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巴西里约热内卢北海岸公元前7000年以来喜湿森林被田野植被取代的孢粉学证据。

Palynological evidence of the replacement of the hygrophilous forest by field vegetation during the last 7,000 years B.P. in the northern coast of Rio de Janeiro, Brazil.

作者信息

Luz Cynthia F P da, Barth Ortrud M, Martin Louis, Silva Cleverson G, Turcq Bruno J

机构信息

Instituto de Botânica, Núcleo de Pesquisa em Palinologia, São Paulo, SP, Brasil.

出版信息

An Acad Bras Cienc. 2011 Sep;83(3):939-52. doi: 10.1590/s0001-37652011005000031. Epub 2011 Aug 5.

DOI:10.1590/s0001-37652011005000031
PMID:21830004
Abstract

Historians claim that European colonizers of the northern coast of Rio de Janeiro State found vast herbaceous fields when arrived in this region. Hypotheses about the origin of these fields include forest burning by the Goitacás indians and periodical floods by the Paraíba do Sul River and the lagoon system. The palynologycal analysis of two lake cores obtained in the municipality of Campos dos Goytacazes revealed opening episodes of hygrophilous forest and the establishment of field vegetation, recorded at ca. 6,500 and ca. 4,000 (14)C yr BP. The partial replacement of forest by field vegetation in the first episode was probably caused by floods of the lower areas during the development of the Holocene lagoon phase. During the second episode, successions of vegetational patterns occurred due to lowering of the sea level. Drying and enlarging of the coastal plain have allowed its colonization by herbs and heliophyte plants. The palynological analysis does not provide any evidence that sustains the theories of use of fire and agricultural activities by indigenous groups during these periods.

摘要

历史学家称,里约热内卢州北部海岸的欧洲殖民者抵达该地区时发现了广阔的草本田野。关于这些田野的起源假说包括戈伊塔卡斯印第安人焚烧森林以及南帕拉伊巴河和泻湖系统的周期性洪水。对在坎波斯-多斯戈伊塔卡泽斯市获取的两个湖泊岩芯进行的孢粉学分析显示,在约6500和约4000碳-14年BP记录到了喜湿森林的开放期和田野植被的建立。在第一阶段,森林被田野植被部分取代可能是由于全新世泻湖阶段发展期间低地的洪水所致。在第二阶段,由于海平面下降,植被模式发生了演替。沿海平原的干燥和扩大使其被草本植物和阳生植物殖民。孢粉学分析没有提供任何证据支持这些时期土著群体使用火和进行农业活动的理论。

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