2018
DOI: 10.1007/s12542-018-0419-3
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Problematic archaic whale Phococetus (Cetacea: Odontoceti) from the Lee Creek Mine, North Carolina, USA, with comments on geochronology of the Pungo River Formation

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Cited by 3 publications
(2 citation statements)
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“…In a study of cetacean specimens from the Miocene Pungo River Formation and Pliocene Yorktown Formation of the Lee Creek Mine, further north in North Carolina, Whitmore and Kaltenbach ( [40]: [188][189] reported an odontocete mandible fragment (USNM 182924) with widely spaced double rooted alveoli and embrasure pits in line with the toothrow, which they speculated might represent a xenorophid. Boessenecker [41] agreed, noting that such mandibular embrasure pits are otherwise unknown amongst stem odontocetes. Boessenecker [41] further identified an isolated xenorophid bulla (CCNHM 936) from the Pungo River Formation, and speculated that such specimens perhaps represent reworking of Oligocene fossils into the base of the Pungo River Formation or perhaps the survival of these archaic taxa into the earliest Miocene.…”
Section: History Of Study Of the Xenorophidaementioning
confidence: 99%
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“…In a study of cetacean specimens from the Miocene Pungo River Formation and Pliocene Yorktown Formation of the Lee Creek Mine, further north in North Carolina, Whitmore and Kaltenbach ( [40]: [188][189] reported an odontocete mandible fragment (USNM 182924) with widely spaced double rooted alveoli and embrasure pits in line with the toothrow, which they speculated might represent a xenorophid. Boessenecker [41] agreed, noting that such mandibular embrasure pits are otherwise unknown amongst stem odontocetes. Boessenecker [41] further identified an isolated xenorophid bulla (CCNHM 936) from the Pungo River Formation, and speculated that such specimens perhaps represent reworking of Oligocene fossils into the base of the Pungo River Formation or perhaps the survival of these archaic taxa into the earliest Miocene.…”
Section: History Of Study Of the Xenorophidaementioning
confidence: 99%
“…Boessenecker [41] agreed, noting that such mandibular embrasure pits are otherwise unknown amongst stem odontocetes. Boessenecker [41] further identified an isolated xenorophid bulla (CCNHM 936) from the Pungo River Formation, and speculated that such specimens perhaps represent reworking of Oligocene fossils into the base of the Pungo River Formation or perhaps the survival of these archaic taxa into the earliest Miocene. More recent discoveries of xenorophid specimens apparently straddling the Oligocene-Miocene boundary [7] lend support to this latter hypothesis.…”
Section: History Of Study Of the Xenorophidaementioning
confidence: 99%