Understanding the spatio-temporal dynamics of Anadenanthera colubrina var. cebil in the biogeographical context of Neotropical seasonally dry forest

Abstract

Neotropical seasonally dry forest (dry forest) is a fragmented biome that occurs in regions with pronounced seasonal rainfall. There are several hypotheses about the evolution of the distribution of these forests concerning the influence of climatic changes during the Quaternary. Anadenanthera colubrina var. cebil is a native tree that is considered the most paradigmatic and ecologically specialized key species of dry forest. The present work aims to test whether the current disjunct distribution of A. colubrina var. cebil is a remnant of a formerly widespread range during the cold and dry phases of the Last Glacial Maximum (LGM). Here, we take an approach that combines chloroplast DNA, palaeodistribution modelling and fossil evidence to understand the spatial and temporal dynamics of the distribution of Anadenanthera colubrina var. cebil. Seven haplotypes were detected in the two non-coding regions of cpDNA analysed and their divergence was dated to the Neogene. Maps of climatic suitability for A. colubrina var. cebil throughout South America showed that the potential distribution of the species was extensive and fragmented from the lower Pleistocene to modern times. Data from the fossil record confirm the occurrence of A. colubrina var. cebil at the southern limit of the dry forest distribution in historical times before the Quaternary. We found that climate change during the Pleistocene cannot be considered the main cause of molecular divergence of A. colubrina var. cebil haplotypes. We also found that A. colubrina var. cebil already had a widespread and fragmented distribution in South America during the Pleistocene, and that A. colubrina var. cebil was already present in northern Argentina in pre-Pleistocene.