Implications of variable late Cenozoic surface uplift across the Peruvian central Andes View Full Text


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Article Info

DATE

2019-12

AUTHORS

Kurt E. Sundell, Joel E. Saylor, Thomas J. Lapen, Brian K. Horton

ABSTRACT

Changes in Earth's surface elevation can be linked to the geodynamic processes that drive surface uplift, which in turn modulate regional climate patterns. We document hydrogen isotopic compositions of hydrated volcanic glasses and modern stream waters to determine late Cenozoic surface uplift across the Peruvian central Andes. Modern water isotopic compositions reproduce mean catchment elevations to a precision better than ±500 m (1σ). Glass isotopic data show a spatiotemporally variable transition from isotopically heavy to isotopically light compositions. The latter are consistent with modern water on the plateau. When interpreted in the context of published paleoelevation estimates and independent geological information, the isotopic data indicate that elevation rapidly increased by 2-2.5 km from 20-17 Ma in the central Western Cordillera, and from 15-10 Ma in the southern Western Cordillera and Altiplano; these patterns are consistent with foundering of mantle lithosphere via Rayleigh-Taylor instability. The Eastern Cordillera was slowly elevated 1.5-2 km between 25 and 10 Ma, a rate consistent with crustal shortening as the dominant driver of surface uplift. The Ayacucho region attained modern elevation by ~22 Ma. The timing of orographic development across southern Peru is consistent with the early Miocene onset and middle Miocene intensification of hyperarid conditions along the central Andean Pacific coast. More... »

PAGES

4877

Identifiers

URI

http://scigraph.springernature.com/pub.10.1038/s41598-019-41257-3

DOI

http://dx.doi.org/10.1038/s41598-019-41257-3

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1112856899

PUBMED

https://www.ncbi.nlm.nih.gov/pubmed/30890755


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    "description": "Changes in Earth's surface elevation can be linked to the geodynamic processes that drive surface uplift, which in turn modulate regional climate patterns. We document hydrogen isotopic compositions of hydrated volcanic glasses and modern stream waters to determine late Cenozoic surface uplift across the Peruvian central Andes. Modern water isotopic compositions reproduce mean catchment elevations to a precision better than \u00b1500\u2009m (1\u03c3). Glass isotopic data show a spatiotemporally variable transition from isotopically heavy to isotopically light compositions. The latter are consistent with modern water on the plateau. When interpreted in the context of published paleoelevation estimates and independent geological information, the isotopic data indicate that elevation rapidly increased by 2-2.5\u2009km from 20-17\u2009Ma in the central Western Cordillera, and from 15-10\u2009Ma in the southern Western Cordillera and Altiplano; these patterns are consistent with foundering of mantle lithosphere via Rayleigh-Taylor instability. The Eastern Cordillera was slowly elevated 1.5-2\u2009km between 25 and 10\u2009Ma, a rate consistent with crustal shortening as the dominant driver of surface uplift. The Ayacucho region attained modern elevation by ~22\u2009Ma. The timing of orographic development across southern Peru is consistent with the early Miocene onset and middle Miocene intensification of hyperarid conditions along the central Andean Pacific coast.", 
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280 https://www.grid.ac/institutes/grid.266436.3 schema:alternateName University of Houston
281 schema:name Department of Earth and Atmospheric Sciences, University of Houston, Houston, Texas, USA
282 rdf:type schema:Organization
283 https://www.grid.ac/institutes/grid.89336.37 schema:alternateName The University of Texas at Austin
284 schema:name Department of Geological Sciences and Institute for Geophysics, University of Texas at Austin, 78712, Austin, TX, USA
285 rdf:type schema:Organization
 




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