Africanacetus

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Phylum:Chordata
Class:Mammalia
Infraorder:Cetacea
Africanacetus
Temporal range: Late Miocene-Early Pliocene
~5.3–3.6 Ma
Scientific classification Edit this classification
Kingdom: Animalia
Phylum: Chordata
Class: Mammalia
Order: Artiodactyla
Infraorder: Cetacea
Family: Ziphiidae
Genus: Africanacetus
Bianucci et al. 2007
Species
  • A. ceratopsis Bianucci et al. 2007 (type)
  • A. gracilis Ichishima et al. 2017

Africanacetus is an extinct genus of ziphiid cetacean known from skulls found in seafloor sediments of Late Miocene to Early Pliocene age off the coasts of South Africa (Banzare Bank), Brazil (São Paulo Ridge), and the Indian Ocean.[1][2]

Africanacetus is placed within the family Ziphiidae and subfamily Hyperoodontinae. It was first described in 2007 from Neogene deposits off South Africa, with Africanacetus ceratopsis as the type species.[3] Two species are currently recognized, A. ceratopsis and A. gracilis, which differ in cranial proportions, with A. gracilis possessing a more slender skull than the more robust A. ceratopsis. Additional material from the sub-Antarctic Indian Ocean has been referred to Africanacetus sp. and may represent a third, as yet undescribed species.[2] The genus is closely related to extant hyperoodontines such as Mesoplodon, Hyperoodon, and Indopacetus, sharing with them key cranial specializations including a mesorostral groove filled by dense bone and a highly modified vertex.[3][4]

Description

The known species and referred material of Africanacetus differ primarily in overall size, robustness of the rostrum, and degree of cranial ossification. A. ceratopsis is a large beaked whale (between 5-7.5 m or 16-25 ft) [5] characterized by a robust rostrum and well-developed dome-like maxillary crests, forming the baseline morphology for the genus.[3] In contrast, A. gracilis possesses a more slender and gracile skull, with comparatively reduced robustness of the rostrum and facial structures. The sub-Antarctic specimens referred to Africanacetus sp. are notably larger than A. ceratopsis, estimated at around 6 m (20 ft) with a broader and more massive rostrum and especially hypertrophied mesorostral ossification, suggesting either pronounced intraspecific variation or the presence of a distinct, as yet undescribed species.[2] The development of the vertex and surrounding cranial structures implies complex sound production and focusing capabilities, with the melon likely functioning in acoustic beam formation as in extant ziphiids.[2]

Paleobiology

Paleoecology

References

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