Cornaceae

The systematics of Cornaceae has been remarkably unsettled and controversial, and many genera have been added to it and removed from it over time. (One researcher called it a "dustbin".) Molecular phylogenetics have clarified the relatedness of some associated genera, and at least nine genera that were previously included in Cornaceae have been eliminated from the order Cornales entirely, but the circumscription of Cornaceae is still unclear. The Angiosperm Phylogeny Group usually defines Cornaceae as comprising the genera Cornus and Alangium as well as five genera now separated into the family Nyssaceae. However, many of these genera are sometimes split off into their own families (e.g. Alangiaceae), and the usage remains inconsistent.

Fossil record

The oldest fossil that can be related to Cornaceae is †Hironoia fusiformis, an extinct taxon collected from the Futaba Group sediments at Kamitikaba, Japan. Synapomorphies of the fruits of the fossil occur also in extant Cornaceae. The age of the sediments is of early Coniacian to early Santonian (about 88 Ma). Although the mosaic of characters in Hironoia precludes assignment to an extant genus, the fiber rather than sclereid composition of the fruit places it within the Nyssaceae-Mastixiaceae. Other possible Cornaceae from Cretaceous sediments include endocarps resembling Cornus from the Santonian-Campanian mesofossil assemblage of Åsen. In slightly younger Late Cretaceous sediments (Maastrichtian) four genera of fossil mastixioid fruits (Beckettia, Eomastixia, Mastixicarpum and Mastixiopsis) have been described from Germany.