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  • 1
    Publication Date: 2015-07-30
    Description: Meandering fluvial channels and their meander belts are common in modern continental sedimentary basins, yet compose a minor constituent of the reported fluvial rock record. Here we document exhumed amalgamated meander belt deposits from the upper Jurassic Morrison Formation, Utah (United States). The size of the amalgamated meander belt (9000 km 2 ) is significantly larger than any documented previously and comparable in size to those from modern sedimentary basins. We describe a representative outcrop of sandy point bar deposits that shows features considered characteristic of both braided and meandering fluvial systems. Lateral accretion sets compose 〈5% of the outcrop area, yet point bar morphology is clearly visible in plan view. We suggest that difficulties in the identification of sandy, amalgamated meander belt deposits indicate that they have gone largely unrecognized in the rock record. Their recognition has important implications for basin-scale reconstructions of fluvial systems and interpretation of tectonic setting.
    Print ISSN: 0091-7613
    Electronic ISSN: 1943-2682
    Topics: Geosciences
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  • 2
    Publication Date: 2015-06-23
    Description: The stratigraphic record is heavily biased because it is uniquely composed of sediments that were laid down in basins, whereas the majority of the present and historic land surface of the planet is composed of areas that are in net long-term erosion with no preservation potential. Global mapping and quantification of the distribution of currently active sedimentary basins suggest that only 16% of Earth’s terrestrial land surface is within sedimentary basins; the remainder of the land is in upland areas that will not be represented in the future rock record. Furthermore, 60% of the modern basin area has an arid climate, as opposed to 27% of the land surface. Tectonic classification of modern basins indicates that intracratonic and foreland basins cover the greatest area, whereas forearc, extensional, and strike-slip basins are the least represented by area. While this modern snapshot does not account for differences in subsidence rate or basin longevity, the mapping and quantification of modern basins highlight the incompleteness of the stratigraphic record, and the importance of caution when assuming "the present is the key to the past."
    Print ISSN: 0091-7613
    Electronic ISSN: 1943-2682
    Topics: Geosciences
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