In this paper, we compare the populations of the Lusitanian toadfish Halobatrachus didactylus along the Portuguese shore, using a putative fragment of the mitochondrial control region and the first intron of the S7 ribosomal protein gene. This demersal species ranges from the tropical West African coast to the Iberian Peninsula and the Mediterranean, having its northern limit in the Tagus River. For the putative control region, a single haplotype occurs in all fish from Tagus and Sado (the location immediately to the south) with a clear increase in diversity to the South, peaking at Algarve (south Portugal). The data seem to point to a very recent Holocenic colonization of Tagus and Sado from the South (possibly Algarve). We suggest that even small oscillations in sea surface temperature (SST) may cause local extinctions and subsequent recolonizations in populations of thermophilic fish that are at the cold limit of their distributions.
IntroductionMany phylogeographic studies of marine organisms with larval dispersal have detected little structure along stretches of coastlines that span hundreds of kilometres or more (e.g. . This is assumed to result from the presence of planktonic eggs and/or larvae capable of dispersing over distances of kilometres or hundreds of kilometres per generation (however, see Ayre et al. 2009). Most studies assume that the Pleistocene and specially the Last Glacial Maximum (LGM) were critical times when populations were absent from the frozen north and suffered severe bottlenecks in their refugial habitats. In temperate areas like the west coast of Portugal and most of the south-west European shore, however, the conditions seem to have been more complicated. Although sea surface temperatures (SSTs) during the LGM along the coast of Portugal were not significantly different from what they are today (Abreu et al. 2003), several cold episodes towards the end of the Last glaciation considerably lowered mean summer SST (as much as 5°C).During the Holocene the oscillations in SSTs continued to be a salient feature of this geographic area, although their amplitudes were smaller. Some cold pulses such as the 8,400 years ago cold event and the Little Ice Age (LIA) caused temperature drops of one or a few degrees (Casper 2010) and may have affected the distributions of fish populations. A temperature anomaly need not to last very long to extirpate a population, it suffices that the population does not breed during a period that surpasses the lifespan of all its members. So, even short pulses that last for a few fish generations can cause a very substantial local effect. Even in present conditions small interannual oscillations can substantially affect the fish fauna, at least for the populations that are at or near the higher latitude limits of the Communicated by M. I. Taylor.