Pingel et al.(1) combined δD analyses of volcanic glass from a few new samples with
selected published paleoaltimetry proxy data and putative field relationships in the Puna …

We appreciate Carrapa et al.'s (1) interest in our work (2) and welcome the opportunity to
address their comments on the deformation and surface-uplift history of the central Puna …

Compared to the thin‐skinned Subandean foreland fold‐and‐thrust belt of northern
Argentina and Bolivia, the tectonically active morphotectonic province of the Santa Bárbara …

Lithospheric foundering is an important mechanism of crustal deformation and recycling,
basin subsidence, and surface uplift in orogenic systems. The Arizaro Basin, in the Puna …

Hydrated volcanic glass δD (δDg) values of pure tuffs have been used to reconstruct
paleoprecipitation δD in paleoelevation and paleoclimate studies. These hydrated glasses …

We present a study in the southern Puna (26° 30′–27° 30′ S), aiming to explore the late
Cenozoic evolution of the deformation and the stress field during its uplift. Through U‐Pb …

Frogs (Anura) are major components of tetrapod communities in the Neotropics and,
according to divergence-time estimates, were already diverse in early Palaeogene times …