Dehm & Oettingen-Spielberg 1958 described the first pakicetid, Ichthyolestes, but, though, at the time, they did not recognize it as a cetacean, instead, identifying it as a fish-eating mesonychid. West 1980 was the first to identify pakicetids as cetaceans and, following the discovery of a braincase, Gingerich & Russell 1981 were able to describe the genus Pakicetus. During the following two decades, more research resulted in additional pakicetid cranial material and Thewissen et al. 2001 described postcranial material for the family. Though all parts of pakicetid postcrania are known, no complete skeleton from a single individual has been recovered. The pakicetid goldmine is the "H-GSP Locality 62" site in the Kala Chitta Hills where fossils from all three genera have been found. However, this site is so littered with bones that identifying bones from a single individual is impossible, and pakicetid skeletons are consequently composites of bones from several individuals.
Pakicetids have been found in or near river deposits in northern Pakistan and northwestern India, a region which was probably arid with only temporal streams when these animals lived there. No pakicetids have been found in marine deposits, and they were apparently terrestrial or freshwater animals. Their long limbs and small hands and feet also indicate they were poor swimmers. Their bones are heavy and compact and were probably used as ballast; they clearly indicate pakicetids were not fast runners notwithstanding their otherwise cursorial morphology. Most likely, pakicetids lived in or near bodies of freshwater and their diet can have included both land animals and aquatic organisms.
|Pakicetids have many apomorphic traits (derived traits shared by several taxa) found in artiodactyls, including:||Traits linking pakicetids to cetaceans include:|
Pakicetid ears had an external auditory meatus and ear ossicles (i.e. incus, malleus, tympanic ring, etcetera) similar to those in living land mammals and most likely used normal land mammal hearing in air. In the pakicetid mandible, the mandibular foramen is small and comparable in size to those of extant land mammals and the acoustic mandibular fat pad characteristic of later whales was obviously not present. The lateral wall of the mandible is also relatively thick in pakicetids, further preventing sound transmission through the jaw. The tympanic bulla in pakicetid ears is similar to those in all cetaceans, with a relatively thin lateral wall and thickened medial part known as the involucrum. However, in contrast to later cetaceans, the tympanic bone makes contact with the periotic bone which is firmly attached to the skull leaving no space for isolating air sinuses, effectively preventing directional hearing in water. Pakicetids most likely used bone conduction for hearing in water.
Interpretations of pakicetid habitat and locomotion behaviour varies considerably:
Thewissen et al. 2001 concluded that "pakicetids were terrestrial mammals, no more amphibious than a tapir." According to them, none of the aquatic adaptations found in the oldest obligate aquatic cetaceans, basilosaurids and dorundontids, are present in pakicetids. Pakicetid cervical vertebrae are longer than in late Eocene whales, the thoracic vertebrae increase in size from the neck backwards, and the lumbar and caudal vertebrae are longer than in modern cetaceans (but still shorter than in some extinct cetaceans with undulating spines.) Motion in the spine of pakicetids was further reduced by the revolute zygapophyses (processes between the vertebrae) like in stiff-backed runners such as mesonychians. The sacral vertebrae are fused and the sacroiliac joints present like in land mammals and amphibious cetaceans.
Furthermore, according to Thewissen et al., the pakicetid scapulae have large supraspinous fossae with small acromions, in contrast to other cetaceans. The deltopectoral crests are absent in the long and slender humeri like in cursorial animals but unlike other Eocene cetaceans. Pakicetid elbows are rigid hinge joints like in running mammals and the forearms are not flattened like in truly aquatic cetaceans. In the pakicetid pelvis, the innominates are large and the ischia are longer than the ilia. The pakicetid tibiae are long with a short tibial crest. Hindlimb features that all more reminiscent of running and jumping animals than swimming ones.
Gingerich 2003 disagreed and got support from Madar 2007: postcranial morphology and microstructural features suggest that pakicetids were adapted to an aquatic lifestyle which included bottom wading, paddling, and undulatory swimming, but probably not sustained running. Isotopic evidence indicate Pakicetids spent a considerable part of their life in freshwater and probably ate freshwater prey.
- Family Pakicetidae
- Ichthyolestes (Dehm & Oettingen-Spielberg 1958)
- Ichtyolestes pinfoldi (Dehm & Oettingen-Spielberg 1958)
- Nalacetus (Thewissen & Hussain 1998)
- Nalacetus ratimitus (Thewissen & Hussain 1998)
- Pakicetus (Gingerich & Russell 1981)
- Ichthyolestes (Dehm & Oettingen-Spielberg 1958)
|Wikispecies has information related to: Pakicetidae|
- Cooper, Lisa Noelle; Thewissen, J. G. M.; Hussain, S. T. (2009). "New middle Eocene archaeocetes (Cetacea: Mammalia) from the Kuldana Formation of northern Pakistan". Journal of vertebrate paleontology 94 (4): 1289–99. doi:10.1671/039.029.0423. OCLC 506008976.
- Dehm, Richard; Oettingen-Spielberg, Therese zu (1958). Paläontologische und geologische Untersuchungen im Tertiär von Pakistan. 2. Die mitteleocänen Säugetiere von Ganda Kas bei Basal in Nordwest-Pakistan. Abhandlungen / Neue Folge, 91. Munich: Beck. OCLC 163296508.
- Gingerich, Philip D. (2003). "Land-to-sea transition in early whales: evolution of Eocene Archaeoceti (Cetacea) in relation to skeletal proportions and locomotion of living semiaquatic mammals". Paleobiology 29 (3): 429–54. doi:10.1666/0094-8373(2003)029<0429:ltiewe>2.0.co;2. OCLC 716582744.
- Gingerich, Philip D.; Russell, Donald E. (1981). "Pakicetus inachus, A New Archaeocete (Mammalia, Cetacea) from the Early-Middle Eocene Kuldana Formation of Kohat (Pakistan)". Contributions from the Museum of Paleontology, The Museum of Michigan 25 (11). OCLC 742729300. Retrieved February 2013.
- Madar, S. I. (2007). "The postcranial skeleton of early Eocene pakicetid cetaceans". J. Paleontol. 81 (1): 176–200. doi:10.1666/0022-3360(2007)81[176:TPSOEE]2.0.CO;2. OCLC 204527975.
- Nummela, Sirpa; Thewissen, J.G.M.; Bajpai, Sunil; Hussain, Taseer; Kumar, Kishor (2007). "Sound transmission in archaic and modern whales: Anatomical adaptations for underwater hearing". The Anatomical Record (Special Issue: Anatomical Adaptations of Aquatic Mammals) 290 (6): 716–33. doi:10.1002/ar.20528. PMID 17516434.
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- Thewissen, J. G. M.; Hussain, S. T. (1998). "Systematic review of the Pakicetidae, Early and middle Eocene Cetacea (Mammalia) from Pakistan and India". Bulletin of the Carnegie Museum 34: 220–38.
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- Thewissen, J. G. M.; Williams, E. M.; Roe, L. J.; Hussain, S. T. (2001). "Skeletons of terrestrial cetaceans and the relationship of whales to artiodactyls". Nature 413: 277–81. doi:10.1038/35095005. OCLC 118116179. PMID 11565023. Retrieved February 2013.
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- West, Robert M (1980). "Middle Eocene large mammal assemblage with Tethyan affinities, Ganda Kas region, Pakistan". Journal of Paleontology 54 (3): 508–533. JSTOR 1304193. OCLC 4899161959.
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