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Volcanism and Settlement of the Northern Slope of the Central Caucasus in the Middle Paleolithic: New Data from Saradj-Chuko Grotto

机译:中肿性中央高加索北坡的火山主义和解决:Saradj-Chuko Grotto的新数据

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The problem of the settlement of the territory of the Northern Caucasus in the Paleolithic and its dependence on volcanic activity factors, climate, and shift in ecological niches is very relevant in modern domestic and foreign studies. Previous research at Mezmaiskaya cave in the northwestern Caucasus revealed that volcanism significantly affected the Middle Paleolithic population of this region and the disappearance of the Neanderthal population. In 2016, the first stratified Middle Paleolithic site was discovered in the Elbrus region (Republic of Kabardino-Balkaria), on the northern slopes of the central Caucasus. This site was called Saradj-Chuko grotto. This region is fundamentally important for understanding the dynamics of the Northern Caucasus settlement in the Paleolithic because it is located at the crossroads between the northern and southern slopes. The only obsidian outcrop in the Northern Caucasus is located also here. Obsidian is a volcanic raw material that was highly valued by ancient people in that period and transported by Neanderthals hundreds of kilometers. We have investigated the chemical composition and morphology of minerals in 76 samples of the ZZ0 longitudinal section in Saradj-Chuko grotto. As a result, traces of volcanic activity were revealed in 2 (6A and 4) out of 11 layers. It has been found that volcanism in the Middle Paleolithic affected the settlement of the Elbrus region and most likely the entire northern slope of the central Caucasus. Specifically, layer 6A (where ash was found) overlaps layer 6B (the level of active habitation in the grotto). After the eruption recorded in layer 6A, the Neanderthals only occasionally visited the cave. Preliminary conclusions are made about a possible source of ash in these layers of Saradj-Chuko grotto. The materials were analyzed in a wide context of the currently known data on the presence of ashes in other sites of the Caucasus.
机译:在旧石器时代的北部高加索地区定居的问题及其对生态利基的火山活动因素,气候和转变的依赖性在现代国内外研究方面非常相关。以前在西北高加索的Mezmaiskaya洞穴上的研究表明,火山主义显着影响了该地区的古石英中较近人口和尼安德特人口的消失。在2016年,在埃尔布鲁斯地区(Kabardino-Balkaria共和国)发现了第一个分层的中肿点,在中央高加索的北坡上。这个网站被称为Saradj-Chuko Grotto。该地区对了解旧石器时代北部高加索沉降的动态,因为它位于北部和南坡之间的十字路口。北部高加索的唯一的黑曜石露头也在这里。黑曜石是那个时期古代人民高度重视的火山原料,并由尼安德特人运输数百公里。我们研究了Saradj-Chuko Grotto的ZZ0纵向部分76个样品中的矿物质的化学成分和形态。结果,在11层中的2(6A和4)中显示了火山活性的痕量。已经发现,中肿性的火山主义影响了埃尔布鲁斯地区的沉降,最有可能是中央高加索的整个北坡。具体地,层6a(发现灰烬)与层6b重叠(石窟中的主动居所水平)。在爆发层6a中爆发后,只有偶尔偶尔访问洞穴。初步结论是关于这些赛勒拉德·楚科石窟中的可能灰烬来源。在当前已知的数据的广泛背景下分析了材料,就在高加索地区的其他部位存在灰烬中。

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