Climate and tectonics along the southern margin of the Puna Plateau, NW Argentina: Origin of the late Cenozoic Punaschotter conglomerates

Lindsay M. Schoenbohm, Barbara Carrapa, Heather M. McPherson, Jonathan R. Pratt, Sharon Bywater-Reyes, Estelle Mortimer

Research output: Chapter in Book/Report/Conference proceedingChapter

11 Scopus citations

Abstract

Basins around the margin of the Puna Plateau in NW Argentina each record the onset over a few hundred thousand years of alluvial-fan facies sedimentation with the deposition of the Punaschotter conglomerates in the late Cenozoic, despite differing tectonic histories. Their striking similarity suggests that these conglomerates might have a common origin, such as the climatically driven coarsening and increase in sedimentation rate proposed to have occurred worldwide at 4-2 Ma. With this contribution, we present new U-Pb geochronology of intercalated ashes that bracket the onset of Punaschotter deposition along the margin of the Puna Plateau in the Fiambalá and El Cajon Basins. Combining this with existing data, we explore the relative roles of climate and tectonics in shaping sedimentation in this region. Our analysis reveals that Punaschotter deposition was diachronous and only occurred if both aridity and structural deformation were present. Development of orographic barriers and global climate change may have contributed to establishing regional aridity. In the eastern part of the study region (Santa Maria and Angastaco), onset of Punaschotter deposition tracks the establishment of aridity. In the already arid western basins (Fiambalá, Corral Quemado), a reactivation of structural deformation may have triggered the onset of Punaschotter deposition. Our study shows that initiation of coarse alluvial facies in this part of the Andes largely preceded the 4-2 Ma global climate change and emphasizes the coupled nature of local climate and tectonics in controlling sedimentation.

Original languageEnglish (US)
Title of host publicationGeodynamics of a Cordilleran Orogenic System
Subtitle of host publicationThe Central Andes of Argentina and Northern Chile
EditorsMihai N. Ducea, Mihai N. Ducea, Peter G. DeCelles, Paul A. Kapp, Barbara Carrapa
PublisherGeological Society of America
Pages251-260
Number of pages10
ISBN (Electronic)9780813712123
DOIs
StatePublished - Jan 1 2015

Publication series

NameMemoir of the Geological Society of America
Volume212
ISSN (Print)0072-1069

ASJC Scopus subject areas

  • Geology

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    Schoenbohm, L. M., Carrapa, B., McPherson, H. M., Pratt, J. R., Bywater-Reyes, S., & Mortimer, E. (2015). Climate and tectonics along the southern margin of the Puna Plateau, NW Argentina: Origin of the late Cenozoic Punaschotter conglomerates. In M. N. Ducea, M. N. Ducea, P. G. DeCelles, P. A. Kapp, & B. Carrapa (Eds.), Geodynamics of a Cordilleran Orogenic System: The Central Andes of Argentina and Northern Chile (pp. 251-260). (Memoir of the Geological Society of America; Vol. 212). Geological Society of America. https://doi.org/10.1130/2015.1212(13)