モレノヒル累層
出典: フリー百科事典『ウィキペディア（Wikipedia）』 (2019/05/16 08:38 UTC 版)
モレノヒル累層（モレノヒルるいそう、英語: Moreno Hill Formation）は、ニューメキシコ州の白亜紀後期の地層。恐竜の化石が発見されている[1]。
- ^ Weishampel, David B; et al. (2004). "Dinosaur distribution (Late Cretaceous, North America)." In: Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. Pp. 574-588. ISBN 0-520-24209-2.
- ^ Denton, R., Ranson, W.V., Nesbitt, S., Wolfe, D.G., and Holtz, T. (2004). "A new small theropod dinosaur from the Moreno Hill Formation (Turonian, Upper Cretaceous) of New Mexico." Journal of Vertebrate Paleontology, 24(sup. 3): 52A.
- ^ McDonald, A.T., Wolfe, D.G., and Kirkland, J.I. (2006). "On a hadrosauromorph (Dinosauria: Onithopoda) from the Moreno Hill Formation (Cretaceous, Turonian) of New Mexico." Pp. 277-280 in Lucas, S.G. and Sullivan, R.M. (eds.), Late Cretaceous vertebrates from the Western Interior. New Mexico Museum of Natural History and Science Bulletin, 35.
- ^ Kirkland, J.I., and Wolfe, D.G. (2001). "First definitive therizinosaurid (Dinosauria: Theropoda) from North America." Journal of Vertebrate Paleontology, 21(3): 410-414.
- ^ "Table 7.1," in Weishampel, et al. (2004). Page 152.
- ^ Wolfe, D.G. and Kirkland, J.I. (1998). "Zuniceratops christopheri n. gen. & n. sp., a ceratopsian dinosaur from the Moreno Hill Formation (Cretaceous, Turonian) of west-central New Mexico." Pp. 303-317 in Lucas, S.G., Kirkland, J.I., Estep, J.W. (eds.), Lower and Middle Cretaceous Terrestrial Ecosystems: New Mexico Museum of Natural History and Science, Bulletin, 14.
- ^ "Table 22.1," in Weishampel, et al. (2004). Page 480.
[続きの解説]
「モレノヒル累層」の続きの解説一覧
- 1 モレノヒル累層とは
- 2 モレノヒル累層の概要
- モレノヒル累層のページへのリンク
