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在东南美洲的全新世纪期间的人类与环境的相互作用:快速的气候变化和人口动态

Astolfo G M Araujo¹, Letícia Cristina Correa², Glauco Constantino Perez¹

¹Museum of Archaeology and Ethnology, University of São Paulo, São Paulo, Brazil.

|February 3, 2025

概括

南美洲的Holocene中期"古老差距"比以前想象的要大,影响了亚马逊和潘坦纳尔等地区. 气候变化,而不仅仅是干旱,可能导致了这些人口转移,为全球变暖的影响提供了洞察力.

科学领域:

考古学的考古学
古代环境科学古代环境科学
气候科学气候科学

背景情况:

中期的全新世 (Holocene) 时期.
陈旧的差距的差距 .
这种气候变化以前被归因于南美洲低地低温时期的干旱程度增加.
最近的古老环境和考古数据允许重新评估这一现象.

研究的目的:

重新评估中 Holocene 的空间范围和原因.
陈旧的差距的差距 .
在南美洲东部.
为了提供一个更广泛的理解人类-环境的互动自晚普莱斯托纪以来.

主要方法:

考古环境重建的分析.
综合了来自南美洲低地地区的最新考古数据.
对现有假设的重新评估,对现有假设的重新评估.
陈旧的差距的差距 .
. . . . . . . . . . . . . . 这是一个很好的时刻.

主要成果:

在Holocene中期,人口减少的地区比最初提出的更为广泛,包括亚马逊和潘坦纳尔的部分地区.
考古证据表明,一些地区的振荡表明重新占领.
增加的气候变化,而不是仅仅增加的干旱,被确定为主要的驱动因素.

结论:

中期的全新世 (Holocene) 时期.
陈旧的差距的差距 .
南美洲东部的气候变化现象在地理上广泛,并由气候变化加剧驱动.
这些发现对理解全球变暖对人类人口的影响有重要意义.

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