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From footprints to locomotor anatomy? The contribution of geometric morphometrics to the study of the hominin footprints from the Upper Pleistocene site of Rozel (Normandie, France)

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HAL Id: hal-03000249

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Submitted on 11 Nov 2020

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From footprints to locomotor anatomy? The

contribution of geometric morphometrics to the study of the hominin footprints from the Upper Pleistocene site

of Rozel (Normandie, France)

Jérémy Duveau, Gilles Berillon, Gilles Laisné, Christine Verna, Dominique Cliquet

To cite this version:

Jérémy Duveau, Gilles Berillon, Gilles Laisné, Christine Verna, Dominique Cliquet. From footprints to locomotor anatomy? The contribution of geometric morphometrics to the study of the hominin footprints from the Upper Pleistocene site of Rozel (Normandie, France). International Union of the Prehistoric and Protohistoric Sciences Congress, Jun 2018, Paris, France. �hal-03000249�

(2)

From footprints to locomotor anatomy?

The contribution of geometric morphometrics to the study of the hominin footprints

from the Upper Pleistocene site of “Le Rozel” (Normandie, France)

Jérémy Duveau1, Gilles Berillon1, Gilles Laisné2, Christine Verna1 & Dominique Cliquet2 .

jeremy.duveau@mnhn.fr

1CNRS UMR 7194 Histoire Naturelle de l'Homme Préhistorique, Département Homme et environnement, Muséum national d'Histoire naturelle, France, Paris

2Direction Régionale des Affaires Culturelles, Normandie, France. PCR "Les Premiers Hommes en Normandie"

XVIIIe world UISPP Congress (4th-9th June 2018)

Results

What anatomical information about the “Le Rozel” hominins is it possible to obtain from the morphometric study of their footprints?

➢Comparative geometry morphometrics analysis of the “Le Rozel” footprints with experimental and fossil footprints

Issue & Aim

References:

Bennett, M.R., Harris, J.W., Richmond, B.G., Braun, D.R., Mbua, E., Kiura, P., Olago, D., Kibunjia, M., Omuombo, C., Behrensmeyer, A.K., others, 2009. Early hominin foot morphology based on 1.5- million-year-old footprints from Ileret, Kenya. Science. 323, 1197–1201.

Mercier, N., Martin, L., Kreutzer, S., Moineau, V., Cliquet, D., 2017. Dating the palaeolithic footprints of « Le Rozel » (Normandy, France). Quaternary Geochronology.

Hominin footprints represent a unique snapshot of a moment in the life of extinct individuals. In addition to the original information they may provide about group composition, many authors have taken an interest about the anatomical information they can reveal by benefiting from the development of new recording techniques and 2D/3D morphometric studies. We report here a morphometric study of 8 human footprints recently discovered at the Middle Palaeolithic site of Le Rozel (Normandie, France)

Methods

Procustes analysis 1

Landmarks’ position

Principal Component

Analysis 3

2

Procustes analysis

Material

8 3D models of «Le Rozel » footprints coming from a single stratigraphic unit compared to models of footprints made in various ground natures by different hominin species.

Using 11 landmarks that represent the foot outline (1-9) and maximum depth points (10-11) based on Bennett et al., 2009:

1-2 : Longitudinal axis of the footprint 3-4 : Maximal width of the heel

5-6 : Minimal width of the midfoot 7-8 : Maximal width of the forefoot 9 : Distal inflection point of the hallux 10 : Maximal depth of the heel

11 : Maximal depth of the forefoot

Le Rozel

« Le Rozel » hominin footprints (photos: D. Cliquet)

Levallois flakes (A) and a deer’s lower jaw (B) discovered in “Le Rozel”

(photos : D. Cliquet) A

B

The archaeological site of « Le Rozel »

▪ Discovered during the early 60’s

▪ New excavations since 2012

▪ Located in a paleodune system

▪ Several occupation layers having delivered a rich archaeological material (faunal remains, lithic industries, charcoals…) attesting to several Neandertal occupations 80 000 years ago (Mercier et al., 2017)

▪ Discovery of 290 hominin footprints since 2012 made in muddy flows covering sandy elements

Acknowledgements:

We particularly thank the British Museum for the free access of the Happisburgh footprint 3D model. We especially thank M. Bennett (University of Bournemouth) and S. Menconero (Sapienza University of Rome) for the Laetoli footprint scans.

This study was realized thanks to a doctoral fellowship (Muséum national d’Histoire naturelle). The archaeological excavations at Le Rozel were possible thanks to government funding and funding from the department of La Manche. The analysis of experimental footprints enabled thanks to IRN Bipedal Equilibrum funding.

H. sapiens

Le Rozel

Happisburgh Laetoli

Mean footprint shape

The locations of the maximum depth areas of the heel and the forefoot are similar to Homo sapiens footprints. Besides, the adduction of the hallux is identical to anatomically modern footprints.

However, 2 main differences with H. sapiens :

➢ A slightly wider heel

➢ A wider midfoot reflecting a less pronounced plantar vault than for Homo sapiens

Morphometric analysis have shown that Le Rozel footprints differ from Homo sapiens footprints, reflecting anatomical features such as a wider heel or a less pronounced plantar vault. These anatomical features of Le Rozel footprints are consistent with our knowledge of the anatomy of the Neandertal foot. Ongoing analyses of the impact of taphonomic

agents on the footprints’ morphology will help improving our interpretation of Le Rozel footprints. A Neandertal foot : La Ferrassie 2

(photo : G. Berillon with the permission of the Musée de l’Homme)

One of the

experimental footprint

(photo: J. Duveau)

Site Period Associated taxon Depositional settings

Number of footprints

Number of individuals Experimental1 H. sapiens Nearby the site in

a similar sediment 46 20

Le Rozel1 Upper

Pleistocene H. neanderthalensis Sand/Sandy mud 8 8 Happisburgh2 Lower

Pleistocene H. antecessor Silt 1 1

Laetoli2 Pliocene Au. afarensis Volcanic Tuf 17 3 (G1, S1, S2)

Principal Component Analysis (PCA)

PCA analyses show that « Le Rozel » footprints differ on average from the other footprints. They are closest to the anatomically modern footprints.

13D surfaces digitized in situ

23D surfaces from a freely accessible database

Références

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