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Ichthyolestes

From Wikipedia, the free encyclopedia
Genus of mammals

Ichthyolestes
Temporal range:Early Eocene, circa50 Ma
Ichthyolestes life restoration, pencil drawing.
Scientific classificationEdit this classification
Domain:Eukaryota
Kingdom:Animalia
Phylum:Chordata
Class:Mammalia
Order:Artiodactyla
Infraorder:Cetacea
Family:Pakicetidae
Genus:Ichthyolestes
Dehm & Oettingen-Spielberg 1958
Type species
Ichthyolestes pinfoldi

Ichthyolestes ("fish thief") is an extinct genus ofarchaic cetacean that was endemic to the northernIndian subcontinent during theLutetian stage.[1] To date, thismonotypic genus is only represented byIchthyolestes pinfoldi.[1]

Like other members of the familyPakicetidae, which are considered the earliest and least specialized of the archaic cetaceans,[2]Ichthyolestes represents an early quadrupedal phase of the land-to-sea transition which occurs in the cetacean lineage.[3][4]

Discovery and classification

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Size ofIchthyolestes compared to a human.

Ichthyolestes pinfoldi was initially known only from teeth, which were found in theEocene epoch near what is now Ganda Kas,Pakistan.[1][5] Upon their discovery,I. pinfoldi was placed within the familyMesonychidae,[1][3] a group of terrestrial mammals from which cetaceans were previously thought to have evolved.[6] Due to morphological distinctions from other mesonychids,I. pinfoldi was later acknowledged and described as anarchaeocete,[7][8] making it the first pakicetid to be described.[4]

Cranial and postcranial material ofI. pinfoldi have also been found in theKuldana Formation located in present-day Pakistan, from the early-middle Eocene,[8][6][9][2] and from theSubathu sediments of Jammu and Kashmir,India.[10]

Description

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Ichthyolestes is the smallest pakicetid, approximately 29% smaller thanPakicetus, and has been considered “fox-sized.”[9] They retain many features typical of terrestrial Eoceneartiodactyls, including long and gracilelimb bones, a fusedsacrum, smallmandibular foramen, and no cranial telescoping.[9][11] The body plan ofIchthyolestes is generally similar toPakicetus, but smaller and more gracile.[2][4] Therefore, locomotion is also thought to be reliant on quadrupedal paddling.[4]

Teeth

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Ichthyolestes exhibitsheterodont anddiphyodont dentition withcusped cheek teeth.[4] The upper second molar has pointed cusps with a high narrowparacone and a lower connatemetacone behind it.[8][10] The molars are also relatively labio-lingually compressed with serrated crests along the labial cusps.[8][10]

Braincase and orbital region anIchthyolestes pinfoldi skull (HGSP 98134)

Cranial

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Ichthyolestes has dorsally oriented eyes and a narrow skull, which is smaller than the skulls of bothPakicetus andNalacetus.[3] Like other pakicetids,Ichthyolestes lacks asupraorbital shield; however, there is some variation in supraorbitalmorphology between the three genera. The supraorbital region ofIchthyolestes andPakicetus is cup-like and cradles the dorsal portion of the eye.Ichthyolestes also has a weaker incisure on the dorsal side of the supraorbital region compared toPakicetus.[3]

All three pakicetid taxa largely retained the peripheral ear morphology of terrestrial mammals,[11] but likely used bone conducting mechanisms when hearing underwater. Thetympanic bulla also differs between pakicetid taxa.[3] The absolute size ofIchthyolestes tympanic bulla is smaller than eitherPakicetus orNalacetus; but when compared relative to their body size, the tympanic bulla ofIchthyolestes is proportionally larger than that ofPakicetus.[3]

Thesemicircular canal system of thevestibular apparatus in the inner ear, which is involved in neural control of locomotion, is similar in size to that of Eocene artiodactyls.[12] They do not show the size reduction as seen in other pakicetids and Eocene cetaceans likeRemingtonocetus,Indocetus, andDorudon, which have canal sizes within the upper range of modern cetaceans.[12] This suggests thatIchthyolestes had not fully invaded aquatic ecosystems and still remained somewhat terrestrial.[12]

Postcranial

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AlthoughIchthyolestes is the smallest pakicetid, some features are larger or more robust thanNalacetus, such as theastragalus,calcaneus, andpelvis.Ichthyolestes also has proportionally longerlumbar andcaudal vertebrae relative to its shorter limb segments.[2]

Ichthyolestes also has long digits and strong post-thoracic vertebrae.[2] Thesacrum is composed of four elongate vertebrae with complete fusion, except for thespinous processes of S2 to S4 which are columnar with smooth ventral faces.[2] The lumbar vertebrae are narrower and shallower toPakicetus andNalacetus.[2] Although still relatively large compared to other related taxa, the atlas vertebrae ofIchthyolestes is smaller and more gracile thanPakicetus orNalacetus, and theneural canal is disproportionately large.[2]

Terrestrial or semi-aquatic locomotion

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Theastragalus bone, which is present in the ankle ofartiodactyls and archaic whales that retained feet, has similar dimensions in both Eocene artiodactyls andIchthyolestes.[5] In addition to lending evidence to the theory of a direct relationship between artiodactyls and cetaceans,[11] this knowledge has led to two competing hypotheses about the locomotion ofIchthyolestes and otherpakicetids. The first states thatIchthyolestes andPakicetus were terrestrial andcursorial, implying that aquatic locomotor adaptation occurred after the origin ofCetacea.[9][13] The second states thatIchthyolestes andPakicetus were already semi-aquatic and cetaceans originated from an earlier unknown Eocene artiodactyl, such asElomeryx[14][15] orIndohyus,[16][17] implying that aquatic locomotor adaptations occurred before or during the origin of Cetacea.[5]

Although the postcranial anatomy ofIchthyolestes is similar to that of Eocene artiodactyls and implies cursoriality,[2][5] the assessment ofbonemorphology andmicrostructure indicate that they, and other pakicetids, were semi-aquatic likeprotocetids.[2] Hypermineralization occurs in all regions of the skeleton; in particular, thelong bones andribs had small or absent marrow cavities due to the thick cortices which developed.[2] Hypermineralization of load-bearing skeletal elements putIchthyolestes at an increased risk of fractures during prolonged terrestrial loading and this risk increased withvelocity, implying that terrestriality was limited.[2] Additionally, the dense skeletons may have allowed bottom-walking or wading in shallow pools as it would counteract buoyancy created by inflatedlungs andfur-trapped air.[2] Therefore, the retention of an artiodactyl-like astragalus does not signify full terrestriality or cursoriality inIchthyolestes.[2][5]

Paleoenvironment

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Fossil findings indicateIchthyolestes sharedhabitat with its relativesPakicetus andNalacetus.[18] Their fossils are usually found around river channel deposits, not marine deposits or fauna.[4] The regions around northern Pakistan and northwest India, where fossils have been recovered, are thought to have been anarid environment with ephemeral streams and moderately developedfloodplains.[19]Ichthyolestes, therefore, had an affinity for water and were either terrestrial or semi-aquatic.[4] The fluvial facies of the lower Kuldana Formation represent shallow tropical riverine complexes and were likely habitats for the initial stages of transition into water.[5][2]

See also

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References

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  1. ^abcdDehm, R.; zu Oettingen-Spielberg, T. (1958).Paläontologische und geologische Untersuchungen im Tertiär von Pakistan. 2. Die mitteleocänen Säugetiere von Ganda Kas bei Basal in Nordwest-Pakistan(PDF). Bayerische Akademie der Wissenschaften, Mathematisch-naturwissenschaftliche Klasse, Abhandlungen, Neue Folge. Vol. 91. Munich: C. Beck’sche Verlagsbuchhandlung.
  2. ^abcdefghijklmnoMadar, S. (2007). "The postcranial skeleton of early Eocene Pakicetid cetaceans".Journal of Paleontology.81 (1):176–200.doi:10.1666/0022-3360(2007)81[176:TPSOEE]2.0.CO;2.
  3. ^abcdefNummela, S.; Hussain, S. T.; Thewissen, J. G. M. (2006). "Cranial anatomy of Pakicetidae (Cetacea, Mammalia)".Journal of Vertebrate Paleontology.26 (3):746–759.doi:10.1671/0272-4634(2006)26[746:CAOPCM]2.0.CO;2.
  4. ^abcdefgThewissen, J. G. M.; Williams, E. M. (2002). "The early radiation of Cetacea (Mammalia): Evolutionary pattern and development correlations".Annual Review of Ecology and Systematics.33 (1):73–90.Bibcode:2002AnRES..33...73T.doi:10.1146/annurev.ecolsys.33.020602.095426.
  5. ^abcdefGingerich, P. D.; Heissig, K.; Bebej, R. M.; von Koenigswald, W. (2017). "Astragali of Pakicetidae and other early-to-middle Eocene archaeocetes (Mammalia, Cetacea) of Pakistan: Locomotion and habitat in the initial stages of whale evolution".PalZ.91 (4):601–627.Bibcode:2017PalZ...91..601G.doi:10.1007/s12542-017-0362-8.
  6. ^abGingerich, P. D.; Wells, N. A.; Russell, D. E.; Ibrahim Shah, S. M. (1983). "Origin of whales in epicontinental seas: New evidence from the early Eocene of Pakistan".Science.220 (4595):403–406.doi:10.1126/science.220.4595.403.PMID 17831411.
  7. ^Gingerich, P. D.; Russell, D. E.; Sigogneau-Russell, D.; Hartenberger, J. -L.; Ibrahim Shah, S. M.; Hassan, M.; Rose, K. D.; Ardrey, R. H. (1979). "Reconnaissance survey and vertebrate paleontology of some Paleocene and Eocene formations in Pakistan".Contributions from the Museum of Paleontology University of Michigan.25 (5):105–116.
  8. ^abcdWest, R. M. (1980). "Middle Eocene large mammal assemblage with Tethyan affinities, Ganda Kas Region, Pakistan".Journal of Paleontology.54:508–533.
  9. ^abcdThewissen, 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 (6853):277–281.Bibcode:2001Natur.413..277T.doi:10.1038/35095005.PMID 11565023.
  10. ^abcKumar, K.; Sahni, A. (1985). "Eocene mammals from the Upper Subathu group, Kashmir Himalaya, India".Journal of Vertebrate Paleontology.5 (2):153–168.Bibcode:1985JVPal...5..153K.doi:10.1080/02724634.1985.10011853.
  11. ^abcMarx, F. G.; Lambert, O.; Uhen, M. D. (2016).Cetacean Paleobiology. Chichester, UK; Hoboken, NJ: John Wiley & Sons Ltd.Bibcode:2016cepa.book.....M.
  12. ^abcSpoor, F.;Bajpai, S.; Hussain, S. T.; Kumar, K.;Thewissen, J. G. M. (2002). "Vestibular evidence for the evolution of aquatic behaviour in early cetaceans".Nature.417 (6885):163–166.Bibcode:2002Natur.417..163S.doi:10.1038/417163a.PMID 12000957.
  13. ^Fish, F. E. (2016). "Secondary evolution of aquatic propulsion in higher vertebrates: Validation and prospect".Integrative and Comparative Biology.56 (6):1285–1297.doi:10.1093/icb/icw123.PMID 27697779.
  14. ^Gingerich, P. D.; Haq, M.; Zalmout, I. S.; Khan, I. H.; Malkani, M. S. (2001). "Origin of whales from early artiodactyls: Hands and feet of Eocene Protocetidae from Pakistan".Science.293 (5538):2239–2242.Bibcode:2001Sci...293.2239G.doi:10.1126/science.1063902.PMID 11567134.
  15. ^Gingerich, P. D. (2003). "Land-to-sea transition of early whales: Evolution of Eocene Archaeoceti (Cetacea) in relation to skeletal proportions and locomotion of living semiaquatic mammals".Paleobiology.29 (3):429–454.Bibcode:2003Pbio...29..429G.doi:10.1666/0094-8373(2003)029<0429:LTIEWE>2.0.CO;2.
  16. ^Thewissen, J. G. M.; Cooper, L. N.; Clementz, M. T.;Bajpai, S.; Tiwari, B. N. (2007). "Whales originated from aquatic artiodactyls in the Eocene epoch of India".Nature.450 (7173):1190–1195.Bibcode:2007Natur.450.1190T.doi:10.1038/nature06343.PMID 18097400.
  17. ^Cooper, L. N.;Thewissen, J. G. M.;Bajpai, S.; Tiwari, B. N. (2011). "Postcranial morphology and locomotion of the Eocene raoellidIndohyus (Artiodactyla: Mammalia)".Historical Biology.24:279–310.
  18. ^Cooper L.N.,Thewissen J.G.M. & Hussain S.T. (2009). "New middle Eocene archaeocetes (Cetacea: Mammalia) from the Kuldana Formation of northern Pakistan".Journal of Vertebrate Paleontology29(4): p. 746-759. [[doi:10.1671/0272-4634(2006)26[746:CAOPCM]2.0.CO;2]]
  19. ^Aslan, A.; Thewissen, J. G. M. (1996). "Preliminary evaluation of paleosols and implications for interpreting vertebrate fossil assemblages, Kuldana Formation, northern Pakistan".Palaeovertebrata.25 (2–4):261–277.

Works cited

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  • 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.

External Sources

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Ichthyolestes in thePaleobiology Database. Retrieved June 2013.

Archaeocete genera by family
Pakicetidae
Ambulocetidae
Remingtonocetidae
Protocetidae
Georgiacetinae
Makaracetinae
Protocetinae
Basilosauridae
Dorudontinae
Basilosaurinae
Pachycetinae
Ichthyolestes
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