Macedo Rodrigo S, Teixeira Wenceslau G, Corrêa Marcelo M, Martins Gilvan C, Vidal-Torrado Pablo
Soil Science Department, University of São Paulo, Piracicaba, São Paulo, Brazil.
Embrapa Solos, Rio de Janeiro, Rio de Janeiro, Brazil.
PLoS One. 2017 May 23;12(5):e0178038. doi: 10.1371/journal.pone.0178038. eCollection 2017.
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.
被称为亚马逊黑土(ADE)的人为土见证了亚马逊中部定居模式的强化和人口增长。因此,人们观察到一种反复出现的模式:因家庭活动和废物处理而产生的带有ADE的土堆。本研究的目的是证明巴西伊兰杜巴市这些人类活动与ADE的成土形成过程之间的关系。从两个ADE区域(网纹层)和一个非人为土剖面采集了扰动和未扰动的土壤样本。进行了物理、化学、微观形态和扫描电子显微镜-能谱分析。网纹层的粗颗粒物质主要由石英、铁结核、陶瓷和木炭碎片组成,细颗粒物质是有机-矿物。网纹层的颜色与木炭碎片数量之间存在直接关系。ADE的厚度是由于木炭通过生物扰动在深度上重新分布,将地下层转变为人为层而形成的。ADE呈现出地球化学和动物成因的颗粒状微团聚体。铁结核在网纹层中的降解加剧,促进了一个反向成土过程,有助于黄化过程。令人惊讶的是,人类活动也有利于粘土的分散和粘化作用;陶瓷碎片和孔隙上的粘土涂层表明这是一个当前正在发生的过程。确定为有助于ADE形成的过程包括:i)使用火添加有机残留物和陶瓷制品(堆积作用);ii)人类、根系和大型动物的机械作用(生物扰动);iii)生物扰动导致较深层的黑化;iv)粘化作用和铁结核的降解。这项研究为亚马逊中部关于ADE形成过程的考古研究提供了新的支持,并证实了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土过程这一假设。