Rock magnetism in two loess–paleosol sequences in Córdoba, Argentina

This work presents new rock magnetic results along two loess–paleosol profiles in nearby locations in Argentina. The main objective of this study is to compare the magnetic signals and mineral content of two profiles and determine if the climate during Marine Isotope Stage 5 (MIS 5) and MIS 3 were s...

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Autores principales:	Orgeira, María Julia, Vasquez, Carlos Alberto, Tofalo, Ofelia Rita de las Mercedes
Publicado:	2015
Materias:	Geomorphology Mineralogy MIS 5 Rock magnetism Isotopes Lithology Magnetite Minerals Rocks Sediments Climate condition Environmental magnetism Laboratory procedures Late Pleistocene Magnetic signals Marine isotope stages Water saturations Magnetism
Acceso en línea:	https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_18666280_v73_n10_p6323_Rouzaut http://hdl.handle.net/20.500.12110/paper_18666280_v73_n10_p6323_Rouzaut
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

id	paper:paper_18666280_v73_n10_p6323_Rouzaut
record_format	dspace
spelling	paper:paper_18666280_v73_n10_p6323_Rouzaut2025-07-30T19:05:21Z Rock magnetism in two loess–paleosol sequences in Córdoba, Argentina Orgeira, María Julia Vasquez, Carlos Alberto Tofalo, Ofelia Rita de las Mercedes Geomorphology Mineralogy MIS 5 Rock magnetism Geomorphology Isotopes Lithology Magnetite Mineralogy Minerals Rocks Sediments Climate condition Environmental magnetism Laboratory procedures Late Pleistocene Magnetic signals Marine isotope stages Rock magnetism Water saturations Magnetism This work presents new rock magnetic results along two loess–paleosol profiles in nearby locations in Argentina. The main objective of this study is to compare the magnetic signals and mineral content of two profiles and determine if the climate during Marine Isotope Stage 5 (MIS 5) and MIS 3 were similar to the present one. The two profiles are located in two different geomorphological settings, with effects on the water saturation characteristics and seasonality. Selected samples taken at these profiles were analyzed using laboratory procedures and environmental magnetism parameters to determine the climatic influence during the Late Pleistocene. Despite their proximity there are several differences between both profiles, such as their depth and geomorphological positions among others. The results of these analyses led to the following conclusions: climate conditions during MIS 5 were very similar to those of the present conditions. The hypothesis for this area suggests a slight increase in the magnetic signal associated with the generation of small amounts of magnetite and preservation of detrital magnetite and titano-magnetite. The results in this paper show a slight gain in the buried soils of Córdoba that would confirm the hypothesis. © 2014, Springer-Verlag Berlin Heidelberg. Fil:Orgeira, M.J. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Vásquez, C. 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. 2015 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_18666280_v73_n10_p6323_Rouzaut http://hdl.handle.net/20.500.12110/paper_18666280_v73_n10_p6323_Rouzaut
institution	Universidad de Buenos Aires
institution_str	I-28
repository_str	R-134
collection	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic	Geomorphology Mineralogy MIS 5 Rock magnetism Geomorphology Isotopes Lithology Magnetite Mineralogy Minerals Rocks Sediments Climate condition Environmental magnetism Laboratory procedures Late Pleistocene Magnetic signals Marine isotope stages Rock magnetism Water saturations Magnetism
spellingShingle	Geomorphology Mineralogy MIS 5 Rock magnetism Geomorphology Isotopes Lithology Magnetite Mineralogy Minerals Rocks Sediments Climate condition Environmental magnetism Laboratory procedures Late Pleistocene Magnetic signals Marine isotope stages Rock magnetism Water saturations Magnetism Orgeira, María Julia Vasquez, Carlos Alberto Tofalo, Ofelia Rita de las Mercedes Rock magnetism in two loess–paleosol sequences in Córdoba, Argentina
topic_facet	Geomorphology Mineralogy MIS 5 Rock magnetism Geomorphology Isotopes Lithology Magnetite Mineralogy Minerals Rocks Sediments Climate condition Environmental magnetism Laboratory procedures Late Pleistocene Magnetic signals Marine isotope stages Rock magnetism Water saturations Magnetism
description	This work presents new rock magnetic results along two loess–paleosol profiles in nearby locations in Argentina. The main objective of this study is to compare the magnetic signals and mineral content of two profiles and determine if the climate during Marine Isotope Stage 5 (MIS 5) and MIS 3 were similar to the present one. The two profiles are located in two different geomorphological settings, with effects on the water saturation characteristics and seasonality. Selected samples taken at these profiles were analyzed using laboratory procedures and environmental magnetism parameters to determine the climatic influence during the Late Pleistocene. Despite their proximity there are several differences between both profiles, such as their depth and geomorphological positions among others. The results of these analyses led to the following conclusions: climate conditions during MIS 5 were very similar to those of the present conditions. The hypothesis for this area suggests a slight increase in the magnetic signal associated with the generation of small amounts of magnetite and preservation of detrital magnetite and titano-magnetite. The results in this paper show a slight gain in the buried soils of Córdoba that would confirm the hypothesis. © 2014, Springer-Verlag Berlin Heidelberg.
author	Orgeira, María Julia Vasquez, Carlos Alberto Tofalo, Ofelia Rita de las Mercedes
author_facet	Orgeira, María Julia Vasquez, Carlos Alberto Tofalo, Ofelia Rita de las Mercedes
author_sort	Orgeira, María Julia
title	Rock magnetism in two loess–paleosol sequences in Córdoba, Argentina
title_short	Rock magnetism in two loess–paleosol sequences in Córdoba, Argentina
title_full	Rock magnetism in two loess–paleosol sequences in Córdoba, Argentina
title_fullStr	Rock magnetism in two loess–paleosol sequences in Córdoba, Argentina
title_full_unstemmed	Rock magnetism in two loess–paleosol sequences in Córdoba, Argentina
title_sort	rock magnetism in two loess–paleosol sequences in córdoba, argentina
publishDate	2015
url	https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_18666280_v73_n10_p6323_Rouzaut http://hdl.handle.net/20.500.12110/paper_18666280_v73_n10_p6323_Rouzaut
work_keys_str_mv	AT orgeiramariajulia rockmagnetismintwoloesspaleosolsequencesincordobaargentina AT vasquezcarlosalberto rockmagnetismintwoloesspaleosolsequencesincordobaargentina AT tofaloofeliaritadelasmercedes rockmagnetismintwoloesspaleosolsequencesincordobaargentina
_version_	1840323303077576704

Rock magnetism in two loess–paleosol sequences in Córdoba, Argentina

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