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Titlebook: Geology and Paleontology of the Quaternary of Uruguay; Martin Ubilla,Sergio Martínez Book 2016 United Nations University 2016 Holocene.Mam

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樓主: Encounter
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發(fā)表于 2025-3-23 13:24:12 | 只看該作者
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發(fā)表于 2025-3-23 14:31:58 | 只看該作者
https://doi.org/10.1007/978-3-642-96526-5ution in this region of South America. Most of the units described have a rich paleontological content encompassing wood, fresh-water mollusks, pollen, trace-fossils, and a panoply of vertebrates, with mammals the dominant group (updated tables and selected material on them is included). Lithologica
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發(fā)表于 2025-3-23 18:14:33 | 只看該作者
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發(fā)表于 2025-3-24 01:19:45 | 只看該作者
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發(fā)表于 2025-3-24 06:40:03 | 只看該作者
Marine and Transitional Deposits,e last thousands of years. They yield abundant molluskan faunas that are crucial for these interpretations, and other invertebrates, vertebrates, ichnofaunas, microfaunas and microfloras. These deposits have been classified in a disorderly way over the years with a large number of stratigraphical un
17#
發(fā)表于 2025-3-24 13:36:11 | 只看該作者
Continental Beds,ution in this region of South America. Most of the units described have a rich paleontological content encompassing wood, fresh-water mollusks, pollen, trace-fossils, and a panoply of vertebrates, with mammals the dominant group (updated tables and selected material on them is included). Lithologica
18#
發(fā)表于 2025-3-24 18:38:25 | 只看該作者
The Quaternary of Uruguay at Regional Scale,e past, many names and units were introduced in the literature, mainly designating facies, but currently, and thanks to a good data base of numerical ages, we can simplify this former, almost anarchic situation, with the correlation by numerical ages made much easier. In Uruguay, the Pleistocene dep
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發(fā)表于 2025-3-24 21:09:10 | 只看該作者
20#
發(fā)表于 2025-3-25 01:24:43 | 只看該作者
https://doi.org/10.1007/978-3-642-96526-5entary beds are representative of different time periods, including a fluvial braided system related to a proto Uruguay river in western Uruguay, fluvial contexts with channels and plain-flooded facies along with paleosoils in northern Uruguay, and transitional deposits in southern Uruguay. Accordin
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