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Pedogenetic processes in anthrosols with pretic horizon (Amazonian Dark Earth) in Central Amazon, Brazil.

机译:巴西中部亚马逊河流域具有前掠层(亚马逊暗地球)的人类成岩过程。

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摘要

Anthrosols known as Amazonian Dark Earth (ADE) have borne witness to the intensification of sedentary patterns and the demographic increase in Central Amazon. As a result, a recurring pattern has been observed of mounds with ADE arising from domestic activities and the disposal of waste. The objective of this research was to demonstrate the relationship of these anthropic activities with pedogenetic formation processes of ADE in the municipality of Iranduba, Brazil. Disturbed and undisturbed soil samples were taken from two areas of ADE (pretic horizon) and from a non-anthropic pedon. Physical, chemical, micromorphological and SEM-EDS analyses were performed. The coarse material of the pretic horizons consisted predominantly of quartz, iron nodules, ceramics and charcoal fragments, and the fine material is organo-mineral. There was a direct relationship between the color of pretic horizons and the number of charcoal fragments. The thickness of the ADE results from the redistribution of charcoal at depth through bioturbation, transforming subsurface horizons into anthropic horizons. ADE presents granular microaggregates of geochemical and zoogenetic origin. Degradation of iron nodules is intensified in pretic horizons, promoting a reverse pedogenic process contributing to the xanthization process. Surprisingly the anthropic activities also favor clay dispersion and argilluviation; clay coatings on the ceramic fragments and in the pores demonstrate that this is a current process. Processes identified as contributing to ADE genesis included: i) addition of organic residues and ceramic artifacts (cumulization) with the use of fire; ii) mechanical action of humans, roots and macrofauna (bioturbation); iii) melanization of deeper horizons as a result of bioturbation; iv) argilluviation and degradation of iron nodules. This study offers new support to archaeological research in respect to ADE formation processes in Central Amazon and confirmed the hypothesis that ancient anthropic activities may trigger and/or accelerate pedogenetic processes previously credited only to natural causes.
机译:被称为亚马逊黑土(ADE)的人类住处见证了久坐模式的加剧和亚马逊河中部人口的增长。结果,观察到了由家庭活动和废物处置引起的带有ADE的土丘的重复模式。这项研究的目的是证明这些人类活动与巴西伊兰杜巴市ADE的成岩作用形成过程之间的关系。扰动和未扰动的土壤样本取自两个区域的ADE(非视界)和一个非人类的。进行了物理,化学,微观形态和SEM-EDS分析。原始层的粗物质主要由石英,铁结核,陶瓷和木炭碎片组成,而细物质是有机矿物。上层地平线的颜色与木炭碎片的数量之间存在直接的关系。 ADE的厚度是由于生物扰动使木炭在深处重新分布而产生的,从而将地下视界转换为人类视界。 ADE提供了地球化学和动物遗传学起源的颗粒状微聚集体。铁结节的降解在原始视野中加剧,促进了反向黄土化过程,从而促进了黄原化过程。令人惊讶的是,人类活动也有利于粘土的分散和泥炭化作用。陶瓷碎片上和孔隙中的粘土涂层表明这是当前的过程。被确定为有助于ADE发生的过程包括:i)使用火添加有机残留物和陶瓷伪像(累积); ii)人,根和大型动物的机械作用(生物扰动); iii)由于生物扰动而使较深层的黑化; iv)铁结节的精氨化和降解。这项研究为中部亚马逊地区ADE形成过程的考古研究提供了新的支持,并证实了以下假设:古代人类活动可能触发和/或加速以前仅归因于自然原因的成岩过程。

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