Premium
Phylogeography and biogeography of the lower C entral A merican N eotropics: diversification between two continents and between two seas
Author(s) -
Bagley Justin C.,
Johnson Jerald B.
Publication year - 2014
Publication title -
biological reviews
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 4.993
H-Index - 165
eISSN - 1469-185X
pISSN - 1464-7931
DOI - 10.1111/brv.12076
Subject(s) - phylogeography , diversification (marketing strategy) , biogeography , biology , genetics , ecology , phylogenetics , gene , marketing , business
Lower C entral A merica ( LCA ) provides a geologically complex and dynamic, richly biodiverse model for studying the recent assembly and diversification of a N eotropical biota. Here, we review the growing literature of LCA phylogeography studies and their contribution to understanding the origins, assembly, and diversification of the LCA biota against the backdrop of regional geologic and climatic history, and previous biogeographical inquiry. Studies to date reveal that phylogeographical signal within taxa of differing distributions reflects a diversity of patterns and processes rivalling the complexities of LCA landscapes themselves. Even so, phylogeography is providing novel insights into regional diversification (e.g. cryptic lineage divergences), and general evolutionary patterns are emerging. Congruent multi‐taxon phylogeographic breaks are found across the N icaraguan depression, C horotega volcanic front, western and central P anama, and the D arién isthmus, indicating that a potentially shared history of responses to regional‐scale (e.g. geological) processes has shaped the genetic diversity of LCA communities. By contrast, other species show unique demographic histories in response to overriding historical events, including no phylogeographic structure at all. These low‐structure or incongruent patterns provide some evidence for a role of local, ecological factors (e.g. long‐distance dispersal and gene flow in plants and bats) in shaping LCA communities. Temporally, comparative phylogeographical structuring reflects P liocene– P leistocene dispersal and vicariance events consistent with the timeline of emergence of the LCA isthmus and its major physiographic features, e.g. cordilleras. We emphasise the need to improve biogeographic inferences in LCA through in‐depth comparative phylogeography projects capitalising on the latest statistical phylogeographical methods. While meeting the challenges of reconstructing the biogeographical history of this complex region, phylogeographers should also take up the critical service to society of applying their work to the conservation of its fascinating biodiversity.