Laser microdissection of grapevine leaf phloem infected by stolbur reveals site‐specific gene responses associated to sucrose transport and metabolism

Bois Noir is an emergent disease of grapevine that has been associated to a phytoplasma belonging to the XII‐A stolbur group. In plants, phytoplasmas have been found mainly in phloem sieve elements, from where they spread moving through the pores of plates, accumulating especially in source leaves. To examine the expression of grapevine genes involved in sucrose transport and metabolism, phloem tissue, including sieve element/companion cell complexes and some parenchyma cells, was isolated from healthy and infected leaves by means of laser microdissection pressure catapulting (LMPC). Site‐specific expression analysis dramatically increased sensitivity, allowing us to identify specific process components almost completely masked in whole‐leaf analysis. Our findings showed decreased phloem loading through inhibition of sucrose transport and increased sucrose cleavage activity, which are metabolic changes strongly suggesting the establishment of a phytoplasma‐induced switch from carbohydrate source to sink. The analysis focused at the infection site also showed a differential regulation and specificity of two pathogenesis‐related thaumatin‐like genes (TL4 and TL5) of the PR‐5 family.     

The Rift Valley is a major barrier to dispersal of African clawed frogs (Xenopus) in Ethiopia

The Ethiopian highlands – home to striking species diversity and endemism – are bisected by the Rift Valley, a zone of tectonic divergence. Using molecular data we examined the evolutionary history of two co‐distributed species of African clawed frog (Xenopus clivii and X. largeni) that are endemic to this region. Our field collections substantially extend the known distribution of X. largeni, a species formerly known from highlands southeast of the Rift, but that also occurs to the northwest. In both species, analysis of mitochondrial DNA and 19 autosomal loci identifies significant population structure, suggests little or no recent migration across the Rift Valley, and provides divergence time estimates across the Rift of ～1–3.5 million years. These results indicate that the Ethiopian Rift Valley is a major obstacle to dispersal of highland‐adapted amphibians.