仪式化景观中的人类与气候:哥伦比亚东部高原托塔湖的案例

Maria I Vélez, Jorge Salgado, Miguel Delgado, Luisa F Patiño, Broxton Bird, Jaime H Escobar, Sebastian Fajardo
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摘要

托塔是位于哥伦比亚东安第斯山脉阿尔蒂普拉诺地区的一个安第斯湖泊,埃雷拉和穆伊斯卡社会政治等级森严的社会在这里繁衍生息了数千年。对他们来说,湖泊和周围的森林是进行各种活动(包括宗教仪式)的场所。在这项研究中,我们利用硅藻、同位素和地球化学进行了多代理古气候学重建,试图了解该湖在自然气候变化和人类活动影响下的变化路径。硅藻记录主要是浮游生物 Staurosirella dubia 和浮游生物 Aulacoseira,包括 A. cf lirata、A. granulata、A. distans 和 A. ambigua。硅藻被划分为不同的功能组别,用于推断湖沼学的变化,并通过沉积物的地球化学特征来重建过去的环境。结果显示,湖泊在三个主要时期发生了显著变化,时间分别为公元约 800 年至 1200 年、1200 年至 1500 年以及 1500 年至 1900 年。与该地区考古记录、人种史记载和气候的相关性表明,这些变化是与考古阶段的变化、西班牙人的到来以及最近的工业革命和小冰河时期同时发生的。
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Humans and climate in ritualized landscapes, the case of Lake Tota in the eastern highlands of Colombia
Tota is an Andean lake located in the Altiplano of the Eastern Andes of Colombia where socio-politically hierarchical societies of the Herrera and Muisca, flourished for millennia. To them, the lake and surrounding forest were places used for diverse of activities including religious rituals. In this study we produced a multi-proxy paleolimnological reconstruction using diatoms, isotopes, and geochemistry, to try to understand the lake’s pathways of change in response to natural climatic variations and anthropogenic activities. The diatom record is dominated by tychoplanktonic Staurosirella dubia and planktonic Aulacoseira species including species A. cf lirata, A. granulata, A. distans, and A. ambigua. Diatoms were grouped into functional groups and used to infer limnological changes that were further complemented with the geochemistry of the sediments to reconstruct the past environment. Results show three main periods in which the lake changed significantly, these are dated from ~800 to 1200, 1200 to 1500, and 1500 to 1900 CE. A correlation with the archeological record of the region, ethnohistoric accounts and climate suggests that these changes occurred simultaneously with changes in archeological stages, the Spanish arrival, and more recently by the industrial revolution, and the Little Ice Age.
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