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THE SUN, CLIMATE CHANGE AND THE EXPANSION OF THE SCYTHIAN CULTURE AFTER 850 BC

机译:太阳,气候变化和850年后的席克文文化的扩张

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The climate shift towards wetter conditions at the transition from Subboreal to Subatlantic in NW-Europe (ca 850 cal. yrs BC; caused by a decline of solar activity), is also evident in South Siberia. Areas that initially were hostile semi-deserts changed into attractive steppe landscapes with a high biomass production, and therefore high carrying capacity. We focus on south-central Siberia where an acceleration of cultural development and an increase in the density of nomadic Scythian populations took place shortly after 850 BC. We hypothesize a causal relationship between the Scythian expansion and migration, and the early Subatlantic shift towards increased humidity.
机译:在NW-Europe(CA 850 CAR中,从亚底层到亚洲洛杉矶过渡的气候转变为潜伏期(CA 850 CAR。YRS BC;由于太阳能活动的下降),在南西伯利亚也是明显的。最初是敌对半沙漠的地区变成了具有高生物量生产的有吸引力的草原景观,因此高承载能力。我们专注于西伯利亚南部,在850年公元前850年后,不久发生了文化发展的加速和游牧民族人群密度的增加。我们假设席克斯扩张和迁移之间的因果关系,以及早期的亚多兰转向增加湿度。

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