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Featured researches published by Anne Dambricourt Malassé.


Quaternary International | 1993

Continuity and discontinuity during hominization

Anne Dambricourt Malassé

Abstract Recent observations on an ontogenetic craniofacial phenomenon have led to new concepts of facial morphogenesis and to recognition of a process called craniofacial contraction. This begins at embryogenesis, in association with the growth of the brain. The degree of craniofacial contraction is acquired in major part during embryogenesis. It separates the living primates into four ontogenic levels: prosimians, monkeys, apes and Homo sapiens (‘Sapiens’). The phenomenon is modeled and quantified using an architectural analysis, the double pantograph. The hypothesis is that hominization represents a continous phenomenon from fossil apes to Sapiens, i.e. an increase in the embryonic contraction, but with discontinous effects, i.e. ontogenic organization plans. The fossil hominid record verifies the hypothesis. Hominization appears as a continuous process of craniofacial contraction, with three ontogenic thresholds: Australopithecus, Homo and Sapiens. Neanderthal man is not Sapiens. He results from a decrease in the embryonic contraction of Homo erectus , in association with an impoverishment of the meningeal vascularization. Sapiens does not emerge before skulls such as Qafzeh. The increase in endocranial capacity in Homo does not alone allow us to define an evolutionary trend in Sapiens. The concept of archaic H. sapiens has no ontogenic reality.


Acta Biotheoretica | 1995

Les Attracteurs Inedits de l'hominisation

Anne Dambricourt Malassé

The recent discovery of a phenomenon of craniofacial growth, called craniofacial contraction, throws a new light on the process of hominization. The main interest of this discovery lies in a growth principle combining the different craniofacial units, that is to say, the neurocranium (neural skull), the chondrocranium (basal skull) and the splanchnocranium (visceral archs including the mandible). Until recent years, these different parts were considered as neighbouring element without any morphogenic or morphodynamic connection. But now, we know that the morphogenesis of the base of the skull governs that of the face. This basicranial morphogenesis is the occipital flexion. It generates morphogenic correlations with the face since embryogenesis. The ontogenic pathway of this phenomenon is the craniofacial contraction. It concerns embryonic dynamics connected with the spatial development of the embryonic neural system, the neural tube. These morphodynamics are common to each primate species, but they are differenciated by the amplitude of the embryonic contraction. We ask ourself the question: is hominization of the neurocephalic embryogenesis, that is the craniofacial contraction, plausible over a very long period, with gradual and chaotic evolutionary pathways, or, on the contrary, is the complexity of such an embryonic phenomenon, a limiting factor generating determined and predictible ontogenic thresholds? The study of extant and fossil primate skulls demonstrates that species are organized around 6 levels of embryonic contraction, which, starting from 60 millions years, evolve from the less to the most contracted skull. Among each ontogenic level, living and fossil species develop from the same embryonic system but between both levels, the embryos suddenly are reorganized. Therefore, I have defined an evolutive ontogenic unity, that is the fundamental ontogenesia. The cephalic pole has a fundamental ontogenesis, meaning that, beyond the diversities, we can see the same contraction in many living and extinct species. The ontogenic diversities are the result of the microevolution and are not predictible. In such a perspective, the ontogenic morphodynamics evolve with chaotic trajectories. But, between two embryonic levels, or two fundamental ontogeneses, evolutionary modalities are different. Eventually, from 60 millions years to XXth century, we observe the same phenomenon than during human ontogenesis; hominization of the cephalic pole is a craniofacial contraction. The evolutive pathway is stable, whatever the number of thresholds, the cranial shape changes but the ontogenic trajectory is preserved. This is a macroevolution because the embryonic system is reorganized. The logics of the phenomenon are an increasing dynamization, the human ontogenesis is the more unstable and the longer morphodynamics to stabilize the craniofacial contraction. To conclude, hominization is an iteration of an ontogenic process when embryos reach successive dynamic thresholds. The attractors are neither static, periodic, nor chaotic because the successive ontogenic trajectories are themselves in a stable evolutive trajectory, and the results with increasing contraction, complexified neocortical tissues and cephalocaudal reorganization are predictible. During hominization, irreversibility and innovations do not emerge with chaotic determinism, but with harmonic determinism in association with the correlations established between the embryonic tissues. When the system is destabilized, the embryonic systems do not forget the previous ontogenic pattern, on the contrary, they develop the pattern with new dynamical conditions. This sort of phenomenon is not described in the sciences of complexity. In the present case, we are in front of many millions years and the necessity to propose new concepts such as a new familly of attractors, namely the harmonic attractors.The recent discovery of a phenomenon of craniofacial growth, called craniofacial contraction, throws a new light on the process of hominization. The main interest of this discovery lies in a growth principle combining the different craniofacial units, that is to say, the neurocranium (neural skull), the chondrocranium (basal skull) and the splanchnocranium (visceral archs including the mandible). Until recent years, these different parts were considered as neighbouring element without any morphogenic or morphodynamic connection. But now, we know that the morphogenesis of the base of the skull governs that of the face. This basicranial morphogenesis is the occipital flexion. It generates morphogenic correlations with the face since embryogenesis. The ontogenic pathway of this phenomenon is the craniofacial contraction. It concerns embryonic dynamics connected with the spatial development of the embryonic neural system, the neural tube. These morphodynamics are common to each primate species, but they are differentiated by the amplitude of the embryonic contraction. We ask ourself the question: is hominization of the neurocephalic embryogenesis, that is the craniofacial contraction, plausible over a very long period, with gradual and chaotic evolutionary pathways, or, on the contrary, is the complexity of such an embryonic phenomenon, a limiting factor generating determined and predictable ontogenic thresholds? The study of extant and fossil primate skulls demonstrates that species are organized around 6 levels of embryonic contraction, which, starting from 60 millions years, evolve from the less to the most contracted skull. Among each ontogenic level, living and fossil species develop from the same embryonic system but between both levels, the embryos suddenly are reorganized. Therefore, I have defined an evolutive ontogenic unity, that is the fundamental ontogenesis. The cephalic pole has a fundamental ontogenesis, meaning that, beyond the diversities, we can see the same contraction in many living and extinct species. The ontogenic diversities are the result of the microevolution and are not predictable. In such a perspective, the ontogenic morphodynamics evolve with chaotic trajectories. But, between two embryonic levels, or two fundamental ontogeneses, evolutionary modalities are different. Eventually, from 60 millions years to XXth century, we observe the same phenomenon than during human ontogenesis; hominization of the cephalic pole is a craniofacial contraction. The evolutive pathway is stable, whatever the number of thresholds, the cranial shape changes but the ontogenic trajectory is preserved. This is a macroevolution because the embryonic system is reorganized.(ABSTRACT TRUNCATED AT 400 WORDS)


Comptes Rendus De L Academie Des Sciences Serie Ii Fascicule A-sciences De La Terre Et Des Planetes | 1998

Quantification de révolution morphologique du crâne des Hominidés et hétérochronies

Jean Chaline; Bruno David; Françoise Magniez-Jannin; Anne Dambricourt Malassé; Didier Marchand; Frédéric Courant; Jean-Jacques Millet

Abstract Comparisons of adult skulls of various species of great apes, fossil hominids and modern humans in the sagittal, Francfort and ortho-sagittal planes reveal a series of three separate organisation plans: ‘Great Ape’, ‘Australopithecine’ and ‘Homo’, the latter including primitive men ( Homo ergaster-erectus-neandertalensis ) and modern humans ( Homo sapiens ). Morphological changes between these plans are quantified for the first time here by vector fields. This study confirms the existence of cranio-facial contraction, which occurs as a series of leaps. The juvenile morphology of the great ape skull is broadly preserved in adult Homo sapiens, suggesting that numerous heterochronies have occurred in mosaic during ontogeny (hypermorphosis, hypomorphosis, post-displacements).


Comptes Rendus Palevol | 2016

Intentional cut marks on bovid from the Quranwala zone, 2.6 Ma, Siwalik Frontal Range, northwestern India

Anne Dambricourt Malassé; Anne-Marie Moigne; Mukesh Singh; Thomas Calligaro; Baldev Karir; Claire Gaillard; Amandeep Kaur; Vipnesh Bhardwaj; Surinder Pal; Salah Abdessadok; Cécile Chapon Sao; Julien Gargani; Alina Tudryn; Miguel Garcia Sanz


Quaternary International | 2011

Late Pleistocene to Early Holocene Lithic industries in the southern fringes of the Himalaya

Claire Gaillard; Mukesh Singh; Anne Dambricourt Malassé


Comptes Rendus Palevol | 2016

Anthropic activities in the fossiliferous Quranwala Zone, 2.6 Ma, Siwaliks of Northwest India, historical context of the discovery and scientific investigations

Anne Dambricourt Malassé; Mukesh Singh; Baldev Karir; Claire Gaillard; Vipnesh Bhardwaj; Anne-Marie Moigne; Salah Abdessadok; Cécile Chapon Sao; Julien Gargani; Alina Tudryn; Thomas Calligaro; Amandeep Kaur; Surinder Pal; Manjil Hazarika


Comptes rendus de l’Académie des sciences. Série IIa, Sciences de la terre et des planètes | 1997

Quantification de l'évolution morphologique du crâne des Hominidés et hétérochronies

Jean Chaline; Bruno David; Françoise Magniez-Jannin; Anne Dambricourt Malassé; Didier Marchand; Frédéric Courant; Jean-Jacques Millet


Comptes Rendus Palevol | 2016

Stratigraphy and paleoenvironment during the Late Pliocene at Masol paleonto-archeological site (Siwalik Range, NW India): Preliminary results

Alina Tudryn; Salah Abdessadok; Julien Gargani; Anne Dambricourt Malassé; Claire Gaillard; Anne-Marie Moigne; Cécile Chapon Sao; Mukesh Singh; Vipnesh Bhardwaj; Baldev Karir; Serge Miska


Comptes Rendus Palevol | 2016

The faunal assemblage of the paleonto-archeological localities of the Late Pliocene Quranwala Zone, Masol Formation, Siwalik Range, NW India

Anne-Marie Moigne; Anne Dambricourt Malassé; Mukesh Singh; Amandeep Kaur; Claire Gaillard; Baldev Karir; Surinder Pal; Vipnesh Bhardwaj; Salah Abdessadok; Cécile Chapon Sao; Julien Gargani; Alina Tudryn


Comptes Rendus Palevol | 2016

The first Indo-French Prehistorical Mission in Siwaliks and the discovery of anthropic activities at 2.6 million years

Anne Dambricourt Malassé

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Claire Gaillard

Centre national de la recherche scientifique

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Mukesh Singh

Guru Nanak Dev University

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Cécile Chapon Sao

Centre national de la recherche scientifique

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Salah Abdessadok

Centre national de la recherche scientifique

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Alina Tudryn

University of Paris-Sud

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Bruno David

University of Burgundy

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