TY - JOUR
T1 - New remains of eocene and oligocene afrosoricida (Afrotheria) from Egypt, with implications for the origin(s) of afrosoricid zalambdodonty
AU - Seiffert, Erik R.
AU - Simons, Elwyn L.
AU - Ryan, Tomothy M.
AU - Bown, Thomas M.
AU - Attia, Yousry
N1 - Funding Information:
We thank H. Hamouda, K. Soliman, Z. el-Alfy, and the staff of the Egyptian Mineral Resources Authority and Egyptian Geological Museum for supporting our project in the Fayum area. Fieldwork was managed by P. Chatrath. Recent research in Egypt has been funded by the U.S. National Science Foundation, The Leakey Foundation, and Gordon Getty. E. Gheerbrant, L. Gordon, P. Jenkins, B. Marandat, and R. Tabuce provided access to comparative material. Two anonymous reviewers and R. Beck provided useful comments on a previous version of the manuscript.
PY - 2007/12/12
Y1 - 2007/12/12
N2 - Molecular estimates for the divergence of Chrysochloridae (golden moles) and Tenrecoidea (tenrecs) date back to near the K-T boundary, but at present the oldest undoubted fossil members of these clades are early Miocene in age (-20 Ma). The only Paleogene African genus that has been proposed as a possible stem tenrecoid is late Eocene (-34 Ma) Widanelfarasia from Egypt, heretofore known only from the lower dentition. Here we employ high-resolution computed tomography to reveal the morphology of the maxillary post-canine dentition of Widanelfarasia, and describe fragmentary dental and mandibular remains of early Oligocene Jawharia (gen. nov.) and Eochrysochloris (gen. nov.). The upper molar dentition of Widanelfarasia provides evidence for an intermediate morphological stage between moderate dilambdodonty and incipient zalambdodonty. Phylogenetic analysis employing the morphological character matrix of Asher and Hofreiter (2006) places Widanelfarasia within crown Tenrecoidea, but an alternative placement of that genus as a stem tenrecoid could not be statistically rejected. Additional support for the latter hypothesis, and for the hypothesis of convergent evolution of zalambdodonty within Afrosoricida, is provided by Eochrysochloris gen. nov., which shares apomorphic premolar features with Miocene Prochrysochloris and extant chrysochlorids, but retains a well-developed talonid basin on its lower molars. Jawharia gen. nov. is interpreted as an advanced stem tenrecoid that provides additional support for the hypothesis that tenrecoid zalambdodonty evolved from moderate dilambdodonty. Some of the apomorphic morphological features shared by Widanelfarasia and early Miocene Protenrec are also seen in Todralestes, from the oldest (late Paleocene) placental mammal-bearing locality in Africa. As such Todralestes may be a stem or crown afrosoricid, and, if so, the oldest known Afro-Arabian member of Afrotheria.
AB - Molecular estimates for the divergence of Chrysochloridae (golden moles) and Tenrecoidea (tenrecs) date back to near the K-T boundary, but at present the oldest undoubted fossil members of these clades are early Miocene in age (-20 Ma). The only Paleogene African genus that has been proposed as a possible stem tenrecoid is late Eocene (-34 Ma) Widanelfarasia from Egypt, heretofore known only from the lower dentition. Here we employ high-resolution computed tomography to reveal the morphology of the maxillary post-canine dentition of Widanelfarasia, and describe fragmentary dental and mandibular remains of early Oligocene Jawharia (gen. nov.) and Eochrysochloris (gen. nov.). The upper molar dentition of Widanelfarasia provides evidence for an intermediate morphological stage between moderate dilambdodonty and incipient zalambdodonty. Phylogenetic analysis employing the morphological character matrix of Asher and Hofreiter (2006) places Widanelfarasia within crown Tenrecoidea, but an alternative placement of that genus as a stem tenrecoid could not be statistically rejected. Additional support for the latter hypothesis, and for the hypothesis of convergent evolution of zalambdodonty within Afrosoricida, is provided by Eochrysochloris gen. nov., which shares apomorphic premolar features with Miocene Prochrysochloris and extant chrysochlorids, but retains a well-developed talonid basin on its lower molars. Jawharia gen. nov. is interpreted as an advanced stem tenrecoid that provides additional support for the hypothesis that tenrecoid zalambdodonty evolved from moderate dilambdodonty. Some of the apomorphic morphological features shared by Widanelfarasia and early Miocene Protenrec are also seen in Todralestes, from the oldest (late Paleocene) placental mammal-bearing locality in Africa. As such Todralestes may be a stem or crown afrosoricid, and, if so, the oldest known Afro-Arabian member of Afrotheria.
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U2 - 10.1671/0272-4634(2007)27[963:NROEAO]2.0.CO;2
DO - 10.1671/0272-4634(2007)27[963:NROEAO]2.0.CO;2
M3 - Article
AN - SCOPUS:38149109697
SN - 0272-4634
VL - 27
SP - 963
EP - 972
JO - Journal of Vertebrate Paleontology
JF - Journal of Vertebrate Paleontology
IS - 4
ER -