|Giraffe with calves - John Storr (Wikimedia Commons)|
Rise and fall of tragulidsThe most basal group is Tragulidae, represented by present day chevrotains or mouse deer. In the Early Miocene they were the most prevalent ruminants but were subsequently displaced by the pecorans. The principal difference was the evolution in pecorans of an additional forestomach, the omasum, and this seems to have given them the edge over tragulids.
Both tragulids and pecorans have synepitheliochorial placentation where binucleate trophoblast cells fuse with uterine epithelial cells at the fetal-maternal interface. However, tragulids lack the cotyledons typical of the placenta in pecorans.
Rise and fall of giraffoidsAmong pecorans, Giraffidae is basal to both Bovidae (cattle, sheep, antelopes) and Cervidae (deer). Looking at the equivalent fossil clades, Clauss and Rössner found that Giraffoidea were much more abundant in the later Early to Middle Miocene but then steadily declined to be supplanted by Bovoidea in Africa and by Bovoidea and Cervoidea in Eurasia. Why?
Based on extant species, the most striking difference between giraffids and other pecoran ruminants is their extremely long gestation - in excess of a year. Assuming this also was the case in fossil species, could that explain their decline? Clauss and Rössner argue that they were unable to develop a seasonal breeding pattern. This put them at a disadvantage compared to other pecorans with shorter gestation times such as bovids and cervids.
Perhaps in support of this narrative, fossil giraffoids occupied a much greater range of ecological niches and many were grazers. The giraffes grew a long neck and survived as browsers in a special niche. The okapi is highly adapted to its restricted forest habitat.
Placentation in the giraffe has recently been described (see previous post).