TL;DR: A parsimony analysis of 101 morphological characters of the skull, auditory area and dentary tested on 23 taxa confirms the paraphyly of the Cetotheriidae as traditionally defined and suggests that six of the studied fossil baleen mysticetes constitute a clade.
Abstract: Piscobalaena nana Pilleri & Siber, 1989 is a small fossil baleen-bearing mysticete from the early Pliocene of the Pisco Formation, Peru. The holotype of this species is an incomplete skull (lacking the vertex) with associated tympanics. The description of five remarkably preserved new specimens of this taxon (three of them associated with partial post-cranial skeletons) provides the opportunity to understand the intraspecific variation within one single fossil mysticete species. These specimens constitute a partial ontogenetic series including one sub-adult animal, three adults and one old individual. Piscobalaena nana is compared to Nannocetus eremus Kellogg, 1929, Cetotherium rathkei Brandt, 1843, Herpetocetus sendaicus (Hatai, Hayasaka & Masuda, 1963) and Metopocetus durinasus Cope, 1896, which are similar in morphology and age to the Peruvian species. A parsimony analysis of 101 morphological characters of the skull, auditory area and dentary tested on 23 taxa confirms the paraphyly of the Cetotheriidae as traditionally defined. It also suggests that six (Piscobalaena, Herpetocetus, Metopocetus, Cetotherium, Nannocetus, Mixocetus) of the 12 studied fossil baleen mysticetes constitute a clade: the Cetotheriidae s.s. Its monophyly is supported by 10 characters of the skull (e.g., ascending processes of the maxillae contacting medially or very approximated at apex; lateral edges of nasals strongly convergent posteriorly; supraorbital process of the frontal anteriorly oriented), and five characters of the auditory area (e.g., anterior edge of facial foramen on the internal acoustic meatus is notched [slightly to deeply] for the passage of the greater petrosal nerve). The Cetotheriidae share with the Balaenopteridae the presence of an interdigitation of the rostral and cranial bones such as the posteriorly elongated ascending process of the maxilla. This condition reinforces the cranial architecture and could suggest a similar engulfment way of feeding as observed in the Balaenopteridae.
TL;DR: A cladistic analysis that includes representatives of all recent genera of mysticetes and several fossil species that were previously referred to the family Cetotheriidae, with tooth-bearing mysticete and an archaeocete as an outgroup forms the base of a revised classification of Mysticeti.
TL;DR: The phylogenetic analysis confirmed that the pygmy right whale cannot be considered a member of Cetotheriidae and revealed that the family originated in the Pacific basin during the Burdigalian and subsequently underwent a sequence of dispersal and vicariance events that allowed its members to enter other ocean basins.
Abstract: Herentalia nigra gen. et sp. nov. is described and compared to other mysticetes. It belongs to Cetotheriidae s.s. and represents one of the best-preserved cetotheriid skulls from the southern border of the North Sea. A comprehensive phylogenetic analysis revealed that it is closely related to Nannocetus and to a Japanese Herpetocetus, suggesting that it belongs to the subfamily Herpetocetinae. The phylogenetic analysis performed tests the recent hypothesis that Caperea marginata belongs to Cetotheriidae. However the present results confirm that the pygmy right whale cannot be considered a member of Cetotheriidae. The phylogenetic analysis was used as the basis for a cladistic palaeobiogeographical analysis of Cetotheriidae that revealed that the family originated in the Pacific basin during the Burdigalian and subsequently underwent a sequence of dispersal and vicariance events that allowed its members to enter other ocean basins. The evolution of Cetotheriidae diversity was punctuated by two distinct pha...
TL;DR: Two fossil baleen whale dentaries from the Upper Miocene Santa Margarita Sandstone of Central California preserve several distinct features similar to the enigmatic herpetocetine whale Herpetocetus, which suggests that the mandibular morphology of fossil mysticetes may be more homoplastic than previously assumed.
Abstract: Two fossil baleen whale (Mysticeti) dentaries from the Upper Miocene (10–12 Ma) Santa Margarita Sandstone of Central California preserve several distinct features similar to the enigmatic herpetocetine whale Herpetocetus. These features include an elongate coronoid process, a mandibular condyle with a planar articular surface, and a posteriorly extended angular process. The dentary is unknown for several Herpetocetinae (and the more inclusive clade Cetotheriidae), including the coeval Nannocetus eremus. This occurrence would extend the known record of Herpetocetus by 6 Ma. Given the currently poor knowledge of Pacific Cetotheriidae during the Miocene, these specimens are identified to the subfamily Herpetocetinae, despite the similarity of these specimens to Herpetocetus. As the morphology of the supposedly distinctive lectotype dentary of Herpetocetus scaldiensis (the type species of Herpetocetus) may not be unique to Herpetocetus, this study suggests that the mandibular morphology of fossil mysticetes may be more homoplastic (or conservative) than previously assumed. Mysticete taxonomy should employ autapomorphic characters beyond the morphology of the dentary alone.