Four millennia of geomorphic change and human settlement in the lower Usumacinta–Grijalva River Basin, Mexico

IF 3 3区 地球科学 Q2 GEOGRAPHY, PHYSICAL Progress in Physical Geography-Earth and Environment Pub Date : 2023-02-19 DOI:10.1177/03091333231156506
E. Muñoz-Salinas, Duncan E. Cook, M. Castillo, T. Beach, Sheryl Luzzadder-Beach
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Abstract

The lower Usumacinta–Grijalva River Basin contains one of the richest biodiversity landscapes of the Maya region. Our research is based on (1) an integrative literature review of the geomorphological and archaeological papers published about the lower Usumacinta–Grijalva River Basin and (2) topographic analysis of digital elevation models using a geographical information system to explore the relationship between past human settlement and landscape accessibility along the coastal plain of Tabasco. This work provides a new synthesis of previous research and proposes new models for the geomorphic evolution of the lower Usumacinta–Grijalva River Basin in the context of four millennia of human land use and settlement. For the evolution of the strand-plain of the Usumacinta and Grijalva rivers, there are two published geochronological models that provide different chronologies. We discuss here how both geochronological models encompass Pre-Columbian human settlement in the delta. Interestingly, we notice that one of them overlaps a possible high-magnitude flood event (or events) that drove large geomorphic change around 750 CE (1200 BP), with implications for settlement patterns and chronology. Based on topographical analysis of the eastern-distal sector of the Usumacinta–Grijalva delta, we propose a new model for the evolution of this area with implications for the human occupation during the Mesoamerican Terminal Classic and Early Postclassic on the delta. As one of the main conclusions, we propose that the Pom–Atasta water bodies predate much of the Usumacinta–Grijalva delta and the most recent phase of delta building overlays the original lagoon barriers, resulting in a geomorphic setting more attractive to local human occupation after the Terminal Classic period. According to one of the geochronological models of the delta, this dates to ca. 900 CE, preceding the establishment of nearby settlements such as Atasta.
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墨西哥乌苏马辛塔-格里哈尔瓦河流域下游四千年的地貌变化和人类定居
乌苏马辛塔-格里哈尔瓦河下游流域是玛雅地区生物多样性最丰富的地区之一。我们的研究基于(1)对Usumacinta-Grijalva河下游的地貌和考古论文进行综合文献综述;(2)利用地理信息系统对数字高程模型进行地形分析,探索塔巴斯科沿海平原过去人类住区与景观可达性之间的关系。这项工作对以前的研究进行了新的综合,并提出了在四千年人类土地利用和定居背景下的Usumacinta-Grijalva河下游流域地貌演化的新模型。对于乌苏马辛塔河和格里哈尔瓦河的滩平原的演变,有两种已发表的地质年代学模型提供了不同的年代学。我们在这里讨论了这两种地质年代学模型是如何涵盖前哥伦布时期三角洲的人类定居的。有趣的是,我们注意到其中一个可能与公元750年(1200年前)左右导致大规模地貌变化的一次(或多次)高震级洪水事件重叠,这对定居模式和年代产生了影响。本文通过对Usumacinta-Grijalva三角洲东部远段的地形分析,提出了该地区演化的新模式,并对中美洲末端经典期和后古典期早期三角洲人类活动的影响进行了分析。作为主要结论之一,我们提出,波姆-阿塔斯塔水体早于乌苏马辛塔-格里哈尔瓦三角洲的大部分地区,而三角洲建筑的最新阶段覆盖了原始的泻湖屏障,导致了一个地貌环境,在终端古典时期之后对当地人类居住更具吸引力。根据三角洲的一个地质年代学模型,这可以追溯到公元900年左右,在阿塔斯塔等附近定居点建立之前。
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来源期刊
CiteScore
7.20
自引率
5.10%
发文量
53
审稿时长
>12 weeks
期刊介绍: Progress in Physical Geography is a peer-reviewed, international journal, encompassing an interdisciplinary approach incorporating the latest developments and debates within Physical Geography and interrelated fields across the Earth, Biological and Ecological System Sciences.
期刊最新文献
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