pastures by people of the Almazinka Culture, marking the climax of the local Neolithic development. A uniform adaptation to local natural settings with mixed basic (huntingegathering and extensive pastoral) economies persisted throughout millennia until historical times. Most of the cultural horizons are sealed in abiotically distorted palaeosols, indicating climate instability and marked environmental shifts in the north-central Primor'ye area during the Holocene. (C) 2015 Elsevier Ltd and INQUA. All rights reserved.
机译：与较南端的远东亚洲地区相比，俄罗斯Primor'ye的全新世气候和环境变化仍然没有得到充分的记录。过去几年中，在靠近满洲的滨海边疆区中部进行的系统野外调查，对9号和3号磨坊之间的当地文化发展产生了新的，最令人着迷的印象。 BP。来自Bol'shaya Ussurka（Iman）流域关键分层考古遗址的多代古生态记录显示了明显的环境变化，据职业场所的背景地质和花粉证据表明，这些变化反映出这些林地的早期史前形成和全新世中期。重建的植被历史表明，伊曼盆地新石器时代的出现与区域气候改善的趋势具有良好的相关性，其特征是温度和湿度的升高，并最终达到全新世气候最佳（9-6 ka BP），随后文化在新石器时代和新石器时代（古金属）晚期的多元化和进步。从花粉序列推断出的区域植被覆盖度变化（C-14日期至大约11月）。 4500-3500卡路里BP可能与原始环境的人为压力有关，Almazinka文化的人们对新牧场进行了地点附近的针叶林清除，这标志着当地新石器时代的发展高潮。在整个千年以前，一直到混合历史的基础（狩猎采集和广泛的畜牧业）经济对当地自然环境的统一适应。大多数文化视野都被封闭在非生物变形的古土壤中，这表明在全新世期间气候不稳定以及北中部普里莫尔地区发生了明显的环境变化。 （C）2015 Elsevier Ltd和INQUA。版权所有。

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