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Rugged relief and climate promote isolation and divergence between two neotropical cold-associated birds
Fábio Raposo do Amaral1, Gregory Thom2, Matheus S Lima-Ribeiro3
1Departamento de Ecologia e Biologia Evolutiva, Universidade Federal de São Paulo, Rua Professor Artur Riedel, 275, Diadema, SP, 09972-270, Brazil.
Climate and topography drive diversification in tropical mountains. Warbling finches in the Atlantic Forest show distinct populations shaped by cyclical climate changes, leading to divergence and admixture.
Area of Science:
- Ecology and Evolutionary Biology
- Bioinformatics and Computational Biology
- Neotropical Biogeography
Background:
- Tropical mountain diversity is shaped by historical factors, including climate fluctuations and complex topography.
- Understanding diversification dynamics requires explicit spatio-temporal analyses of range shifts and their genomic impact.
- Previous studies highlight climate-topography interactions but lack detailed temporal frameworks.
Purpose of the Study:
- To investigate the evolutionary history of two warbling finch species (genus Microspingus) in the Montane Atlantic Forest.
- To test the role of climate and topography in shaping diversification patterns using niche modeling and population genomics.
- To elucidate historical range shifts and their consequences on genetic structure and gene flow.
Main Methods:
- Utilized niche modeling to predict species distributions over the last 800,000 years.
- Employed subgenomic population-level datasets to infer population structure and demographic history.
- Conducted demographic simulations to test hypotheses of isolation, population size stability, and gene flow.
Main Results:
- Identified three genetically distinct populations of warbling finches, congruent with geographic and phenotypic variation.
- Demographic simulations indicated asynchronous population isolation around 40,000 years ago, with stable sizes and past gene flow.
- Niche models revealed cyclical range expansions into lowlands during glacial periods and contractions to higher altitudes during interglacials, consistent with observed introgression.
Conclusions:
- Cyclical climate changes play a dual role: promoting divergence and persistence in mountains during warm periods, and expansion/admixture in lowlands during cold periods.
- The interplay between landscape complexity and climate is a crucial mechanism driving Neotropical montane biota evolution.
- Findings provide a spatio-temporal framework for understanding diversification in response to past climate dynamics.
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