4.0 Article

Evolutionary biogeography of the Revillagigedo Archipelago, Mexico

Journal

JOURNAL OF NATURAL HISTORY
Volume 57, Issue 9-12, Pages 685-709

Publisher

TAYLOR & FRANCIS LTD
DOI: 10.1080/00222933.2023.2203337

Keywords

biotic components; dispersal; endemism; island biogeography

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This article analyzes the biotic assembly of the Revillagigedo Archipelago, Mexico, using an evolutionary biogeographic framework. The study identifies the archipelago as an area where Nearctic and Neotropical biotic components overlap and suggests classifying it as a province or a district of the Pacific Lowlands province. The analysis also identifies two cenocrons that originated from the Baja California Peninsula and Pacific coast, respectively, and arrived at the archipelago during the Pliocene-Pleistocene.
The biotic assembly of the Revillagigedo Archipelago, Mexico, was analysed under an evolutionary biogeographic framework. We undertook a parsimony analysis of endemicity with progressive character elimination of 194 plant and animal species, which allowed us to identify the archipelago as a complex area or node where Nearctic and Neotropical biotic components overlap. We undertook a cladistic biogeographic analysis using the phylogenetic information of 42 taxon-area cladograms, from which one general-area cladogram was obtained: (Revillagigedo, (Sonoran, (Baja California, (Veracruzan, Pacific Lowlands)))). These results suggest that the Revillagigedo Archipelago may be classified as a province, although we prefer to keep it as a district of the Pacific Lowlands province. We identified two cenocrons (temporally integrated set of taxa) that can be dated to the Pliocene-Pleistocene: one Nearctic that dispersed from the Baja California Peninsula, and another Neotropical where the species dispersed from the Pacific coast to the islands. The geological information and the general-area cladograms allowed us to propose a geobiotic scenario for the archipelago where the islands are probably the result of volcanism associated with the oceanic Mathematician Ridge, and the arrival of the cenocrons to the archipelago may have occurred during the Pliocene-Pleistocene, after the islands were available for colonisation.

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