Abstract

Glacial periods have been considered inhospitable environments that consisted of treeless vegetation at higher latitudes. The fossil record suggests many species survived the Last Glacial Maximum (LGM) within refugia, usually at lower latitudes. However, phylogeographic studies have given support to the existence of previously unknown high-latitude refugia not detected in the fossil record. Here we test the hypothesis that cold-tolerant trees of Patagonia survived cold periods in microclimatically favourable locales where hybridisation occurred between sister taxa. To study local presence through glacial periods in multiple refugia we used pollen records and genetic information (isozymes, microsatellites, and combined nuclear and chloroplast DNA sequences) of population pairs of Nothofagus antarctica and N. pumilio, that belong to the ancient subgenus Nothofagus which can potentially hybridize in nature, along their entire latitudinal range in Patagonia. Studied species share the N. dombeyi type pollen which was abundant >20% at the northern-most latitudinal bands (35-43°S), even during the LGM. Mid- and southern latitudinal records (44-55°S) yielded lower abundances of ~10% that increased after c. 15.0 cal. ka BP. Therefore, fossil pollen evidence suggests a long-lasting local presence of Nothofagus throughout glacial-interglacial cycles but mostly as small populations between 44-51°S. We found species-specific and shared genetic variants, the latter of which attained relatively high frequencies thus providing evidence of ancestral polymorphisms. Populations of each species were similarly diverse suggesting survival throughout the latitudinal range. Estimates of coalescent divergence times were broadly synchronous across latitudes suggesting that regional climates similarly affected populations and species that hybridized through climate cycles fostering local persistence.

Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.