Abstract

Diaphyseal morphology of long bones, in part, reflects in vivo loads experienced during the lifetime of an individual. The first metatarsal, as a cornerstone structure of the foot, presumably expresses diaphyseal morphology that reflects loading history of the foot during stance phase of gait. Human feet differ substantially from those of other apes in terms of loading histories when comparing the path of the center of pressure during stance phase, which reflects different weight transfer mechanisms. Here we use a novel approach for quantifying continuous thickness and cross-sectional geometric properties of long bones in order to test explicit hypotheses about loading histories and diaphyseal structure of adult chimpanzee, gorilla, and human first metatarsals. For each hallucal metatarsal, 17 cross sections were extracted at regularly-spaced intervals (2.5% length) between 25% and 65% length. Cortical thickness in cross sections was measured in one degree radially-arranged increments, while second moments of area were measured about neutral axes also in one degree radially-arranged increments. Standardized thicknesses and second moments of area were visualized using false color maps, while penalized discriminant analyses were used to evaluate quantitative species differences. Humans systematically exhibit the thinnest diaphyseal cortices, yet the greatest diaphyseal rigidities, particularly in dorsoplantar regions. Shifts in orientation of maximum second moments of area along the diaphysis also distinguish human hallucal metatarsals from those of chimpanzees and gorillas. Diaphyseal structure reflects different loading regimes, often in predictable ways, with human versus non-human differences probably resulting both from the use of arboreal substrates by non-human apes and by differing spatial relationships between hallux position and orientation of the substrate reaction resultant during stance. The novel morphological approach employed in this study offers the potential for transformative insights into form-function relationships in additional long bones, including those of extinct organisms (e.g., fossils).

Highlights

  • Humans exhibit a unique foot structure that is distinct from African ape foot structure [1,2,3,4]

  • Using a morphometric map approach, the present study has demonstrated that a range of high Second moment of area (SMA) reinforce hallucal metatarsal diaphyses to either side of the direction of its greatest bending stiffness (Fig. 5)

  • Unlike chimpanzee and gorilla hallucal metatarsals, human hallucal metatarsals exhibit the greatest resistance to bending in dorsoplantar orientations

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Summary

Introduction

Humans exhibit a unique foot structure that is distinct from African ape foot structure [1,2,3,4]. That the human hallux functions comparatively better as a stable lever in a metatarsi-fulcrimating foot is likely a consequence of selection favoring a more medial and stereotyped path of the center of pressure during human bipedalism compared to the more lateral and variable path of the center of pressure observed during Pan terrestrial bipedalism or quadrupedalism [8], [28,29,30]. This difference is accentuated even more by speed (i.e., during higher pressures) since the center of pressure in the human foot follows an even more medial trajectory at faster speeds [11]. The comparatively more medial position of the center of pressure during stance would facilitate more close-packing of joints comprising the human bony longitudinal arch and elastic energy return from its associated ligamentous structures such as the plantar aponeurosis [11], [15], [17,18]

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