Munroa argentina, a Grass of the South American Transition Zone, Survived the Andean Uplift, Aridification and Glaciations of the Quaternary.

The South American Transition Zone (SATZ) is a biogeographic area in which not only orogeny (Andes uplift) and climate events (aridification) since the mid-Miocene, but also Quaternary glaciation cycles had an important impact on the evolutionary history of the local flora. To study this effect, we...

Full description

Bibliographic Details
Main Authors: Leonardo D Amarilla, Ana M Anton, Jorge O Chiapella, María M Manifesto, Diego F Angulo, Victoria Sosa
Format: Article
Language:English
Published: Public Library of Science (PLoS) 2015-01-01
Series:PLoS ONE
Online Access:http://europepmc.org/articles/PMC4484249?pdf=render
id doaj-34ecdbfda3804621b211a7b12e0b9242
record_format Article
spelling doaj-34ecdbfda3804621b211a7b12e0b92422020-11-24T21:10:45ZengPublic Library of Science (PLoS)PLoS ONE1932-62032015-01-01106e012855910.1371/journal.pone.0128559Munroa argentina, a Grass of the South American Transition Zone, Survived the Andean Uplift, Aridification and Glaciations of the Quaternary.Leonardo D AmarillaAna M AntonJorge O ChiapellaMaría M ManifestoDiego F AnguloVictoria SosaThe South American Transition Zone (SATZ) is a biogeographic area in which not only orogeny (Andes uplift) and climate events (aridification) since the mid-Miocene, but also Quaternary glaciation cycles had an important impact on the evolutionary history of the local flora. To study this effect, we selected Munroa argentina, an annual grass distributed in the biogeographic provinces of Puna, Prepuna and Monte. We collected 152 individuals from 20 localities throughout the species' range, ran genetic and demographic analyses, and applied ecological niche modeling. Phylogenetic and population genetic analyses based on cpDNA and AFLP data identified three phylogroups that correspond to the previously identified subregions within the SATZ. Molecular dating suggests that M. argentina has inhabited the SATZ since approximately 3.4 (4.2-1.2) Ma and paleomodels predict suitable climate in these areas during the Interglacial period and the Last Glacial Maximum. We conclude that the current distribution of M. argentina resulted from the fragmentation of its once continuous range and that climate oscillations promoted ecological differences that favored isolation by creating habitat discontinuity.http://europepmc.org/articles/PMC4484249?pdf=render
collection DOAJ
language English
format Article
sources DOAJ
author Leonardo D Amarilla
Ana M Anton
Jorge O Chiapella
María M Manifesto
Diego F Angulo
Victoria Sosa
spellingShingle Leonardo D Amarilla
Ana M Anton
Jorge O Chiapella
María M Manifesto
Diego F Angulo
Victoria Sosa
Munroa argentina, a Grass of the South American Transition Zone, Survived the Andean Uplift, Aridification and Glaciations of the Quaternary.
PLoS ONE
author_facet Leonardo D Amarilla
Ana M Anton
Jorge O Chiapella
María M Manifesto
Diego F Angulo
Victoria Sosa
author_sort Leonardo D Amarilla
title Munroa argentina, a Grass of the South American Transition Zone, Survived the Andean Uplift, Aridification and Glaciations of the Quaternary.
title_short Munroa argentina, a Grass of the South American Transition Zone, Survived the Andean Uplift, Aridification and Glaciations of the Quaternary.
title_full Munroa argentina, a Grass of the South American Transition Zone, Survived the Andean Uplift, Aridification and Glaciations of the Quaternary.
title_fullStr Munroa argentina, a Grass of the South American Transition Zone, Survived the Andean Uplift, Aridification and Glaciations of the Quaternary.
title_full_unstemmed Munroa argentina, a Grass of the South American Transition Zone, Survived the Andean Uplift, Aridification and Glaciations of the Quaternary.
title_sort munroa argentina, a grass of the south american transition zone, survived the andean uplift, aridification and glaciations of the quaternary.
publisher Public Library of Science (PLoS)
series PLoS ONE
issn 1932-6203
publishDate 2015-01-01
description The South American Transition Zone (SATZ) is a biogeographic area in which not only orogeny (Andes uplift) and climate events (aridification) since the mid-Miocene, but also Quaternary glaciation cycles had an important impact on the evolutionary history of the local flora. To study this effect, we selected Munroa argentina, an annual grass distributed in the biogeographic provinces of Puna, Prepuna and Monte. We collected 152 individuals from 20 localities throughout the species' range, ran genetic and demographic analyses, and applied ecological niche modeling. Phylogenetic and population genetic analyses based on cpDNA and AFLP data identified three phylogroups that correspond to the previously identified subregions within the SATZ. Molecular dating suggests that M. argentina has inhabited the SATZ since approximately 3.4 (4.2-1.2) Ma and paleomodels predict suitable climate in these areas during the Interglacial period and the Last Glacial Maximum. We conclude that the current distribution of M. argentina resulted from the fragmentation of its once continuous range and that climate oscillations promoted ecological differences that favored isolation by creating habitat discontinuity.
url http://europepmc.org/articles/PMC4484249?pdf=render
work_keys_str_mv AT leonardodamarilla munroaargentinaagrassofthesouthamericantransitionzonesurvivedtheandeanupliftaridificationandglaciationsofthequaternary
AT anamanton munroaargentinaagrassofthesouthamericantransitionzonesurvivedtheandeanupliftaridificationandglaciationsofthequaternary
AT jorgeochiapella munroaargentinaagrassofthesouthamericantransitionzonesurvivedtheandeanupliftaridificationandglaciationsofthequaternary
AT mariammanifesto munroaargentinaagrassofthesouthamericantransitionzonesurvivedtheandeanupliftaridificationandglaciationsofthequaternary
AT diegofangulo munroaargentinaagrassofthesouthamericantransitionzonesurvivedtheandeanupliftaridificationandglaciationsofthequaternary
AT victoriasosa munroaargentinaagrassofthesouthamericantransitionzonesurvivedtheandeanupliftaridificationandglaciationsofthequaternary
_version_ 1716755395366617088