Abstract

Historical processes of long-distance migration and ocean-wide expansion feature the global biogeographic pattern ofRhizophoraspecies. Throughout the Indian Ocean,Rhizophora stylosaandRhizophora mucronataseem to be a young phylogenetic group with an expansion ofR. mucronatatoward the Western Indian Ocean (WIO) driven by the South Equatorial Current (SEC). Nuclear microsatellites revealed genetic patterns and breaks; however, the estimation of propagule dispersal routes requires maternally inherited cytoplasmic markers. Here, we examine the phylogeography of 21R. mucronataprovenances across a >4,200 km coastal stretch in the WIO usingR. stylosaas an outgroup. Full-length chloroplast genome (164,474 bp) and nuclear ribosomal RNA cistron (8,033 bp) sequences were assembled. The boundaries, junction point, sequence orientation, and stretch between LSC/IRb/SSC/IRa/LSC showed no differences withR. stylosachloroplast genome. A total of 58 mutations inR. mucronataencompassing transitions/transversions, insertions-deletions, and mononucleotide repeats revealed three major haplogroups. Haplonetwork, Bayesian maximum likelihood (ML), and approximate Bayesian computation (ABC) analyses supported discrete historical migration events. An ancient haplogroup A in the Seychelles and eastern Madagascar was as different from other haplogroups as fromR. stylosa. A star-like haplonetwork referred as the recent range expansion of haplogroup B from northern Madagascar toward the African mainland coastline, including a single variant spanning >1,800 km across the Mozambique Channel area (MCA). Populations in the south of Delagoa Bight contained haplogroup C and was originated from a unique bottleneck dispersal event. Divergence estimates of pre- and post-Last Glacial Maximum (LGM) illustrated the recent emergence ofRhizophoramangroves in the WIO compared to other oceans. Connectivity patterns could be aligned with the directionality of major ocean currents. Madagascar and the Seychelles each harbored haplogroups A and B, albeit among spatially separated populations, explained from a different migration era. Likewise, the Aldabra Atoll harbored spatially distinct haplotypes. Nuclear ribosomal cistron (8,033 bp) variants corresponded to haplogroups and confirmed admixtures in the Seychelles and Aldabra. These findings shed new light on the origins and dispersal routes ofR. mucronatalineages that have shaped their contemporary populations in large regions of the WIO, which may be the important information for defining marine conservation units both at ocean scale and at the level of small islands.

Highlights

  • Mangroves represent characteristic intertidal forests along tropical, subtropical, and some warm-temperate coasts (Tomlinson, 2016)

  • Most genes occurred in a single copy, whereas eight protein-coding genes, eight transfer RNA (tRNA) genes, and the four ribosomal RNA (rRNA) genes in inverted repeat (IR) regions were duplicated

  • A previously mentioned null hypothesis of a single evolutionary unit was already rejected based on nuclear microsatellitebased connectivity patterns and genetic breaks (Triest et al, 2021b) such that a search for maternally inherited markers would give complementary information

Read more

Summary

Introduction

Mangroves represent characteristic intertidal forests along tropical, subtropical, and some warm-temperate coasts (Tomlinson, 2016). Sea-faring propagules as dispersal units allow mangrove tree species to be globally distributed and for connectivity between populations in different ocean basins (Van der Stocken et al, 2019a). Their origin and history over geological time offer an interesting multidisciplinary field involving continental drift, phylogenetic reconstruction, and molecular evolutionary genetics (Duke et al, 2002; Triest, 2008; Lo et al, 2014; Yan et al, 2016; Tomizawa et al, 2017; Takayama et al, 2021). Ocean currents and isolation by distance (IBD) are the significant predictors of the genetic structure in R. mangle from the Caribbean area though the historical factors or changes in ocean current patterns could interfere (Hodel et al, 2018)

Methods
Results
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call