Philip Gingerich | University of Michigan (original) (raw)
Papers by Philip Gingerich
Fossil vertebrate remains were first found in the Bighorn Basin of northwestern Wyoming in 1880, ... more Fossil vertebrate remains were first found in the Bighorn Basin of northwestern Wyoming in 1880, and the Bighorn Basin and adjacent Clark's Fork Basin have since become classic collecting areas documenting the succession of early Cenozoic vertebrate faunas in ...
J Vertebrate Paleontol, 1995
Paleobiology, Sep 1, 2003
Skeletal remains of Eocene Archaeoceti provide the only direct and unequivocal evidence of the ev... more Skeletal remains of Eocene Archaeoceti provide the only direct and unequivocal evidence of the evolutionary transition of whales from land to sea. Archaeocete skeletons complete enough to be informative about locomotion are rare (principally Rodhocetus and Dorudon), and ...
Journal of Vertebrate Paleontology, Aug 24, 2010
Annual Review of Ecology Evolution and Systematics, 2009
Palaeontographica Abteilung a Stuttgart, 2009
Fossil vertebrate remains were first found in the Bighorn Basin of northwestern Wyoming in 1880, ... more Fossil vertebrate remains were first found in the Bighorn Basin of northwestern Wyoming in 1880, and the Bighorn Basin and adjacent Clark's Fork Basin have since become classic collecting areas documenting the succession of early Cenozoic vertebrate faunas in ...
J Vertebrate Paleontol, 1995
Paleobiology, Sep 1, 2003
Skeletal remains of Eocene Archaeoceti provide the only direct and unequivocal evidence of the ev... more Skeletal remains of Eocene Archaeoceti provide the only direct and unequivocal evidence of the evolutionary transition of whales from land to sea. Archaeocete skeletons complete enough to be informative about locomotion are rare (principally Rodhocetus and Dorudon), and ...
Journal of Vertebrate Paleontology, Aug 24, 2010
Annual Review of Ecology Evolution and Systematics, 2009
Palaeontographica Abteilung a Stuttgart, 2009