Abstract

Fossil evidence for longitudinal arches in the foot is frequently used to constrain the origins of terrestrial bipedality in human ancestors. This approach rests on the prevailing concept that human feet are unique in functioning with a relatively stiff lateral mid-foot, lacking the significant flexion and high plantar pressures present in non-human apes. This paradigm has stood for more than 70 years but has yet to be tested objectively with quantitative data. Herein, we show that plantar pressure records with elevated lateral mid-foot pressures occur frequently in healthy, habitually shod humans, with magnitudes in some individuals approaching absolute maxima across the foot. Furthermore, the same astonishing pressure range is present in bonobos and the orangutan (the most arboreal great ape), yielding overlap with human pressures. Thus, while the mean tendency of habitual mechanics of the mid-foot in healthy humans is indeed consistent with the traditional concept of the lateral mid-foot as a relatively rigid or stabilized structure, it is clear that lateral arch stabilization in humans is not obligate and is often transient. These findings suggest a level of detachment between foot stiffness during gait and osteological structure, hence fossilized bone morphology by itself may only provide a crude indication of mid-foot function in extinct hominins. Evidence for thick plantar tissues in Ardipithecus ramidus suggests that a human-like combination of active and passive modulation of foot compliance by soft tissues extends back into an arboreal context, supporting an arboreal origin of hominin bipedalism in compressive orthogrady. We propose that the musculoskeletal conformation of the modern human mid-foot evolved under selection for a functionally tuneable, rather than obligatory stiff structure.

Highlights

  • The human foot is considered one of our most distinctive morphological and functional features, yet few of the many hypothesized form –function relationships associated with its mechanics and evolution have ever been tested [1]

  • These findings suggest a level of detachment between foot stiffness during gait and osteological structure, fossilized bone morphology by itself may only provide a crude indication of mid-foot function in extinct hominins

  • This study provides the first quantitative analysis of relative mid-foot function in human and non-human great apes during bipedal terrestrial locomotion

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Summary

Introduction

The human foot is considered one of our most distinctive morphological and functional features, yet few of the many hypothesized form –function relationships associated with its mechanics and evolution have ever been tested [1]. License http://creativecommons.org/licenses/by/3.0/, which permits unrestricted use, provided the original author and source are credited This apparent dichotomy has provided anthropology with a crucial interpretative paradigm: that fossil evidence for longitudinal arches of the foot and a mid-foot seemingly stabilized in bone can be used to constrain the time of appearance of terrestrial bipedality and modern foot function in human ancestors [2,3,4,5]. We analyse a unique dataset of over 21 500 human plantar pressure records collected at a standardized walking speed using a Zebris FDM-T treadmill Analysis of this new dataset in comparison to pressure records of two NHAs (bonobos and orangutans) allows us to begin to quantitatively constrain the nature and magnitude of functional differences between the feet of human and NHAs, and shed light on the evolution of compliance in the hominin foot. In addition to analysing the relative frequency within these categories, we conducted topological statistical comparisons [9,11] of these subsampled groups to identify any systematic changes in pressure distribution that correlate with differences in mid-foot pressure

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