Abstract

BackgroundThe Chilean shoreline, a nearly strait line of coast expanding across 35 latitudinal degrees, represents an interesting region to assess historical processes using phylogeographic analyses. Stretching along the temperate section of the East Pacific margin, the region is characterized by intense geologic activity and has experienced drastic geomorphological transformations linked to eustatic and isostatic changes during the Quaternary. In this study, we used two molecular markers to evaluate the existence of phylogeographic discontinuities and detect the genetic footprints of Pleistocene glaciations among Patagonian populations of Mazzaella laminarioides, a low-dispersal benthic intertidal red seaweed that inhabits along ~3,700 km of the Chilean coastal rocky shore.ResultsThree main genetic lineages were found within M. laminarioides. They are distributed along the Chilean coast in strict parapatry. The deep divergence among lineages suggests that they could be considered putative genetic sibling species. Unexpectedly, genetic breaks were not strictly concordant with the biogeographic breaks described in the region. A Northern lineage was restricted to a broad transition zone located between 30°S and 33°S and showed signals of a recent bottleneck. The reduction of population size could be related to warm events linked to El Niño Southern Oscillation, which is known to cause massive seaweed mortality in this region. To the south, we propose that transient habitat discontinuities driven by episodic tectonic uplifting of the shoreline around the Arauco region (37°S-38°S); one of the most active forearc-basins in the South East Pacific; could be at the origin of the Central/South genetic break. The large beaches, located around 38°S, are likely to contribute to the lineages’ integrity by limiting present gene flow. Finally, the Southern lineage, occupies an area affected by ice-cover during the last glaciations. Phylogeny suggested it is a derived clade and demographic analyses showed the lineage has a typical signature of postglacial recolonization from a northern glacial refugium area.ConclusionsEven if environmental adaptation could have strengthened divergence among lineages in M. laminarioides, low dispersal capacity and small population size are sufficient to generate phylogeographic discontinuities determined by genetic drift alone. Interestingly, our results confirm that seaweed population connectivity over large geographic scales does not rely only on dispersal capacity but also seem to depend highly on substratum availability and population density of the receiving locality.

Highlights

  • The Chilean shoreline, a nearly strait line of coast expanding across 35 latitudinal degrees, represents an interesting region to assess historical processes using phylogeographic analyses

  • We considered two possible scenarios of post-Last Glacial Maximum (LGM) recolonization that would lead to distinct genetic footprints: first the recolonization of the Magellanic Province (MP) province from a single refugia located northern to 42°S (Chiloé Island) and second, a recolonization from two refuge areas; Chiloé Island and a remnant population located in Tierra del Fuego (56°S)

  • Within the 233 individuals sequenced for the chloroplast marker Large subunit of the RUBISCO (rbcL) (922 bp), we found 19 polymorphic sites and 10 haplotypes [GenBank: JQ408398-JQ408407]

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Summary

Introduction

The Chilean shoreline, a nearly strait line of coast expanding across 35 latitudinal degrees, represents an interesting region to assess historical processes using phylogeographic analyses. Numerous studies have revealed deep genetic separation for coastal marine taxa that concur with well-known Transition Zones such as: the Isthmus of Panama [1], the south eastern Australian coast [2], the strait of Gibraltar [3], the Southern Florida Transition Zone [4] and the California Transition Zone [5,6]. These transition zones have been related to historical partitions; which are linked to eustatic, tectonic or climatic vicariant factors associated with late Pleistocene glacial cycles [4,7]. Species dispersal potential and effective population size appear to be strong determinants of the phylogeographic discontinuities magnitude; whereas any restriction to gene flow, such as biogeographic breaks, may influence the localization of the break

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