Sunda–Sahul floristic exchange and pathways into the Southwest Pacific: New insights from wet tropical forest trees

Author:

Holzmeyer Laura1ORCID,Hauenschild Frank12ORCID,Muellner‐Riehl Alexandra N.13ORCID

Affiliation:

1. Department of Molecular Evolution and Plant Systematics & Herbarium (LZ) Institute of Biology, Leipzig University D‐04103 Leipzig Germany

2. Centre for Teacher Training and School Research Leipzig University D‐04317 Leipzig Germany

3. German Centre for Integrative Biodiversity Research (iDiv) Halle‐Jena‐Leipzig D‐04103 Leipzig Germany

Abstract

AbstractAimRecent investigations on the floristic exchange between Southeast Asia and Australia have shown a clear dispersal directionality bias (West to East) of wet‐adapted plant taxa. However, dispersal routes and directions of wet forest taxa into the South Pacific remain insufficiently known. We here aimed to establish the most likely routes and directions of plant dispersal into the Southwest Pacific islands.LocationSoutheast Asia, East Asia, Australia, Southwest Pacific.TaxonDysoxylum s.l. (Meliaceae). This includes Dysoxylum s.s., Didymocheton, Epicharis, Goniocheton, Pseudocarapa, and Prasoxylon.MethodWe sampled 75% of the species diversity in Dysoxylum s.l., covering the entire distribution range, all genera and major lineages. Phylogenetic relationships of 149 accessions were reconstructed using Bayesian Evolutionary Analysis and two internal constraints. The dispersal–extinction–cladogenesis variant, founder‐event speciation (DEC+J), was used for reconstructing the biogeographic history, and 100 Biogeographical Stochastic Mappings were simulated.ResultsDysoxylum s.l. originated and firstly diversified in the western part of its current distribution range (including Indochina) during the Miocene to Pliocene, followed by an overall eastern range expansion towards Malesia, Australia and the Southwest Pacific in the Pliocene.Main ConclusionsThe south‐eastward expansion of lineages into Wallacea and Australia is in temporal agreement with the convergence of the Asian and Australian tectonic plates since the Miocene. Long‐distance dispersal is the main mechanism that led to the current distribution. Two dispersal pathways into the Southwest Pacific are identified, (1) through New Guinea and the Solomon Islands to Fiji, and (2) from New Zealand to Fiji. For both routes, Fiji was an important secondary source area for dispersal into the Southwest Pacific.

Funder

Bundesministerium für Bildung und Forschung

Deutsche Forschungsgemeinschaft

Universität Leipzig

Publisher

Wiley

Subject

Ecology,Ecology, Evolution, Behavior and Systematics

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