中世纪南滨海地区发展过程中地质系统转变的证据:Steklyanukha-2堡垒

T. Kornyushenko, N. Razjigaeva, L. Ganzey, T. Grebennikova, E. Kudryavtseva, Y. Piskareva, S. Prokopets
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引用次数: 0

摘要

以Steklyanukha-2中世纪城堡为例,分析了人类活动对景观的影响。对要塞内的地下土壤、堡垒基质、文化层和表层土壤进行了取样。除了在现场取样的材料外,还研究了Steklyanukha河高洪泛区上全新世沉积物的两个剖面。介绍了孢粉谱和硅藻谱的研究结果。恢复了各种考古文化形成时期的古景观,并确定了人为影响植被的迹象。高洪泛区部分掩埋的土壤是扬科夫斯卡亚文化在这片土地上出现期间环境历史的天然档案。土壤是在河谷水分减少的条件下形成的;年龄估计在2万年以上。牛轭湖沉积物形成于1.6 ~ 0.5 ka,是中世纪河谷活跃发育时期。部分顶部的冲积平原沉积物表明,在小冰河期,山谷被大量浇灌。发现了铁器时代早期、漠河时代和中世纪晚期河谷下部定居的花粉标志。次生桦树和橡树林发育的信号被识别。在中世纪形成的文化层和沉积物中发现了Ambrosia和Xanthium花粉,这是山谷农业活动的可靠证据。在人为干扰地区也发现了常见的植物花粉。对城堡洼地中硅藻的研究证实了考古学家的假设,即它是用来储存水的。堡垒和高洪泛区表层土壤的花粉谱反映了19世纪下半叶以来附近河谷农业的积极发展。外来和共生植物和杂草的花粉以及致病真菌(大豆和水稻的病原体)的孢子和火灾指标在这里发现最多。
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Evidence of geosystems transformation during Medieval development of South Primorye: Steklyanukha-2 fortress
We analyzed human impact on landscapes on the example of Steklyanukha-2 Medieval fortress, which is a multi-layered archaeological site, and adjacent territories. Buried soils, rampart matrix, cultural layer and surface soils were sampled within the fortress. Along with the material sampled at the site, two sections of the Upper Holocene deposits of the high floodplain of the Steklyanukha River were studied. The results of studying the sporo-pollen spectra and diatoms are presented. The paleo-landscapes during the formation of various archaeological cultures have been restored and the signs of anthropogenic impact on vegetation have been identified. The buried soil in the section of the high floodplain is a natural archive for the environment history during the appearance of the people of the Yankovskaya Culture on this territory. The soil was formed under conditions of decreasing watering in the valley; the age is estimated at more than 2 ka. Oxbow lake deposits had been accumulated from 1.6 to 0.5 ka, when the valley was actively developed in the Middle Ages. Floodplain deposits at the top of the sections indicate that the valley has been heavily watered during the Little Ice Age. Pollen signs of settlements of the lower part of the valley in the Early Iron Age, Mohe and Late Middle Ages were found. Signals of the development of secondary birch and oak forests are identified. Ambrosia and Xanthium pollen, which are reliable evidence of agricultural activity in the valley, was found in the cultural layer and sediments that formed in the Middle Ages. The pollen of plants common in anthropogenically disturbed territories was also found. The study of diatoms in a depression within the fortress confirmed the archaeologists’ assumption that it was used to store water reserves. The pollen spectra from the surface soils in the fortress and the high floodplain reflect the active agricultural development of the nearby river valleys since the second half of the 19th century. The largest amount of pollen of alien and synanthropic plants and weeds, as well as spores of pathogenic fungi (pathogens of soybeans and rice) and fire indicators were found here.
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