Abstract
AbstractCalluna vulgaris (Ericaceae) is the most widespread and prevalent woody species of the European dry heathland, from the African side of the Strait of Gibraltar to northern Europe. However, previous biogeographic analyses of this species have ignored the western Mediterranean region, despite its preponderant role as a major glacial refugium for European biota. Here, we explore the existence of further Pleistocene glacial refugia for C. vulgaris in the Iberian Peninsula and the Strait of Gibraltar area and provide new insights into the post-glacial colonization of Europe by this emblematic heathland species. We carried out phylogeographical analyses of C. vulgaris samples from 44 locations using four plastid markers (matK, trnH-psbA, trnL-F and rpl16). We built palaeodistribution models using MAXENT to identify possible refugia for C. vulgaris during the mid-Pliocene, Last Interglacial (LIG), Last Glacial Maximum (LGM) and mid-Holocene. Our results identified a genetic lineage exclusive to the Strait of Gibraltar area s.l. (south-western Iberian Peninsula and north-western tip of Africa) as the most probable close to the clade of origin of the species. This lineage also had more private haplotypes than more recent, Eurosiberian clades. The obtained data highlighted two main refugia for C. vulgaris during the LGM, one around the Strait of Gibraltar and another in the north-western Iberian Peninsula. The Strait of Gibraltar area is a major centre of origin or glacial refugium for the heather C. vulgaris. However, the north-western Iberian Peninsula seems to have acted as a secondary glacial refugium for the more recent, Eurosiberian lineage of this species. This study stresses the importance of the Strait of Gibraltar area in the biogeographic history and conservation of the heather and, by extension, the European heathland habitat.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.