SciELO - Scientific Electronic Library Online

 
vol.113 issue11-12 author indexsubject indexarticles search
Home Pagealphabetic serial listing  

Services on Demand

Article

Indicators

Related links

  • On index processCited by Google
  • On index processSimilars in Google

Share


South African Journal of Science

On-line version ISSN 1996-7489
Print version ISSN 0038-2353

S. Afr. j. sci. vol.113 n.11-12 Pretoria Nov./Dec. 2017

http://dx.doi.org/10.17159/sajs.2017/20170306 

RESEARCH LETTER

 

Revisiting the peroneal trochlea of the StW 352 calcaneus

 

 

Ellison J. McNuttI, II; Alexander G. ClaxtonIII; Kristian J. CarlsonIV, V

IDepartment of Anthropology, Dartmouth College, Hanover, New Hampshire, USA
IIEcology, Evolution, Ecosystems and Society, Dartmouth College, Hanover, New Hampshire, USA
IIIDepartment of Anthropology, Boston University, Boston, Massachusetts, USA
IVDepartment of Integrative Anatomical Sciences, University of Southern California, Los Angeles, California, USA
VEvolutionary Studies Institute, University of the Witwatersrand, Johannesburg, South Africa

Correspondence

 

 


ABSTRACT

StW 352, from Sterkfontein Member 4 (South Africa), is a partial calcaneus attributed to Australopithecus africanus and is dated to ~2.0-2.6 Ma. The unusual robusticity of the peroneal trochlea (PT) of StW 352 has been commented on by several authors. The size of hominin PTs has been hypothesised to be positively correlated with the degree of recruitment of peroneus longus during bipedal locomotion and/or climbing. Given the potential functional relevance of an enlarged PT for reconstructing hominin activity patterns, we present the following previously unrecognised structural details of the reconstructed StW 352 that affect current interpretations of its functional morphology: (1) we estimate that the PT has been reattached to the body of the calcaneus ~5 mm dorso-distally from its original anatomical position; and (2) the presence of intrusive matrix has artificially misshaped the PT by expanding it laterally and proximodistally. Future studies of this specimen that apply geometric morphometrics, or other shape analysis tools, should compensate for these inaccuracies before undertaking comparisons between it and other calcanei. Additionally, given that the PT is likely smaller than previously reported for StW 352, caution should be exercised when using it to infer muscle function and extrapolate activity patterns of this individual, and thus by extension, within Australopithecus africanus in general. Lastly, these findings highlight the importance of not only the production of accurate reconstructions, but also the critical evaluation of the accuracy of existing reconstructions when working with damaged fossil material.
SIGNIFICANCE:
This work epitomises the value of critically evaluating original fossil reconstructions, especially of postcranial elements.
New technologies (e.g. microCT) offer non-destructive opportunities for evaluating/improving the accuracy of fossil reconstructions.
Re-assessing StW 352 suggests peroneal muscles may have factored less prominently in A. africanus locomotion than previously thought.

Keywords: Australopithecus africanus; Sterkfontein; peroneus longus; microCT; foot eversion


 

 

StW 352 is a partial right calcaneus from Member 4 of the Sterkfontein Cave formation, South Africa1,2 dated to approximately 2.0-2.6 Ma.3 Because of its provenience in Member 4, StW 352 has typically been attributed to Australopithecus africanus4-6, but that assignation is potentially complicated by a lack of consensus on the number of australopith species present in Sterkfontein Member 47-9.

The distal end of StW 352 is generally well preserved with the exception of damage to the plantar half of the articulation with the cuboid and a missing posterior tubercle. The latter is completely sheared off proximal to the posterior talar facet. There are two additional major breaks running through the calcaneal body, but both have been repaired with an unidentified type of glue. The first of these runs in a parasagittal plane and completely separates the peroneal trochlea from the rest of the calcaneal body. The second is approximately coronal in orientation, passing proximal to the sustentaculum tali, but distal to the posterior talar facet (see Figure 1). Given that the second break does not bisect the peroneal trochlea, it is likely that the trochlea was sheared off prior to the second break.

One prominent feature of the A. africanus StW 352 calcaneus is the unusual robusticity of its peroneal trochlea, as has been noted by several authors.2,5,10,11 This robusticity is noteworthy because apes tend to exhibit larger peroneal trochleae than modern humans12, and the peroneal trochlea of an A. afarensis calcaneus also has been described as 'massive'13. The peroneal trochlea is responsible for redirecting the tendons of peroneus longus and peroneus brevis travelling distally from the leg to their insertion in the foot.14 The peroneal trochlea acts as the anchor point for the retinacula surrounding the tendons of these peroneal muscles and, thus, its size has been hypothesised to vary with their size and activity.15

Stern and Susman16 used telemetered electromyographic studies of peroneus longus and peroneus brevis activation in Pan troglodytes and Homo sapiens to suggest that a large peroneal trochlea could have implications for understanding their functional role during bipedal locomotion and/or climbing in Australopithecus. They noted that both peroneal muscles were active during the second half of stance phase in humans, likely used to maintain the forefoot in relative eversion and assist in 'locking' the metatarsal joints while transferring weight medially towards the big toe.16 In P. troglodytes, by contrast, neither peroneal muscle was active during terrestrial quadrupedalism and both seemed to be only variably active during stance phase of bipedalism.16 More recent electromyographic studies of these peroneal muscles have observed activity in chimpanzees similar to that in humans during the last half of stance phase of bipedal gaits.17 By comparison, both peroneal muscles were very active in chimpanzees during stance phase of quadrupedalism on vertical and horizontal simulated arboreal substrates, likely to aid in everting the foot on such supports.16 Stern and Susman16 hypothesised that the large (ape-like) peroneal trochlea in A. afarensis corresponded to large peroneal muscles reflective of a foot being used in an arboreal setting.16

There are disagreements, however, about the degree to which arboreality was practised by Australopithecus.13,18-21 If the size of the peroneal trochlea is correlated to frequent forceful contraction of the peroneal muscles, as has been suggested,5,10,16 its position, size, and form informs in this debate. Given the uniqueness of the enlarged peroneal trochlea on StW 352, and thus its potential relevance for hominin functional morphology, we chose to carefully investigate its structural integrity using high-resolution computed tomography (CT).

Here, we critically evaluate StW 352's structural integrity, noting two issues that would affect current interpretations of the functional morphology of the reconstructed fossil. First, careful visual examination of the external surface of the peroneal trochlea suggests its proximodistal position may be incorrect. Upon close inspection, it appears that the peroneal trochlea has been reattached to the body of the calcaneus in such a way that there is cortical bone overlapping at both the dorsal and distal sides, leaving an artificial void inferior to the peroneal trochlea (see A and B in Figure 2). This malalignment suggests that the true attachment site should be more plantarly and proximally positioned compared to its current position. Second, the central region of the peroneal trochlea shows evidence of having been split and outwardly expanded by matrix infill, which appears to have spuriously augmented the overall robusticity of this anatomy, and its proximodistal dimension in particular (see C and D in Figure 2).

It is not uncommon to find evidence of taphonomic changes to the remains of fossil hominins from Sterkfontein Member 4. Multiple cranial and postcranial specimens from Sterkfontein Member 4 exhibit varying degrees of damage.22-24 For example, many specimens show evidence of carnivore modification (i.e. bite marks), highlighting the important role of carnivores as accumulation agents in these deposits.22 Thus, our suggestion of taphonomic or post-depositional modifications of StW 352 is not unusual for a specimen from Sterkfontein Member 4.

Visual examinations of external surfaces of the fossil were evaluated further using high-resolution CT. Because the objective here was to qualitatively examine structural integrity, specifically whether the trabecular struts and cortical shell within the fossil were correctly realigned, we compared similar high-resolution CT images from two representative extant hominoid calcanei. The comparative sample included an individual adult right calcaneus from a modern human (H. sapiens) and a chimpanzee (P. troglodytes), loaned from the Anthropology Department at Boston University and the Harvard Museum of Comparative Zoology, respectively. A chimpanzee calcaneus was included because chimpanzees represent the closest-living relatives to modern humans and have a peroneal trochlea that forms from a separate ossification site, as may have occurred in hominins with a large peroneal trochlea.15 Chimpanzees also exhibit a generally more robust postcranial skeleton than modern humans, who appear to exhibit systemically lower bone mass, particularly with age.25 Thus, by including the chimpanzee calcaneus, any gross differences in cortical and trabecular bone distribution, particularly those related to potential internal partitioning of the peroneal trochlea from the calcaneal body, generated by differences in the development of this anatomy should be accounted for in the current evaluation.

Image data from StW 352 were acquired using the industrial high-resolution CT scanner at the Evolutionary Studies Institute of the University of the Witwatersrand (Johannesburg, South Africa). Image data from the two comparative calcanei were acquired using the industrial high-resolution CT scanner at Harvard University's Center for Nanoscale Systems (Cambridge, MA, USA). Scan parameters for all specimens are listed in Table 1. Renderings produced from each image data set were sectioned in two planes through the peroneal trochlea in order to visualise the internal organisation: in a coronal plane (A) near its distal edge and in a transverse plane (B) through the dorsal surface (Figure 3). StW 352 was sectioned in a third plane: transversely (C) through the middle of the peroneal trochlea (Figure 4). There is an unusual partition of cortical bone separating the internal cavity of the peroneal trochlea of StW 352 from the internal cavity of the calcaneal body that is absent in the comparative material (A and B in Figure 3), both of which instead exhibit a single continuous internal cavity filled with trabecular struts extending from the lateral region of the calcaneal body into the peroneal trochlea. Section C (Figure 4) highlights the presence of intrusive matrix causing artificial outward (lateral) and proximodistal expansion of StW 352's peroneal trochlea.

The high-resolution image data verify the initial visual examination of the external surface indicating that the peroneal trochlea in StW 352 has not been accurately reconstructed. Rather, it has been reattached to the main body of the calcaneus in an anatomically inaccurate position, and its robusticity (size and form) is at least partly enhanced by the remaining intrusive matrix. Its current form and the existing breakage pattern suggest that the peroneal trochlea must have been sheared away and proximodistally expanded before the coronally oriented break through the mid-body occurred. Some undefined period of time following this, the posterior tubercle appears to have been broken off and never recovered. Upon recovery of the existing fossil, the peroneal trochlea was reattached to the body approximately 5 mm dorso-distally (estimated from microCT image data) from its original anatomical position.

These observations have several implications. First, any future study of StW 352 employing geometric morphometrics, or other shape analysis tools, should compensate for the external displacement of its peroneal trochlea and use caution when commenting on the robusticity of its peroneal trochlea in comparative contexts. Moreover, a detailed digital reconstruction of the specimen would be advisable in order to more accurately reposition the peroneal trochlea and remove the excess matrix. Second, given the seemingly spurious outward expansion and proximodistal displacement observed, the actual size of the peroneal trochlea of StW 352 is likely smaller to an unknown extent and its anatomical position likely more proximal than previously described.2,5,10,11 While correction of its size would lessen the robusticity of the peroneal trochlea to an uncertain precise extent, it would still appear to us to be relatively larger than typical human morphology. Nonetheless, because the size of hominin peroneal trochleae has been hypothesised to correspond with the degree of recruitment of the peroneal muscles,5,16,18,26,27 and because this morphology is rarely preserved in the hominin fossil record, re-evaluation of StW 352 is crucial. Ultimately, we suggest that caution is warranted when using the present form of this bony anatomy on StW 352 to support interpretations of either an increased reliance on arboreal substrates or the peroneal muscles functioning as a possible compensatory mechanism for a less-developed medial arch during striding bipedalism in either this individual or, by extension, within A. africanus in general.

 

Acknowledgements

We thank Dr Jeremy DeSilva for his advice and aid in funding E.J.M.'s travel to South Africa; the Department of Anthropology at Dartmouth College for funding travel for access to the original fossil material and the high-resolution scanning of comparative material in Boston; Dr Bernhard Zipfel and the Evolutionary Studies Institute of the University of the Witwatersrand for allowing access to StW 352 material; the National Research Foundation and the Department of Science and Technology (South Africa), for providing research funds to conduct high-resolution scanning of StW 352; Judy Chupasko and Mark Omura at the Harvard Museum of Comparative Zoology and the Department of Anthropology at Boston University for their assistance in loaning the comparative material. Scanning of comparative material was performed at the Center for Nanoscale Systems (CNS), a member of the National Nanotechnology Coordinated Infrastructure Network (NNCI), which is supported by the National Science Foundation under NSF award no. 1541959. CNS is part of Harvard University.

 

Authors' contributions

The study was conceived by E.J.M. The paper was written by E.J.M. with contributions and revisions by K.J.C. and A.G.C. Project design and data collection were completed by E.J.M., K.J.C. and A.G.C.

 

References

1. Deloison Y. Anatomie des os fossiles de pieds des hominidés d'Afrique du Sud datés entre 2, 4 et 3, 5 millions d'années. Interprétation quant à leur mode de locomotion. [Anatomy of the fossil bones of feet of hominids from South Africa dated between 2.4 and 3.5 million years. Interpretation as to their mode of locomotion]. Biométrie Hum Anthropol. Société de biométrie humaine. 2003;21(3-4):189-230. French.         [ Links ]

2. McHenry HM. Early hominid postcrania: Phylogeny and function. In: Corruccini RS, Ciochon RL, editors. Integrative pathways to the past: Paleoanthropological papers in Honor of F. Clark Howell. Englewood Cliffs, NJ: Prentice-Hall; 1994. p. 251-268.         [ Links ]

3. Pickering R, Kramers JD. Re-appraisal of the stratigraphy and determination of new U-Pb dates for the Sterkfontein hominin site, South Africa. J Hum Evol. 2010;59(1):70-86. https://doi.org/10.1016/j.jhevol.2010.03.014        [ Links ]

4. DeSilva JM, Throckmorton ZJ. Lucy's flat feet: The relationship between the ankle and rearfoot arching in early hominins. PLoS One. 2010;5(12), e14432, 8 pages. https://doi.org/10.1371/journal.pone.0014432        [ Links ]

5. Prang TC. Calcaneal robusticity in Plio-Pleistocene hominins: Implications for locomotor diversity and phylogeny. J Hum Evol. 2015;80:135-146. https://doi.org/10.1016/j.jhevol.2014.09.001        [ Links ]

6. Zeininger A, Patel BA, Zipfel B, Carlson KJ. Trabecular architecture in the StW 352 fossil hominin calcaneus. J Hum Evol. 2016;97:145-58. https://doi.org/10.1016/j.jhevol.2016.05.009        [ Links ]

7. Ahern J. Underestimating intraspecific variation: The problem with excluding Sts 19 from Australopithecus africanus. Am J Phys Anthropol. 1998;105(4):461-480. https://doi.org/10.1002/(SICI)1096-8644(199804)105:4<461::AID-AJPA5>3.0.CO;2-R        [ Links ]

8. Clarke R. Australopithecus from Sterkfontein Caves, South Africa. In: Reed KE, Fleagle JG, Leakey RE, editors. The paleobiology of Australopithecus. New York: Springer; 2013. p. 105-123. https://doi.org/10.1007/978-94-007-5919-0_7        [ Links ]

9. Grine FE, Delanty MM, Wood BA. Variation in mandibular postcanine dental morphology and hominin species representation in Member 4, Sterkfontein, South Africa. In: Reed KE, Fleagle JG, Leakey RE, editors. The paleobiology of Australopithecus. New York: Springer; 2013. p. 125-146. https://doi.org/10.1007/978-94-007-5919-0_8        [ Links ]

10. Deloison Y. A new hypothesis on the origin of hominoid locomotion. In: Meldrum J, Hilton CE, editors. From biped to strider - the emergence of modern human walking, running, and resource transport. New York: Springer; 2004. p. 35-47. https://doi.org/10.1007/978-1-4419-8965-9_3        [ Links ]

11. DeSilva JM. Vertical climbing adaptations in the anthropoid ankle and midfoot: Implications for locomotion in Miocene catarrhines and Plio-Pleistocene hominins [dissertation]. Ann Arbor, MI: University of Michigan; 2008.         [ Links ]

12. Weidenreich F. The external tubercle of the human tuber calcanei. Am J Phys Anthropol. 1940;26:473-487. https://doi.org/10.1002/ajpa.1330260143        [ Links ]

13. Latimer BM, Lovejoy CO, Johanson DC, Coppens Y. Hominid tarsal, metatarsal, and phalangeal bones recovered from the Hadar Formation 1974-1977 Collections. Am J Phys Anthropol 1982;57:701-719. https://doi.org/10.1002/ajpa.1330570412        [ Links ]

14. Palmanovich E, Laver L, Brin YS, Kotz E, Hetsroni I, Mann G, et al. Peroneus longus tear and its relation to the peroneal tubercle: A review of the literature. Muscles Ligaments Tendons J. 2011;1(4):153-160.         [ Links ]

15. Latimer B, Lovejoy CO. The calcaneus of Australopithecus afarensis and its implications for the evolution of bipedality. Am J Phys Anthropol. 1989;78(3):369-386. https://doi.org/10.1002/ajpa.1330780306        [ Links ]

16. Stern Jr JT, Susman RL. The locomotor anatomy of Australopithecus afarensis. Am J Phys Anthropol. 1983;60(3):279-317. https://doi.org/10.1002/ajpa.1330600302        [ Links ]

17. Larson SG, Stern Jr JT. Chimpanzee hind limb muscle activity patterns during bipedal walking [document on the Internet]. Stony Brook, NY: Stony Brook Primate Locomotion Laboratory; 2017 [cited 2017 October 19].         [ Links ] Available from: http://primatelocomotion.org/chimpanzee-bipedalism-project/overview-of-analyzed-results/chimpanzee-hind-limb-muscle-activity-patterns-during-bipedal-walking/#peroneus-longus

18. Susman RL, Stern Jr JT, Jungers WL. Arboreality and bipedality in the Hadar hominids. Folia Primatol. 1984;43(2-3):113-156. https://doi.org/10.1159/000156176        [ Links ]

19. McHenry HM, Berger LR. Body proportions in Australopithecus afarensis and A. africanus and the origin of the genus Homo. J Hum Evol. 1998;35(1):1-22. https://doi.org/10.1006/jhev.1997.0197        [ Links ]

20. Ward CV. Interpreting the posture and locomotion of Australopithecus afarensis: Where do we stand? Am J Phys Anthropol. 2002;119(S35):185-215. https://doi.org/10.1002/ajpa.10185        [ Links ]

21. Green DJ, Gordon AD, Richmond BG. Limb-size proportions in Australopithecus afarensis and Australopithecus africanus. J Hum Evol. 2007;52(2):187-200. https://doi.org/10.1016/j.jhevol.2006.09.001        [ Links ]

22. Pickering TR, Clarke RJ, Moggi-Cecchi J. Role of carnivores in the accumulation of the Sterkfontein Member 4 hominid assemblage: A taphonomic reassessment of the complete hominid fossil sample (1936-1999). Am J Phys Anthropol. 2004;125(1):1-15. https://doi.org/10.1002/ajpa.10278        [ Links ]

23. Lockwood CA, Tobias PV. Morphology and affinities of new hominin cranial remains from Member 4 of the Sterkfontein Formation, Gauteng Province, South Africa. J Hum Evol. 2002;42(4):389-450. https://doi.org/10.1006/jhev.2001.0532        [ Links ]

24. Vrba ES. A new study of the scapula of Australopithecus africanus from Sterkfontein. Am J Phys Anthropol. 1979;51(1):117-129. https://doi.org/10.1002/ajpa.1330510114        [ Links ]

25. Chirchir H, Kivell TL, Ruff CB, Hublin J-J, Carlson KJ, Zipfel B, et al. Recent origin of low trabecular bone density in modern humans. Proc Natl Acad Sci USA. 2015;112(2):366-371. https://doi.org/10.1073/pnas.1411696112        [ Links ]

26. Zipfel B, DeSilva JM, Kidd RS, Carlson KJ, Churchill SE, Berger LR. The foot and ankle of Australopithecus sediba. Science. 2011;333(6048):1417-1420. https://doi.org/10.1126/science.1202703        [ Links ]

27. Harcourt-Smith WEH, Throckmorton Z, Congdon KA, Zipfel B, Deane AS, Drapeau MSM, et al. The foot of Homo naledi. Nat Commun. 2015;6:8432. https://doi.org/10.1038/ncomms9432        [ Links ]

 

 

Correspondence:
Ellison McNutt
Email: Ellison.J.McNutt.GR@Dartmouth.edu

Received: 06 Sep. 2017
Revised: 20 Oct. 2017
Accepted: 26 Oct. 2017

 

 

FUNDING: Dartmouth College; National Research Foundation (South Africa); Department of Science and Technology (South Africa)

Creative Commons License All the contents of this journal, except where otherwise noted, is licensed under a Creative Commons Attribution License