TL;DR: A phylogenetic analysis including 51 taxa supports a monophyletic group comprising most Neogene and modern whales, with Tranatocetidae being possibly closer related to Balaenopteridae (rorquals) than to Cetotheriidae.
Abstract: Miocene baleen whales were highly diverse and included tens of genera. However, their taxonomy and phylogeny, as well as relationships with living whales, are still a subject of controversy. Here, “Mesocetus” argillarius, a poorly known specimen from Denmark, is redescribed with a focus on the cranial anatomy. It was found to represent not only a new genus, Tranatocetus gen. nov., but also a new family; Tranatocetidae. The whales of this family have the rostral bones either overriding or dividing the frontals; the rostral bones are contacting the parietals and nasals dividing the maxillae on the vertex; the occipital shield is dorsoventrally bent. The tympanic bulla is particularly characteristic of this family featuring a short, narrow anterior portion with a rounded or squared anterior end and a wider and higher posterior portion that is swollen in the posteroventral area. A phylogenetic analysis including 51 taxa supports a monophyletic group comprising most Neogene and modern whales, with Tranatocetidae being possibly closer related to Balaenopteridae (rorquals) than to Cetotheriidae. Tranatocetidae exhibit a charahteristic bulla shape. In fact, all Neogene and modern mysticete families examined have a unique shape of the tympanic bulla that is diagnostic at family-level. Inclusion of problematic taxa like Tranatocetus argillarius in phylogenies brings new understanding of the distribution and diagnostic value of character traits. This underlines the need for re-examination of earlier described specimens in the light of the wealth of new information published in later years.
TL;DR: It would appear from forms such as Diochotichus vanbenedeni and Prosqualodon australis that some sort of echolocation was in existence as early as in the Lower Miocene.
Abstract: A detailed description is given of the lower jaw and cervical vertebrae of an almost complete skeleton of a baleen whale, Mesocetus argillarius sp.n., from the Gram Formation of Jutland, Denmark. After comparison with other baleen whales it is concluded that the Miocene species of Mesocetus are closely related to recent balaenopterids, although not their direct ancestors. The relationship to recent balaenids is more remote. The voluminous mandibular canal found in various Mesocetus species, in Pelocetus mirabilis and in some Arahaeoceti e.g. Zygorhiza kochi and Dorudon osiris, may be one of the prerequisites for the development during whale phylogeny of the echolocation system found in a highly refined form in modern Odontoceti. Asymmetry in the cranial skeleton characteristic of modern odontocetes seems to be closely linked with the echolocation system and when detected in fossil forms, it may indicate that this system was already established there. Accordingly, it would appear from forms such as Diochotichus vanbenedeni and Prosqualodon australis that some sort of echolocation was in existence as early as in the Lower Miocene.