Late Pleistocene and Holocene sea levels from Bahia Anegada, Buenos Aires Province: geochronology and correlations

Littoral deposits were formed during the three transgressive episodes, two during the Late Pleistocene and the third mid-Holocene. The oldest episode is correlated with the Sangamon Interglacial, the middle one with the mid-Wisconsin Interstadial and the youngest is assigned to the mid-Holocene. The...

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Guardado en:
Detalles Bibliográficos
Publicado: 1993
Materias:
Holocene
interglacial
Pleistocene (late)
sea level
transgression
Argentina
Bahia Anegada
Buenos Aires
Buenos Aires Province
Acceso en línea:https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_NIS19192_v48_n3-4_p207_Weiler
http://hdl.handle.net/20.500.12110/paper_NIS19192_v48_n3-4_p207_Weiler
Aporte de:
Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires
id paper:paper_NIS19192_v48_n3-4_p207_Weiler
record_format dspace
spelling paper:paper_NIS19192_v48_n3-4_p207_Weiler2023-06-08T16:39:56Z Late Pleistocene and Holocene sea levels from Bahia Anegada, Buenos Aires Province: geochronology and correlations Holocene interglacial Pleistocene (late) sea level transgression Argentina Bahia Anegada Buenos Aires Buenos Aires Province Littoral deposits were formed during the three transgressive episodes, two during the Late Pleistocene and the third mid-Holocene. The oldest episode is correlated with the Sangamon Interglacial, the middle one with the mid-Wisconsin Interstadial and the youngest is assigned to the mid-Holocene. The deposits belonging to the Sangamon have 14C ages older than 43 000 yr BP. Mid-Wisconsin deposits are those of barrier islands and lagoons. 14C ages for these deposits range between 28 700 and 38 500 yr BP. -from English summary 1993 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_NIS19192_v48_n3-4_p207_Weiler http://hdl.handle.net/20.500.12110/paper_NIS19192_v48_n3-4_p207_Weiler
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic Holocene
interglacial
Pleistocene (late)
sea level
transgression
Argentina
Bahia Anegada
Buenos Aires
Buenos Aires Province
spellingShingle Holocene
interglacial
Pleistocene (late)
sea level
transgression
Argentina
Bahia Anegada
Buenos Aires
Buenos Aires Province
Late Pleistocene and Holocene sea levels from Bahia Anegada, Buenos Aires Province: geochronology and correlations
topic_facet Holocene
interglacial
Pleistocene (late)
sea level
transgression
Argentina
Bahia Anegada
Buenos Aires
Buenos Aires Province
description Littoral deposits were formed during the three transgressive episodes, two during the Late Pleistocene and the third mid-Holocene. The oldest episode is correlated with the Sangamon Interglacial, the middle one with the mid-Wisconsin Interstadial and the youngest is assigned to the mid-Holocene. The deposits belonging to the Sangamon have 14C ages older than 43 000 yr BP. Mid-Wisconsin deposits are those of barrier islands and lagoons. 14C ages for these deposits range between 28 700 and 38 500 yr BP. -from English summary
title Late Pleistocene and Holocene sea levels from Bahia Anegada, Buenos Aires Province: geochronology and correlations
title_short Late Pleistocene and Holocene sea levels from Bahia Anegada, Buenos Aires Province: geochronology and correlations
title_full Late Pleistocene and Holocene sea levels from Bahia Anegada, Buenos Aires Province: geochronology and correlations
title_fullStr Late Pleistocene and Holocene sea levels from Bahia Anegada, Buenos Aires Province: geochronology and correlations
title_full_unstemmed Late Pleistocene and Holocene sea levels from Bahia Anegada, Buenos Aires Province: geochronology and correlations
title_sort late pleistocene and holocene sea levels from bahia anegada, buenos aires province: geochronology and correlations
publishDate 1993
url https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_NIS19192_v48_n3-4_p207_Weiler
http://hdl.handle.net/20.500.12110/paper_NIS19192_v48_n3-4_p207_Weiler
_version_ 1769175831442096128

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