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首页> 外文期刊>Quaternary International >Late Holocene environmental changes in the vicinity of Kiiltepe (Kayseri), Central Anatolia, Turkey
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Late Holocene environmental changes in the vicinity of Kiiltepe (Kayseri), Central Anatolia, Turkey

机译:土耳其中部安那托利亚Kiiltepe(Kayseri)附近的晚全新世环境变化

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摘要

The Central Anatolian Region (CAR), being a high orogenic plateau (1000-1500 masl) is located between the Pontides in the north and the Taurides in the south, has a semi-arid climate. Significant changes occurred in vegetation and human activities within the CAR due to climate changes during the Holocene. On the other hand, the anthropogenic effect on vegetation in the region which has experienced intensive settlements since the beginning of the Neolithic period, has become the destiny of the region. In this study, the pollen data obtained from Lake Engir are presented to show the effect of the late Holocene vegetation, climate changes and anthropogenic effect on vegetation around the archaeological settlement of Kultepe. The archaeological settlement of Kultepe which is an important Assyrian trade colony, dated between 3000 BC and 1000 BP, is located in the north of Kayseri in the CAR. Within the scope of this study, aiming to shed light on the paleo-environmental conditions during this settlement period, the pollen data characterizing the period between 2300 and 300 BP were obtained from core samples collected from Lake Engir near Kultepe. A total of 71 taxa were identified from palynological analysis of core samples. Significant changes in paleoclimatic conditions and vegetation were determined from these analysis. Significant changes were experienced between the years 1930-1820, 1850-1760, 1760-1650 and 1650-1470 BP in vegetation. The climate changes indicated by vegetation changes were determined as wet and dry periods. Wet periods took place between the years 2300-1850, 1760-1650, 1400-1150 and 920-300 BP, and dry periods took place in the years 1850-1760 and 1650-1400 and 1150-920 BP. The Beysehir Occupation Phase representing an intensive agricultural period occurred between the years 1850-1400 BP, and this period suddenly ended at 1400 BP. This situation is related to the abandonment of the land with regard to the Arab raids on Anatolia between the years 1400-1150 BP. The pine forests developed again in this period. Agriculture and animal husbandry activities in which cereal farming was dominant started since 1050 BP. (C) 2018 Elsevier Ltd and INQUA. All rights reserved.
机译:中部安那托利亚地区(CAR)是一个高造山带高原(1000-1500 masl),位于北部的庞特德斯山脉和南部的陶里德斯山脉之间,气候为半干旱。由于全新世期间的气候变化,中非共和国境内的植被和人类活动发生了重大变化。另一方面,自新石器时代开始以来,人为地带对该地区植被的密集影响已成为该地区的命运。在这项研究中,呈现了从恩吉尔湖获得的花粉数据,以显示晚全新世植被,气候变化和人为影响对库尔特佩考古定居点附近的植被的影响。库尔特佩(Kultepe)的考古定居点是亚述重要的贸易殖民地,其历史可追溯到公元前3000年至1000 BP,位于中非共和国开塞利的北部。在本研究的范围内,为了阐明该沉降期的古环境条件,从库尔特佩附近的恩吉尔湖采集的岩心样本获得了表征2300至300 BP期间的花粉数据。从核心样品的孢粉学分析中共鉴定出71个分类单元。通过这些分析确定了古气候条件和植被的重大变化。在1930年至1820年,1850-1760年,1760-1650年和1650-1470年间的植被BP发生了重大变化。植被变化所指示的气候变化被确定为干湿期。湿期发生在2300-1850、1760-1650、1400-1150和920-300 BP之间,而干旱期发生在1850-1760和1650-1400和1150-920 BP之间。代表集约化农业时期的贝西希尔占领阶段发生在1850-1400 BP之间,而这一时期突然在1400 BP结束。这种情况与在1400年至1150年BP之间对安纳托利亚的阿拉伯袭击的土地被放弃有关。在此期间,松树林再次发展。自1050 BP以来,开始以谷物农业为主的农业和畜牧业活动。 (C)2018爱思唯尔有限公司和INQUA。版权所有。

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