解释暗地球的形成过程可能有助于理解其定居策略

IF 5.7 1区 农林科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
Martin Petr Janovský , Lenka Lisá , Marek Hladík , Manuel Arroyo-Kalin , Marian Mazuch , Pavel Samec , Laszlo Ferenczi
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引用次数: 0

摘要

本研究的重点是对中世纪早期mikul遗址边缘保存的占领沉积物进行地质考古分析,mikul遗址是大摩拉维亚原始国家(公元8 - 10世纪)的中心。将土壤地球化学、粒度分析和微观形态观察相结合,应用于两个剖面,并结合更广泛的沉积学和考古学背景,应用于复杂的考古结构。从给定的数据可以明显看出,该地区的沉降受到地下水增加的强烈影响,因此,用渗透性砂反复平整地形是必要的维护,随后是由人类排泄物浓缩的沉积物的沉积,以及土壤形成的过程。这些沉积条件是暗地球形成的最重要因素之一,是由厨房垃圾、木炭、骨头碎片和粪便的生物混合驱动的。这项研究提出了捷克在中世纪高度城市环境之外的第一个黑暗地球描述之一,特别指出它是中世纪早期山丘上的内滞期Arenic Technosols。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Explaining Dark Earth’s formation processes may help to understand the settlement strategy
This study focuses on the geoarchaeological analysis of occupation deposits preserved at the edge of the early medieval site of Mikulčice, the centre of the Great Moravian proto-state (8th–10th century CE). The combination of soil geochemistry, grain size analyses and micromorphological observations applied to two sections and linked with wider sedimentological and archaeological context were applied to complicated archaeological structures. From the given data is obvious, that settling in this area was strongly influenced by the presence of increased underground water, so repeated terrain levelling with permeable sands was the necessary maintenance, followed by the deposition of sediments enriched by human waste, alongside episodes of soils formation. These sedimentary deposits condition were one of the most important factors for the formation of Dark Earth, driven by biological mixing of kitchen waste, charcoal, bone fragments, and excrements. The study presents one of the first descriptions of Dark Earth in Czechia outside a high medieval urban context, specifically identifying it as Endo-stagnic Arenic Technosols at an early medieval hillfort.
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来源期刊
Catena
Catena 环境科学-地球科学综合
CiteScore
10.50
自引率
9.70%
发文量
816
审稿时长
54 days
期刊介绍: Catena publishes papers describing original field and laboratory investigations and reviews on geoecology and landscape evolution with emphasis on interdisciplinary aspects of soil science, hydrology and geomorphology. It aims to disseminate new knowledge and foster better understanding of the physical environment, of evolutionary sequences that have resulted in past and current landscapes, and of the natural processes that are likely to determine the fate of our terrestrial environment. Papers within any one of the above topics are welcome provided they are of sufficiently wide interest and relevance.
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