A new early water frog (<i>Telmatobius</i>) from the Miocene of the Bolivian Altiplano

dc.contributor.authorRaúl O. Gómez
dc.contributor.authorTomás Ventura
dc.contributor.authorGuillermo F. Turazzini
dc.contributor.authorLaurent Marivaux
dc.contributor.authorRubén Andrade Flores
dc.contributor.authorAlberto Boscaini
dc.contributor.authorMarcos Fernández‐Monescillo
dc.contributor.authorBernardino Mamaní Quispe
dc.contributor.authorMercedes B. Prámparo
dc.contributor.authorSéverine Fauquette
dc.coverage.spatialBolivia
dc.date.accessioned2026-03-22T14:57:31Z
dc.date.available2026-03-22T14:57:31Z
dc.date.issued2024
dc.descriptionCitaciones: 4
dc.description.abstractAbstract We describe the new frog Telmatobius achachila sp. nov. from the late Middle to earliest Late Miocene of Achiri, based on a partial skeleton found at 3960 m above sealevel in the Bolivian Altiplano. This skeleton, attributed to a male adult, constitutes the first documented fossil record of the speciose living genus Telmatobius , endemic to the Andean Cordillera and the Altiplano. Phylogenetic analysis confirms the new species as being part of the crown group, and diverging both later than the T. verrucosus group and earlier than the T. bolivianus , T. marmoratus and T. macrostomus groups. Coupled with its accurate stratigraphic provenance and age, this phylogenetic position provides a relevant calibration point for timing the evolutionary history of these highland, mostly aquatic frogs. The skeleton of T. achachila indicates that several of the osteological peculiarities of extant Telmatobius were already acquired at c . 12 Ma, including some that might be linked to their aquatic lifestyle. Together with mixed montane–rainforest pollen vegetation uncovered in the same level, this fossil specimen further provides key data enabling a more accurate reconstruction of ancestral habitats and elevation ranges of Telmatobius , agreeing with the previously postulated conditions in which these water frogs might have first evolved. Ultimately, this discovery adds to the sparse evidence of a humid tropical Bolivian Altiplano just prior to: (1) the Late Miocene uplift pulse of the Central Altiplano; and (2) the drastic climate deterioration that occurred from Late Miocene time onward, leading to the harsh highland‐steppe environments reigning there today.
dc.identifier.doi10.1002/spp2.1543
dc.identifier.urihttps://doi.org/10.1002/spp2.1543
dc.identifier.urihttps://andeanlibrary.org/handle/123456789/49550
dc.language.isoen
dc.publisherWiley
dc.relation.ispartofPapers in Palaeontology
dc.sourceConsejo Nacional de Investigaciones Científicas y Técnicas
dc.subjectLate Miocene
dc.subjectBiology
dc.subjectEcology
dc.subjectRainforest
dc.subjectPaleontology
dc.subjectGenus
dc.titleA new early water frog (<i>Telmatobius</i>) from the Miocene of the Bolivian Altiplano
dc.typearticle

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