High-precision U-Pb calibration of Carboniferous glaciation and climate history, Paganzo Group, NW Argentina

The duration and geographic extent of Carboniferous glacial events in southern Gondwana remain poorly constrained despite recent evidence for a more dynamic glacial history than previously considered. We report 10 high-precision (2σ ± <0.1%) U-Pb ages for the Permian-Carboniferous Paganzo Group,...

Descripción completa

Detalles Bibliográficos
Publicado: 2010
Materias:
Acceso en línea:https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00167606_v122_n9-10_p1480_Gulbranson
http://hdl.handle.net/20.500.12110/paper_00167606_v122_n9-10_p1480_Gulbranson
Aporte de:
id paper:paper_00167606_v122_n9-10_p1480_Gulbranson
record_format dspace
spelling paper:paper_00167606_v122_n9-10_p1480_Gulbranson2023-06-08T14:38:51Z High-precision U-Pb calibration of Carboniferous glaciation and climate history, Paganzo Group, NW Argentina Argentina Chronostratigraphy Climate history Climate shifts Depositional environment Dryland Fluvial deposits Glacial history High-precision Late Paleozoic Permian Radiometric calibrations Regime shift Regional climate Sub-humid U-Pb ages Western region Calibration Clay deposits Deposits Feldspar deposits Lead Glacial geology age determination aridity calibration Carboniferous geochronology glaciation paleoclimate precision uranium-lead dating Argentina Blanco Basin Paganzo Basin The duration and geographic extent of Carboniferous glacial events in southern Gondwana remain poorly constrained despite recent evidence for a more dynamic glacial history than previously considered. We report 10 high-precision (2σ ± <0.1%) U-Pb ages for the Permian-Carboniferous Paganzo Group, NW Argentina, that redefine the chronostratigraphy of the late Paleozoic Paganzo and Río Blanco Basins, and significantly refine the timing of glacial events and climate shifts in the western region of southern Gondwana. Radiometric calibration of the Paganzo Group indicates three pulses of Carboniferous glaciation in the mid-Visean, the late Serpukhovian to earliest Bashkirian, and between the latest Bashkirian to early Moscovian. An abrupt shift in depositional style from high-sinuosity single-storied fluvial deposits and clay-rich paleosols to low-sinuosity multistoried feldspathic fluvial deposits intercalated with eolianites and calcic paleosols is constrained to the latest Moscovian and earliest Kasimovian. These constraints indicate a relatively abrupt climate shift from humid-subhumid to nonseasonal semiarid regional climate conditions that occurred significantly earlier than previously inferred (Early Permian). This period of high-latitude aridity was contemporaneous with a shift to dryland depositional environments and a major vegetation regime shift documented throughout the Pangean paleotropics in the Pennsylvanian. © 2010 Geological Society of America. 2010 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00167606_v122_n9-10_p1480_Gulbranson http://hdl.handle.net/20.500.12110/paper_00167606_v122_n9-10_p1480_Gulbranson
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic Argentina
Chronostratigraphy
Climate history
Climate shifts
Depositional environment
Dryland
Fluvial deposits
Glacial history
High-precision
Late Paleozoic
Permian
Radiometric calibrations
Regime shift
Regional climate
Sub-humid
U-Pb ages
Western region
Calibration
Clay deposits
Deposits
Feldspar deposits
Lead
Glacial geology
age determination
aridity
calibration
Carboniferous
geochronology
glaciation
paleoclimate
precision
uranium-lead dating
Argentina
Blanco Basin
Paganzo Basin
spellingShingle Argentina
Chronostratigraphy
Climate history
Climate shifts
Depositional environment
Dryland
Fluvial deposits
Glacial history
High-precision
Late Paleozoic
Permian
Radiometric calibrations
Regime shift
Regional climate
Sub-humid
U-Pb ages
Western region
Calibration
Clay deposits
Deposits
Feldspar deposits
Lead
Glacial geology
age determination
aridity
calibration
Carboniferous
geochronology
glaciation
paleoclimate
precision
uranium-lead dating
Argentina
Blanco Basin
Paganzo Basin
High-precision U-Pb calibration of Carboniferous glaciation and climate history, Paganzo Group, NW Argentina
topic_facet Argentina
Chronostratigraphy
Climate history
Climate shifts
Depositional environment
Dryland
Fluvial deposits
Glacial history
High-precision
Late Paleozoic
Permian
Radiometric calibrations
Regime shift
Regional climate
Sub-humid
U-Pb ages
Western region
Calibration
Clay deposits
Deposits
Feldspar deposits
Lead
Glacial geology
age determination
aridity
calibration
Carboniferous
geochronology
glaciation
paleoclimate
precision
uranium-lead dating
Argentina
Blanco Basin
Paganzo Basin
description The duration and geographic extent of Carboniferous glacial events in southern Gondwana remain poorly constrained despite recent evidence for a more dynamic glacial history than previously considered. We report 10 high-precision (2σ ± <0.1%) U-Pb ages for the Permian-Carboniferous Paganzo Group, NW Argentina, that redefine the chronostratigraphy of the late Paleozoic Paganzo and Río Blanco Basins, and significantly refine the timing of glacial events and climate shifts in the western region of southern Gondwana. Radiometric calibration of the Paganzo Group indicates three pulses of Carboniferous glaciation in the mid-Visean, the late Serpukhovian to earliest Bashkirian, and between the latest Bashkirian to early Moscovian. An abrupt shift in depositional style from high-sinuosity single-storied fluvial deposits and clay-rich paleosols to low-sinuosity multistoried feldspathic fluvial deposits intercalated with eolianites and calcic paleosols is constrained to the latest Moscovian and earliest Kasimovian. These constraints indicate a relatively abrupt climate shift from humid-subhumid to nonseasonal semiarid regional climate conditions that occurred significantly earlier than previously inferred (Early Permian). This period of high-latitude aridity was contemporaneous with a shift to dryland depositional environments and a major vegetation regime shift documented throughout the Pangean paleotropics in the Pennsylvanian. © 2010 Geological Society of America.
title High-precision U-Pb calibration of Carboniferous glaciation and climate history, Paganzo Group, NW Argentina
title_short High-precision U-Pb calibration of Carboniferous glaciation and climate history, Paganzo Group, NW Argentina
title_full High-precision U-Pb calibration of Carboniferous glaciation and climate history, Paganzo Group, NW Argentina
title_fullStr High-precision U-Pb calibration of Carboniferous glaciation and climate history, Paganzo Group, NW Argentina
title_full_unstemmed High-precision U-Pb calibration of Carboniferous glaciation and climate history, Paganzo Group, NW Argentina
title_sort high-precision u-pb calibration of carboniferous glaciation and climate history, paganzo group, nw argentina
publishDate 2010
url https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00167606_v122_n9-10_p1480_Gulbranson
http://hdl.handle.net/20.500.12110/paper_00167606_v122_n9-10_p1480_Gulbranson
_version_ 1768545536440270848