巴西米纳斯吉拉斯州乌纳伊考古遗址格鲁塔-多-金蒂欧-升的霞石多样性

Ludmila Gurjão, Ondemar Dias, Jandira Neto, Alena Iñiguez
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摘要

巴西首次古寄生虫学分析涉及 Gruta do Gentio ll(GGll)考古遗址,该遗址与乌纳陶瓷传统的开端(公元前 13,000-410 年)有关,有两个生存地层,一个古老的地层与狩猎采集者有关,另一个较新的地层与园艺人口有关。乌纳传统的重要文化痕迹,如陶器、织物、用动物牙齿和贝壳制成的装饰品以及食物残渣,也是在 GGII 发掘期间发现的。粪便化石或矿化粪便是岩石学和沉积学研究的重要内容,可提供有关寄生虫、环境、生产者来源和饮食的宝贵信息。在本研究中,对 GGll 桡足类粪便进行了形态学和形态计量学处理,以确定研究地理位置内样本的可能来源。共生石的鉴定结果显示,共生石有四种不同的形态,包括复合型、扁平型、球形和圆柱形,有 10 种不同的颜色,异质性地分布在 16 个区和 11 个地层中,表明不仅人类共生石种类繁多,动物共生石也是如此。根据收集到的数据以及之前的考古评估,我们可以提出一个主要的 GGII 古生态方案,即在巴西东南部的更新世和全新世时期,有动物和人类使用洞穴。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Coprolite diversity from the archeological site Gruta Do Gentio Ll, Unaí, Minas Gerais, Brazil
The first paleoparasitological analyses in Brazil are related to the Gruta do Gentio ll (GGll) an archeological site related to the beginning of the Una ceramist tradition (13,000–410 cal B.P.), with two subsistence horizons, an ancient one related do hunter-gatherers, and a more recent one related to a horticulturist population. Crucial cultural traces of Una tradition such as pottery, fabric, adornments made from animal teeth and shells, and food remnants were also identified during the GGII excavations. Coprolites, fossilized or mineralized feces are important elements in the studies on taphonomy and sedimentology, and yield valuable information on parasitological, environmental, producer origin, and diet. In the present study, GGll coprolites were submitted to morphological and morphometrical procedures to identify the probable origin of samples within the geographical location of study. The results of the identification of coprolites showed four different morphotypes including complex, flat, spherical, and cylindrical, in 10 distinct colors, distributed heterogeneously in 16 sectors and 11 stratigraphic layers, indicating a great variety of not only human but animal coprolites. With the collected data, along with previous archeological evaluations, we can propose a primary GGII paleoecological scenario, with the presence of animals and humans that used de cave in the Pleistocene and Holocene times of Southeast Brazil.
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