Development of anthocyanin markers: gene mapping, genomic analysis and genetic diversity studies in Ipomoea species.

The anthocyanins are pigments responsible for a wide range of colours in plants, from blue, red and purple, play essential biological roles as well as their genes are evolutionarily conserved. Purple sweet potatoes have anthocyanins as the predominant colour, even though they are present in orange roots masked by carotenoids. Several studies have focused on molecular aspects of anthocyanin genes, mainly in wild Ipomoea species, although the structure and segregation analysis of those genes in sweet potato hexaploid species are still unknown. Based on an "exon-primed intron-crossing" (EPIC) approach, fourteen pairs of primers were designed, on five structural anthocyanin genes as candidates. The strategy exploits the Intron Length Polymorphism (ILP) from Candidate Genes (CG), resulting in 93% of successful markers giving scorable and reproducible alleles. The results allowed to define partial structure and sequence of the introns and exons from the selected CG, and to determine patterns of sequence variation. The evaluation of marker dosage and allelic segregations in an Ipomoea batatas (L.) Lam mapping population identified several alleles for linkage analysis. The study validated the utility of ILP-CG markers for genetic diversity and conservation applicability and a successful amplification gradient across wild Ipomoea species validated their transferability.

Munroa argentina, a Grass of the South American Transition Zone, Survived the Andean Uplift, Aridification and Glaciations of the Quaternary.

The South American Transition Zone (SATZ) is a biogeographic area in which not only orogeny (Andes uplift) and climate events (aridification) since the mid-Miocene, but also Quaternary glaciation cycles had an important impact on the evolutionary history of the local flora. To study this effect, we selected Munroa argentina, an annual grass distributed in the biogeographic provinces of Puna, Prepuna and Monte. We collected 152 individuals from 20 localities throughout the species' range, ran genetic and demographic analyses, and applied ecological niche modeling. Phylogenetic and population genetic analyses based on cpDNA and AFLP data identified three phylogroups that correspond to the previously identified subregions within the SATZ. Molecular dating suggests that M. argentina has inhabited the SATZ since approximately 3.4 (4.2-1.2) Ma and paleomodels predict suitable climate in these areas during the Interglacial period and the Last Glacial Maximum. We conclude that the current distribution of M. argentina resulted from the fragmentation of its once continuous range and that climate oscillations promoted ecological differences that favored isolation by creating habitat discontinuity.