of food crops) or deliberately (associated with the ingestion of herbal infusions for the treatment of certain ailments). The seeds contained high concentrations of pyrrolizidine alkaloids, identified mainly as the N-oxide of heliotrine (74%), and one or two other compounds similar in character to lasiocarpine. Taxonomy Taxonomic revision supported through molecular phylogenetics led to the recognition of Euploca as genus separate from Heliotropium. In contrast, the genus Tournefortia was included in Heliotropium in a 2016 revision. Within Heliotropium, there are four major clades: Heliotropium sect. Heliothamnus Old World Heliotropium clade Heliotropium sect. Cochranea Tournefortia clade, comprising Tournefortia sect. Tournefortia and all remaining New World Heliotropium species Origins of diversification Three of the four major clades within Heliotropium have their centers of diversity in South America. The origins of the remaining Old World Heliotropium clade can be traced back to a single colonization event from the New World. ITS1 data shows there is a single characteristic long deletion between positions 61 and 111 in the genome of the Old World species, which defines the Old World Heliotropium species and separates them from their New World counterparts. Researchers concluded this is a single autapomorphic character from a single deletion event in the past. This most reasonably explains how the whole group may have come to share this characteristic deletion when comparing the genomes of Old World and New World Heliotropium. The most likely driver of Heliotropium diversification across the three New World clades is early Andean uplift. Researchers identified three independent diversification events in the phylogeny of Andean Heliotropium, whose timings correspond to late Miocene Andean uplift as well as the development of arid environments in South America during the Pliocene. These three diversification events each mark the separation of the Heliothamnus, Cochranea, and Tournefortia clades from the rest of Heliotropium. Heliothamnus diversification is estimated to have taken place in the late Miocene. The age of Heliothamnus suggest that its diversification could have been triggered directly by the uplift of the Andes, something that would have promoted speciation in inner-Andean valleys and the Andean scrub. The majority of endemic Heliothamnus taxa in the region are restricted to these sorts of environments, further supporting this theory as the current leading theory explaining Heliothamnus diversification. Before the main rise of the Andes, Cochranea and Tournefortia coinhabited the Andean region at the same time and significant speciation had not yet occurred. Once the Andes began