TY - JOUR
T1 - Structure and composition of the Trinil femora
T2 - Functional and taxonomic implications
AU - Ruff, Christopher B.
AU - Puymerail, Laurent
AU - Macchiarelli, Roberto
AU - Sipla, Justin
AU - Ciochon, Russell L.
N1 - Funding Information:
We thank John de Vos and Reinier van Zelst for access to the Trinil femora housed in the Rijksmuseum van Natuurlijke Historie in Leiden. John de Vos also arranged for and transported the fossils to the Rode Kruis Hospital in The Hague where Tom Hogervorst, M.D. and Heinse Bouma, M.D. undertook the CT scanning in two separate sessions. We also want to thank the following people for help with data collection and organization: Philippe Mennecier, Alain Froment, Arnaud Mazurier, Virginie Volpato, Luca Bondioli, Frank Huffman, and Hannah Marsh. Thanks also to Connie Fellmann and Susan Antón for making available unpublished material and for useful discussions of length estimation in the Trinil femora. Supported by the National Science Foundation , Wenner-Gren Foundation for Anthropological Research, the Human Evolutionary Research Fund at the University of Iowa Foundation, MNHN Paris, and the French INEE CNRS.
Publisher Copyright:
© 2015 Published by Elsevier Ltd.
PY - 2015/3/1
Y1 - 2015/3/1
N2 - The original hominin femur (Femur I) and calotte discovered at Trinil, Java by Eugene Dubois in 1891/1892 played a key role in the early history of human paleontology by purportedly demonstrating the contemporaneity of archaic cranial form with modern human erect (bipedal) posture. On this basis, both specimens were subsequently assigned to Pithecanthropus erectus, later transferred to Homo erectus. However, chronological and phylogenetic links between the two have been questioned from the beginning. Four additional hominin partial femora (Femora II-V) from Trinil were subsequently described but have played a relatively minor part in evolutionary scenarios. Here we present the results of a new analysis of structural and density characteristics of the Trinil femora obtained using computed tomography. Trinil Femur I shows none of the characteristics typical of early Homo femora from elsewhere in Asia or Africa, including a relatively long neck, increased mediolateral bending rigidity of themid-proximal shaft, or a low position of minimum mediolateral breath on the shaft. In contrast, Femora II-V all demonstrate features that are more consistent with this pattern. In addition, material density distributions within the specimens imply more recent and less complete fossilization of Femur I than Femora II-V. Thus, it is very likely that Trinil Femur I derives from a much more recent time period than the calotte, while the less famous and less complete Femora II-V may represent H.erectus at Trinil. The morphological variation within the Trinil femora can be attributed to broader changes in pelvic morphology occurring within the Homo lineage between the Early and late Middle Pleistocene.
AB - The original hominin femur (Femur I) and calotte discovered at Trinil, Java by Eugene Dubois in 1891/1892 played a key role in the early history of human paleontology by purportedly demonstrating the contemporaneity of archaic cranial form with modern human erect (bipedal) posture. On this basis, both specimens were subsequently assigned to Pithecanthropus erectus, later transferred to Homo erectus. However, chronological and phylogenetic links between the two have been questioned from the beginning. Four additional hominin partial femora (Femora II-V) from Trinil were subsequently described but have played a relatively minor part in evolutionary scenarios. Here we present the results of a new analysis of structural and density characteristics of the Trinil femora obtained using computed tomography. Trinil Femur I shows none of the characteristics typical of early Homo femora from elsewhere in Asia or Africa, including a relatively long neck, increased mediolateral bending rigidity of themid-proximal shaft, or a low position of minimum mediolateral breath on the shaft. In contrast, Femora II-V all demonstrate features that are more consistent with this pattern. In addition, material density distributions within the specimens imply more recent and less complete fossilization of Femur I than Femora II-V. Thus, it is very likely that Trinil Femur I derives from a much more recent time period than the calotte, while the less famous and less complete Femora II-V may represent H.erectus at Trinil. The morphological variation within the Trinil femora can be attributed to broader changes in pelvic morphology occurring within the Homo lineage between the Early and late Middle Pleistocene.
KW - Eugene Dubois
KW - Femur
KW - Homo erectus
KW - Java
KW - Skeletal structure
KW - Solo River
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U2 - 10.1016/j.jhevol.2014.12.004
DO - 10.1016/j.jhevol.2014.12.004
M3 - Article
C2 - 25681015
AN - SCOPUS:84923380911
SN - 0047-2484
VL - 80
SP - 147
EP - 158
JO - Journal of Human Evolution
JF - Journal of Human Evolution
ER -