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Abstract:

This paper presents the first palynological record for the dynamics of geoecological belts of the Eastern Cordillera in northwestern Argentina prior to the Last Glacial Maximum (LGM). The study was carried out on a 5-m deep sedimentary core raised at Laguna Blanca (23°09’S, 65°12’W; 4,256 m a.s.l.), province of Jujuy. The geochronol­ogy was based on three14C dating by AMS method. Results show the sensitive response of the geoecological belts to temperature and effective moisture variations from ca. 29,000 to ca. 25,000 cal. years BP. The High Andean belt probably suffered an altitudinal descent forced by intense cold climate conditions ca. 29,000 cal. years BP, and may have reached a comparable distribution to the present one on 26,300 cal. years BP, favored by a milder climate. The Puna belt did not suffer great changes, since it remained with low representation in the pollen spectrum. High percentages of tree species from the Yungas ca. 29,000 cal. years BP are probably a response to the intensification of anabatic winds ascending the slope of the Sub-Andean Range towards the Eastern Cordillera. These results represent an important contribution to the paleoenvironmental discussion of the Late Pleistocene for the northwestern Argentina, where the available information on vegetation history is scarce. © 2016, Servicio Nacional de Geologia y Mineria. All rights reserved.

Registro:

Documento: Artículo
Título:Palynological evidence of the geoecological belts dynamics from Eastern Cordillera of NW Argentina (23° S) during the Pre-Last Glacial Maximum
Autor:Torres, G.R.; Lupo, L.C.; Kulemeyer, J.J.; Pérez, C.F.
Filiación:Centro de Investigación y Transferencia (CIT-Jujuy), CONICET, Avda. Bolivia 1711, Jujuy, 4600, Argentina
Laboratorio de Palinología, Facultad de Ciencias Agrarias, Universidad Nacional de Jujuy, Alberdi 47, Jujuy, 4600, Argentina
Cátedra de Suelos, Facultad de Ingeniería, Universidad Nacional de Jujuy, Gorriti 237, Jujuy, 4600, Argentina
CONICET, Avda. Rivadavia 1917, CABA, C1033AAJ, Argentina
Departamento de Ciencias-Departamento de Ciencias de la Atmósfera y los Océanos, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Pabellón II, 2º piso, Ciudad Universitaria (1428), Buenos Aires, Argentina
Palabras clave:Eastern cordillera; Geoecological belts; Jujuy; Laguna blanca; Pollen; Pre last glacial maximum; environmental change; geochronology; geological record; Last Glacial Maximum; paleoclimate; paleoenvironment; paleotemperature; palynology; Pleistocene; sediment core; vegetation history; Argentina; Jujuy; Laguna Blanca National Park; Neuquen; Puna
Año:2016
Volumen:43
Número:2
Página de inicio:151
Página de fin:165
DOI: http://dx.doi.org/10.5027/andgeoV43n2-a01
Título revista:Andean Geology
Título revista abreviado:Andean Geol.
ISSN:07187092
Registro:https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_07187092_v43_n2_p151_Torres

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Citas:

---------- APA ----------
Torres, G.R., Lupo, L.C., Kulemeyer, J.J. & Pérez, C.F. (2016) . Palynological evidence of the geoecological belts dynamics from Eastern Cordillera of NW Argentina (23° S) during the Pre-Last Glacial Maximum . Andean Geology, 43(2), 151-165.
http://dx.doi.org/10.5027/andgeoV43n2-a01
---------- CHICAGO ----------
Torres, G.R., Lupo, L.C., Kulemeyer, J.J., Pérez, C.F. "Palynological evidence of the geoecological belts dynamics from Eastern Cordillera of NW Argentina (23° S) during the Pre-Last Glacial Maximum " . Andean Geology 43, no. 2 (2016) : 151-165.
http://dx.doi.org/10.5027/andgeoV43n2-a01
---------- MLA ----------
Torres, G.R., Lupo, L.C., Kulemeyer, J.J., Pérez, C.F. "Palynological evidence of the geoecological belts dynamics from Eastern Cordillera of NW Argentina (23° S) during the Pre-Last Glacial Maximum " . Andean Geology, vol. 43, no. 2, 2016, pp. 151-165.
http://dx.doi.org/10.5027/andgeoV43n2-a01
---------- VANCOUVER ----------
Torres, G.R., Lupo, L.C., Kulemeyer, J.J., Pérez, C.F. Palynological evidence of the geoecological belts dynamics from Eastern Cordillera of NW Argentina (23° S) during the Pre-Last Glacial Maximum . Andean Geol. 2016;43(2):151-165.
http://dx.doi.org/10.5027/andgeoV43n2-a01