TY - JOUR
T1 - Juvenile hominoid cranium from the terminal Miocene of Yunnan, China
AU - Ji, Xue Ping
AU - Jablonski, Nina G.
AU - Su, Denise F.
AU - Deng, Cheng Long
AU - Flynn, Lawrence J.
AU - You, You Shan
AU - Kelley, Jay
N1 - Funding Information:
Museum) for help in the field; Dr. Yohannes Haile-Selassie, Curator of Physical Anthropology, and Lyman Jellema, collections manager (Cleveland Museum of Natural History), Linda Gordon, collections manager (United States Natural History Museum) and Richard Kraft, Director (Zo-ologisches Staatssammlung, München) for allowing us to examine specimens housed at their institutions; Zhang Jianjun (Institute of Vertebrate Paleontology and Paleoanthropology) and You Pingping (Yunnan Institute of Cultural Relics and Archaeology) for help in preparing ZT 299; Tim Ryan and Yann Heuze (Penn State University) for the CT rendering; and the Yunnan Bureau of Geology and Mineral Resources Exploration for aid in drilling the borehole. This work was supported by the National Science Foundation (BCS 1035897, BCS 1227838 and BCS 0321893), Bryn Mawr College, the American Association of Physical Anthropologists the Yunnan Natural Science Foundation (2010CC010), the Zhaotong Government, the National Basic Research Program of China and the National Natural Science Foundation of China (2012CB821900 and 40925012). Figure 1 was prepared by George Chaplin and Figures 3–7 by Tess Wilson.
PY - 2013/11
Y1 - 2013/11
N2 - Fossil apes are known from several late Miocene localities in Yunnan Province, southwestern China, principally from Shihuiba (Lufeng) and the Yuanmou Basin, and represent three species of Lufengpithecus. They mostly comprise large samples of isolated teeth, but there are also several partial or complete adult crania from Shihuiba and a single juvenile cranium from Yuanmou. Here we describe a new, relatively complete and largely undistorted juvenile cranium from the terminal Miocene locality of Shuitangba, also in Yunnan. It is only the second ape juvenile cranium recovered from the Miocene of Eurasia and it is provisionally assigned to the species present at Shihuiba, Lufengpithecus lufengensis. Lufengpithecus has most often been linked to the extant orangutan, Pongo pygmaeus, but recent studies of the crania from Shihuiba and Yuanmou have demonstrated that this is unlikely. The new cranium reinforces the view that Lufengpithecus represents a distinct, late surviving lineage of large apes in the late Miocene of East Asia that does not appear to be closely affiliated with any extant ape lineage. It substantially increases knowledge of cranial morphology in Lufengpithecus and demonstrates that species of this genus represent a morphologically diverse radiation of apes, which is consistent with the dynamic tectonic and biotic milieu of southwestern China in the late Miocene.
AB - Fossil apes are known from several late Miocene localities in Yunnan Province, southwestern China, principally from Shihuiba (Lufeng) and the Yuanmou Basin, and represent three species of Lufengpithecus. They mostly comprise large samples of isolated teeth, but there are also several partial or complete adult crania from Shihuiba and a single juvenile cranium from Yuanmou. Here we describe a new, relatively complete and largely undistorted juvenile cranium from the terminal Miocene locality of Shuitangba, also in Yunnan. It is only the second ape juvenile cranium recovered from the Miocene of Eurasia and it is provisionally assigned to the species present at Shihuiba, Lufengpithecus lufengensis. Lufengpithecus has most often been linked to the extant orangutan, Pongo pygmaeus, but recent studies of the crania from Shihuiba and Yuanmou have demonstrated that this is unlikely. The new cranium reinforces the view that Lufengpithecus represents a distinct, late surviving lineage of large apes in the late Miocene of East Asia that does not appear to be closely affiliated with any extant ape lineage. It substantially increases knowledge of cranial morphology in Lufengpithecus and demonstrates that species of this genus represent a morphologically diverse radiation of apes, which is consistent with the dynamic tectonic and biotic milieu of southwestern China in the late Miocene.
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U2 - 10.1007/s11434-013-6021-x
DO - 10.1007/s11434-013-6021-x
M3 - Article
AN - SCOPUS:84887445204
SN - 1001-6538
VL - 58
SP - 3771
EP - 3779
JO - Chinese Science Bulletin
JF - Chinese Science Bulletin
IS - 31
ER -