Paleoclimatic evidence in duricrust, paleosoils and siliciclastic deposit of the Cenozonic of Uruguay
The continental deposits found in southern and western Uruguay show important climatic changes along the Cenozoic. The sequence begins with Paleocene palustrine carbonates known as the Queguay Formation, associated with calcretes of phreatic origin which developed mainly on fluvial sediments of Merc...
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Acceso en línea: | https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v65_n4_p674_Tofalo http://hdl.handle.net/20.500.12110/paper_00044822_v65_n4_p674_Tofalo |
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paper:paper_00044822_v65_n4_p674_Tofalo2023-06-08T14:26:22Z Paleoclimatic evidence in duricrust, paleosoils and siliciclastic deposit of the Cenozonic of Uruguay Tofalo, Ofelia Rita de las Mercedes Duricrusts Paleoclimates Paleosols Siliciclastic sedimentites climate variation duricrust fluvial deposit loess Miocene Paleocene paleoclimate paleosol pedogenesis Pleistocene siliciclastic deposit Uruguay The continental deposits found in southern and western Uruguay show important climatic changes along the Cenozoic. The sequence begins with Paleocene palustrine carbonates known as the Queguay Formation, associated with calcretes of phreatic origin which developed mainly on fluvial sediments of Mercedes Formation (Late Cretaceous), and indicates a semiarid climate, seasonally contrasted. The Asencio Formation (Early Eocene) is separated from Mercedes Formation by the Yapeyu paleosurface, limiting two sedimentary cycles. Fluvial deposits lies above this surface, on which Ultisols developed under a warm and humid climate; periods of intense dryness would provoked their induration and formation of ferricretes, which under subsequent increased precipitation were dismantled. Above, Fray Bentos Formation (Oligocene-Early Miocene) lies unconformably. It is composed by loessic sediments deposited in a semiarid climate, paleosols and diverse pedogenic calcretes developed on these sediments, among which a new type named tubular calcrete, are here described; in the latter the tubular units are related to a coarse prismatic structure derived from shrink-swell processes and the surface morphology of this calcrete refers to a gilgai microrelief, typical for Vertisols. The pedogenic calcretes point to a seasonal semiarid climate. The Raigón Formation (Late Pliocene- Middle Pleistocene) of fluvial origin was formed in a humid period, and shows a paleosol at the top developed in a seasonally contrasted climate. Lying unconformably, the Libertad Formation (Early to Middle Pleistocene) is composed by loesses deposited during glacial periods that were subsequently modified by pedogenesis during interglacial periods. Fil:Tófalo, O.R. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. 2009 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v65_n4_p674_Tofalo http://hdl.handle.net/20.500.12110/paper_00044822_v65_n4_p674_Tofalo |
institution |
Universidad de Buenos Aires |
institution_str |
I-28 |
repository_str |
R-134 |
collection |
Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) |
topic |
Duricrusts Paleoclimates Paleosols Siliciclastic sedimentites climate variation duricrust fluvial deposit loess Miocene Paleocene paleoclimate paleosol pedogenesis Pleistocene siliciclastic deposit Uruguay |
spellingShingle |
Duricrusts Paleoclimates Paleosols Siliciclastic sedimentites climate variation duricrust fluvial deposit loess Miocene Paleocene paleoclimate paleosol pedogenesis Pleistocene siliciclastic deposit Uruguay Tofalo, Ofelia Rita de las Mercedes Paleoclimatic evidence in duricrust, paleosoils and siliciclastic deposit of the Cenozonic of Uruguay |
topic_facet |
Duricrusts Paleoclimates Paleosols Siliciclastic sedimentites climate variation duricrust fluvial deposit loess Miocene Paleocene paleoclimate paleosol pedogenesis Pleistocene siliciclastic deposit Uruguay |
description |
The continental deposits found in southern and western Uruguay show important climatic changes along the Cenozoic. The sequence begins with Paleocene palustrine carbonates known as the Queguay Formation, associated with calcretes of phreatic origin which developed mainly on fluvial sediments of Mercedes Formation (Late Cretaceous), and indicates a semiarid climate, seasonally contrasted. The Asencio Formation (Early Eocene) is separated from Mercedes Formation by the Yapeyu paleosurface, limiting two sedimentary cycles. Fluvial deposits lies above this surface, on which Ultisols developed under a warm and humid climate; periods of intense dryness would provoked their induration and formation of ferricretes, which under subsequent increased precipitation were dismantled. Above, Fray Bentos Formation (Oligocene-Early Miocene) lies unconformably. It is composed by loessic sediments deposited in a semiarid climate, paleosols and diverse pedogenic calcretes developed on these sediments, among which a new type named tubular calcrete, are here described; in the latter the tubular units are related to a coarse prismatic structure derived from shrink-swell processes and the surface morphology of this calcrete refers to a gilgai microrelief, typical for Vertisols. The pedogenic calcretes point to a seasonal semiarid climate. The Raigón Formation (Late Pliocene- Middle Pleistocene) of fluvial origin was formed in a humid period, and shows a paleosol at the top developed in a seasonally contrasted climate. Lying unconformably, the Libertad Formation (Early to Middle Pleistocene) is composed by loesses deposited during glacial periods that were subsequently modified by pedogenesis during interglacial periods. |
author |
Tofalo, Ofelia Rita de las Mercedes |
author_facet |
Tofalo, Ofelia Rita de las Mercedes |
author_sort |
Tofalo, Ofelia Rita de las Mercedes |
title |
Paleoclimatic evidence in duricrust, paleosoils and siliciclastic deposit of the Cenozonic of Uruguay |
title_short |
Paleoclimatic evidence in duricrust, paleosoils and siliciclastic deposit of the Cenozonic of Uruguay |
title_full |
Paleoclimatic evidence in duricrust, paleosoils and siliciclastic deposit of the Cenozonic of Uruguay |
title_fullStr |
Paleoclimatic evidence in duricrust, paleosoils and siliciclastic deposit of the Cenozonic of Uruguay |
title_full_unstemmed |
Paleoclimatic evidence in duricrust, paleosoils and siliciclastic deposit of the Cenozonic of Uruguay |
title_sort |
paleoclimatic evidence in duricrust, paleosoils and siliciclastic deposit of the cenozonic of uruguay |
publishDate |
2009 |
url |
https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v65_n4_p674_Tofalo http://hdl.handle.net/20.500.12110/paper_00044822_v65_n4_p674_Tofalo |
work_keys_str_mv |
AT tofaloofeliaritadelasmercedes paleoclimaticevidenceinduricrustpaleosoilsandsiliciclasticdepositofthecenozonicofuruguay |
_version_ |
1768544529394171904 |