Genetic discontinuities in a dominant mangrove Rhizophora apiculata (Rhizophoraceae) in the Indo-Malesian region
Guo, Zixiao, Huang, Yelin, Chen, Yongmei, Duke, Norman C., Zhong, Cairong, and Shi, Sugua (2016) Genetic discontinuities in a dominant mangrove Rhizophora apiculata (Rhizophoraceae) in the Indo-Malesian region. Journal of Biogeography, 43. pp. 1856-1868.
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Abstract
Aim: Population genomics data were used to determine the genetic diversity, genetic divergence and genetic structure of the mangrove, Rhizophora apiculata, across its distributional range and to re-assess the evolutionary processes that shaped its current distribution.
Location: The Indo-Malesian region section of the Indo-West Pacific region.
Methods: Next-generation sequencing technology was used to sequence 81 nuclear loci from a pooled DNA sample of 31–44 individuals of Rhizophora apiculata from 11 populations. Five nuclear loci from six to eight individuals from 18 populations were sequenced using conventional Sanger sequencing technology to validate the results.
Results: Genetic diversity at the population level was low (π and θ were < 1.0 × 10−3 in most of the populations), but relatively high at the species level (π = 2.419 × 10−3 and θ = 1.362 × 10−3). The populations of R. apiculata in the Indo-Malesian region were genetically differentiated and grouped into three clusters: east Indian Ocean (EIO), South China Sea (SCS) and Australasia (AUA). Based on the genetic distance matrices, two genetic discontinuities were observed, and they correspond to the Malay Peninsula land barrier and the Wallacea zone. The admixture observed in populations from the Malacca Strait was attributed to asymmetric gene flow through the strait, which was simulated by the isolation-with-migration (IM) model.
Main conclusion: Both the Sunda shelf barrier and ocean currents in Wallacea contributed to the observed genetic discontinuity, which separated R. apiculata into three clusters (SCS, EIO and AUA). The cycle between extinction and recolonization in the SCS in response to Pleistocene sea level fluctuations reduced the genetic diversity within populations. The repeated opening and closing of the gene flow corridors, such as the Malacca Strait, may have blurred the genetic discontinuities to an extent and introduced an admixture into populations in boundary areas.