南美洲大排水系统重新排列的时间:基于形态学和生态学证据的研究

IF 3.1 2区 地球科学 Q2 GEOGRAPHY, PHYSICAL Geomorphology Pub Date : 2024-10-30 DOI:10.1016/j.geomorph.2024.109457
Fernanda Apericida da Silva Cassemiro PhD , André Augusto Rodrigues Salgado PhD (Professor) , Rodrigo Wagner Paixão PhD , Éric Andrade Rezende PhD
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引用次数: 0

摘要

本研究旨在描述和确定南美洲巴拉那河流域和圣弗朗西斯科河流域这两个面积各超过 60 万平方公里的大流域之间的一次重大排水重排的时间。我们利用地貌分析和计算黑顶帽(BTH)法来确定河流捕获点。通过使用淡水鱼类分布和进化数据,我们进行了生物地理学分析,以评估鱼类的扩散模式。我们的研究结果表明,过去巴拉那河上游(当地称为格兰德河)曾经流入现在的圣弗朗西斯科河流域。生物地理学分析证实了格兰德河与圣弗朗西斯科河之间过去的联系。该分析还显示,在距今 650 万年到 200 万年之间,发生了一次重大的排水系统重新安排,当时巴拉那河流域接纳了格兰德河及其支流(萨普卡伊河)。在这一过程中,圣弗朗西斯科盆地向巴拉那河盆地流失了 5 万平方公里的面积。
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The timing of large drainage rearrangement in South America: A study based on morphological and ecological evidence
This study aims to characterize and determine the timing of a major drainage rearrangement between two vast river basins, each exceeding 600,000 km2: the Paraná and São Francisco basins in South America. We used geomorphological analyses and the computational Black Top Hat (BTH) method to identify river captures. By using freshwater fish distribution and evolution data, we performer biogeographical analyses to assess the fish dispersal patterns. Our results show that in the past the upper Paraná River (known locally as the Grande River) once flowed into what is now the São Francisco River Basin. Biogeographical analysis corroborates this past connection between Grande and São Fracisco rivers This analysis reveals also that between 6 and 5 and 2 million years ago, a significant drainage rearrangement occurred, when the Paraná River Basin captured the Grande River and its tributary (the Sapucaí River). In this process the São Francisco Basin losing 50,000 km2 of its area to the Paraná River Basin.
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来源期刊
Geomorphology
Geomorphology 地学-地球科学综合
CiteScore
8.00
自引率
10.30%
发文量
309
审稿时长
3.4 months
期刊介绍: Our journal''s scope includes geomorphic themes of: tectonics and regional structure; glacial processes and landforms; fluvial sequences, Quaternary environmental change and dating; fluvial processes and landforms; mass movement, slopes and periglacial processes; hillslopes and soil erosion; weathering, karst and soils; aeolian processes and landforms, coastal dunes and arid environments; coastal and marine processes, estuaries and lakes; modelling, theoretical and quantitative geomorphology; DEM, GIS and remote sensing methods and applications; hazards, applied and planetary geomorphology; and volcanics.
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