The Ensenada and Buenos Aires formations (Pleistocene) in a quarry near La Plata, Argentina

An interdisciplinary study of a section in a quarry near La Plata sheds new light on the geologic, climatic, and biologic evolution of the northeastern Pampean area of Argentina. The stratigraphic succession is composed of seven mainly colian levels, each one including a soil and separated by a disc...

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Autores principales: Tonni, E.P., Nabel, P., Cione, A.L., Etchichury, M., Tófalo, R., Scillato Yané, G., San Cristóbal, J., Carlini, A., Vargas, D.
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Acceso en línea:http://hdl.handle.net/20.500.12110/paper_08959811_v12_n3_p273_Tonni
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spelling todo:paper_08959811_v12_n3_p273_Tonni2023-10-03T15:42:29Z The Ensenada and Buenos Aires formations (Pleistocene) in a quarry near La Plata, Argentina Tonni, E.P. Nabel, P. Cione, A.L. Etchichury, M. Tófalo, R. Scillato Yané, G. San Cristóbal, J. Carlini, A. Vargas, D. paleoenvironment Pleistocene stratigraphy Argentina An interdisciplinary study of a section in a quarry near La Plata sheds new light on the geologic, climatic, and biologic evolution of the northeastern Pampean area of Argentina. The stratigraphic succession is composed of seven mainly colian levels, each one including a soil and separated by a disconformity. Two geosols defined in northern Buenos Aires Province (Hisisa and El Tala) are identified in the Ensenada Formation. The boundary between the Ensenada and Buenos Aires formations is defined by a conspicuous disconformity which overlies the El Tala Geosol. In the section, the boundary between the Tolypeutes pampaeus (Ensenadan) and Megatherium americanum (lower Lujanian) biozones coincides with that of Ensenada and Buenos Aires formations. The boundary between the Matuyama and Brunhes zones of polarity occurs in the upper part of the Ensenada Formation above the Hisisa Geosol. According to geologic evidence, most of the succession was deposited under semiarid to arid climate. Fil:Nabel, P. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Etchichury, M. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Tófalo, R. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Vargas, D. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. JOUR info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar http://hdl.handle.net/20.500.12110/paper_08959811_v12_n3_p273_Tonni
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic paleoenvironment
Pleistocene
stratigraphy
Argentina
spellingShingle paleoenvironment
Pleistocene
stratigraphy
Argentina
Tonni, E.P.
Nabel, P.
Cione, A.L.
Etchichury, M.
Tófalo, R.
Scillato Yané, G.
San Cristóbal, J.
Carlini, A.
Vargas, D.
The Ensenada and Buenos Aires formations (Pleistocene) in a quarry near La Plata, Argentina
topic_facet paleoenvironment
Pleistocene
stratigraphy
Argentina
description An interdisciplinary study of a section in a quarry near La Plata sheds new light on the geologic, climatic, and biologic evolution of the northeastern Pampean area of Argentina. The stratigraphic succession is composed of seven mainly colian levels, each one including a soil and separated by a disconformity. Two geosols defined in northern Buenos Aires Province (Hisisa and El Tala) are identified in the Ensenada Formation. The boundary between the Ensenada and Buenos Aires formations is defined by a conspicuous disconformity which overlies the El Tala Geosol. In the section, the boundary between the Tolypeutes pampaeus (Ensenadan) and Megatherium americanum (lower Lujanian) biozones coincides with that of Ensenada and Buenos Aires formations. The boundary between the Matuyama and Brunhes zones of polarity occurs in the upper part of the Ensenada Formation above the Hisisa Geosol. According to geologic evidence, most of the succession was deposited under semiarid to arid climate.
format JOUR
author Tonni, E.P.
Nabel, P.
Cione, A.L.
Etchichury, M.
Tófalo, R.
Scillato Yané, G.
San Cristóbal, J.
Carlini, A.
Vargas, D.
author_facet Tonni, E.P.
Nabel, P.
Cione, A.L.
Etchichury, M.
Tófalo, R.
Scillato Yané, G.
San Cristóbal, J.
Carlini, A.
Vargas, D.
author_sort Tonni, E.P.
title The Ensenada and Buenos Aires formations (Pleistocene) in a quarry near La Plata, Argentina
title_short The Ensenada and Buenos Aires formations (Pleistocene) in a quarry near La Plata, Argentina
title_full The Ensenada and Buenos Aires formations (Pleistocene) in a quarry near La Plata, Argentina
title_fullStr The Ensenada and Buenos Aires formations (Pleistocene) in a quarry near La Plata, Argentina
title_full_unstemmed The Ensenada and Buenos Aires formations (Pleistocene) in a quarry near La Plata, Argentina
title_sort ensenada and buenos aires formations (pleistocene) in a quarry near la plata, argentina
url http://hdl.handle.net/20.500.12110/paper_08959811_v12_n3_p273_Tonni
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