47,117 research outputs found
Les conflits de motivation
No full textde Bonis M. Les conflits de motivation. In: L'année psychologique. 1966 vol. 66, n°1. pp. 289-305
La loi de Yerkes-Dobson : problèmes méthodologiques liés à sa vérification
No full textde Bonis M. La loi de Yerkes-Dobson : problèmes méthodologiques liés à sa vérification. In: L'année psychologique. 1968 vol. 68, n°1. pp. 121-141
Mustelictis olivieri Bonis 1997
No full text<i>Mustelictis</i> aff. <i>olivieri</i> Bonis, 1997 <p>(Figs 4 C-E, G; 5F)</p> <p>TYPE SPECIMEN. — Holotype: skull, UP MGB60, by author designation; paratype: hemi-mandible, UP MGB 7.</p> <p>NEW MATERIAL. — Left m1, LPL11; left fragment of hemi-mandible, UP LPL12; right m1, UM VBOA 3-4; fragment of right hemi-mandible p2-p4, UM VD 12; left P4, VBO 494.</p> <p>REMARKS</p> <p>The holotype and paratype of the species come from Mas de Got (MP 22). A skull and a hemi-mandible (paratype) were figured by Bonis (1997: figs 1, 2). New research has recovered additional specimens in other localities.</p> <p>DESCRIPTION</p> <p>The premolars are present in UP LPL12 and UM VD12 and all of them have cutting mesial and distal edges. The p2 is dissymmetric, the mesial part being smaller than the distal</p> <p> one and having a more sloping mesial edge, the distal one finishing by a small upturned spur at its base. The p3, less dissymmetric than p2, displays a mesial spur; distally there is a small talonid with a small fovea surrounded by a low cristid; there is also a small pacd at mid-height on the distal edge (Fig. 4G 1, G 2). The p4 is similar to p3 but is larger. The carnassial is very similar to that of the type of <i>M</i>. <i>olivieri</i> but the talonid is less narrow. The m2 is larger than in the type in both absolute size and relative to m1; it has a complete trigonid with high protoconid and metaconid and small but clear paraconid, and a narrow talonid (Fig. 4B). The isolated P4 (VBO 494) figured by Peigné <i>et al.</i> (2014: fig. 22a) is close to that of the type specimen from Mas de Got, with a mesio-lingually elongate protocone finishing by a conic cusp, a buccal cingulum and a small mesial bulging representing a parastyle (Fig. 5F). These remains are close to the material of <i>M</i>. <i>olivieri</i> (Fig. 4F 1, F 2) but the small differences lead us to be cautious about the identification. They could be due to a small difference in the geological age between two localities of MP 22.</p>Published as part of <i>Bonis, Louis de, Gardin, Axelle & Blondel, Cécile, 2019, Carnivora from the early Oligocene of the ' Phosphorites du Quercy' in southwestern France, pp. 601-621 in Geodiversitas 41 (15)</i> on pages 614-615, DOI: 10.5252/geodiversitas2019v41a15, <a href="http://zenodo.org/record/3694209">http://zenodo.org/record/3694209</a>
Filholictis Bonis 2013, n. gen.
No full textFilholictis n. gen. TYPE AND UNIQUE SPECIES. — Canis filholi Munier- Chalmas in Filhol, 1877 by original designation. DERIVATIO NOMINIS. — Dedicated to H. Filhol who published many Quercy fossils. DIAGNOSIS. — Same as that of the type species. Filholictis filholi (Munier-Chalmas in Filhol, 1877) Canis filholi Munier-Chalmas in Filhol, 1877: 319, figs 123, 124. — Beaumont 1965: 23. Cephalogale filholi – Schlosser 1888: 103; 1904-1905: 293. — Bonis 1973: 82. HOLOTYPE. — Mandible figured by Filhol (1877: figs 123, 124); (MNHN.F.nn). DIAGNOSIS. — Primitive middle sized Cephalogalini n.tr. differing from the Amphicynodontidae by the large lower carnassial relative to the premolars and from the other Cephalogalini n. tr. by a less reduced metaconid of m 1 in contact with the paraconid and closing the central valley of the trigonid. High lower premolars without pacd, p3 as tall as p4 both being higher than the paraconid of m1; m2 relatively short for a Hemicyoninae, paraconid present but metaconid more developed than the protoconid. TYPE LOCALITY. — Unknown, “Phosphorites du Quercy ”. GEOLOGICAL AGE. — Unknown but probably Oligocene. Phoberogale Ginsburg & Morales, 1995 DIAGNOSIS. — Medium sized to large Cephalogalini n. tr., low and elongated P2-P3 and p2-p4, p2-p4 with developed pacd, robust cingula and cingulids in all the cheek teeth. TYPE SPECIES. — Cephalogale depereti Viret, 1929 by original designation. OTHER SPECIES. — P. gracile (Viret, 1929); P. bonali (Helbing, 1928); P. minor (Filhol, 1877). Filholictis filholi (Munier-Chalmas in Filhol, 1877) Canis filholi Munier-Chalmas in Filhol, 1877: 319, figs 123, 124. — Beaumont 1965: 23. Cephalogale filholi – Schlosser 1888: 103; 1904-1905: 293. — Bonis 1973: 82. HOLOTYPE. — Mandible figured by Filhol (1877: figs 123, 124); (MNHN.F.nn). DIAGNOSIS. — Primitive middle sized Cephalogalini n.tr. differing from the Amphicynodontidae by the large lower carnassial relative to the premolars and from the other Cephalogalini n. tr. by a less reduced metaconid of m 1 in contact with the paraconid and closing the central valley of the trigonid. High lower premolars without pacd, p3 as tall as p4 both being higher than the paraconid of m1; m2 relatively short for a Hemicyoninae, paraconid present but metaconid more developed than the protoconid. TYPE LOCALITY. — Unknown, “Phosphorites du Quercy ”. GEOLOGICAL AGE. — Unknown but probably Oligocene. Phoberogale Ginsburg & Morales, 1995 DIAGNOSIS. — Medium sized to large Cephalogalini n. tr., low and elongated P2-P3 and p2-p4, p2-p4 with developed pacd, robust cingula and cingulids in all the cheek teeth. TYPE SPECIES. — Cephalogale depereti Viret, 1929 by original designation. OTHER SPECIES. — P. gracile (Viret, 1929); P. bonali (Helbing, 1928); P. minor (Filhol, 1877). Phoberogale Ginsburg & Morales, 1995 DIAGNOSIS. — Medium sized to large Cephalogalini n. tr., low and elongated P2-P3 and p2-p4, p2-p4 with developed pacd, robust cingula and cingulids in all the cheek teeth. TYPE SPECIES. — Cephalogale depereti Viret, 1929 by original designation. OTHER SPECIES. — P. gracile (Viret, 1929); P. bonali (Helbing, 1928); P. minor (Filhol, 1877).Published as part of Bonis, Louis De, 2013, Ursidae (Mammalia, Carnivora) from the Late Oligocene of the " Phosphorites du Quercy " (France) and a reappraisal of the genus Cephalogale Geoffroy, 1862, pp. 787-814 in Geodiversitas 35 (4) on page 790, DOI: 10.5252/g2013n4a4, http://zenodo.org/record/453814
Psychophysiologie et psychologie animale
No full textde Bonis M., Botte M.-C., Thierry B., Goldblum M.-C. Psychophysiologie et psychologie animale. In: L'année psychologique. 1985 vol. 85, n°2. pp. 290-298
Raw materials for ancient ceramic productions from Campania region: provenance studies by means of Sr-Nd isotopes
No full textWhen archaeometric studies on archaeological ceramics are performed, one of the most important questions
asked by archaeologists is the provenance of pottery. This is usually performed by comparing mineropetrographic
and chemical composition of ceramics with that of local raw materials (clays, temper), production
indicators and appropriate reference groups. Nevertheless, the commonly-used analytical techniques (e.g. OM,
SEM-EDS, XRF, ICP-MS) may not always be helpful for the determination of provenance. Indeed, processing
of raw materials, such as tempering or levigation, can significantly modify their original chemical composition,
sometimes leading to an ineffective identification of raw material resources. For this reason, a pioneering
analytical approach has been recently applied by measuring the Sr and Nd isotopic signature.
Isotope analysis has largely used in archaeological sciences to date objects and identify their provenance,
making it also a useful tool for the determination of provenance of ceramic vessels (De Bonis et al., 2018 and
references therein). For this study, 87Sr/86Sr and 143Nd/144Nd isotope ratios were measured on archaeological
pottery from Campania and raw materials (clays and volcanic temper) exploited in antiquity for producing
ceramics. The analyses were focused on samples from both the Bay of Naples and Southern Campania. The
isotope signatures allowed us to better discriminate among different productions and find a strong relationship
between the archaeological pottery and the geological sources of raw materials.
In order to validate the method, Sr-Nd isotope ratios were also measured for the first time on experimental
ceramic materials that replicate archaeological pottery (De Bonis et al., 2018). It was interesting to note that
synthetic mixtures used for the ceramic replicas plot exactly on the theoretical mixing curve between the
clay and volcanic temper end-members. This suggests that the artificial manipulation of raw materials (firing,
levigation, tempering) induces no significant variations to the Sr-Nd isotope fingerprint, which strictly depends
on the geochemical affinity of the raw materials. Thus, isotopic analysis can be considered as an effective
and robust method that could complement the common multi-analytical approach in order to more precisely
constrain potential geological sources for ceramic materials and pottery provenance.
De Bonis, A., Arienzo I., D’Antonio, M., Franciosi, L., Germinario, C., Grifa, C., Guarino, V., Langella, A. & Morra, V.
(2018): Sr-Nd isotopic fingerprint as a tool for ceramic provenance: application on raw materials, ceramic replicas and
ancient pottery. J. Archaeol. Sci., 94, 51-59
Psychologie clinique et pathologique
No full textDoron R., de Bonis M., Marbeau-Cleirens B. Psychologie clinique et pathologique. In: L'année psychologique. 1984 vol. 84, n°3. pp. 469-472
Psychologie clinique et pathologique
No full textDoron R., de Bonis M., Marbeau-Cleirens B. Psychologie clinique et pathologique. In: L'année psychologique. 1984 vol. 84, n°3. pp. 469-472
Constantin M. Mponès (Bonis), Βασιλειὸς Καισαρείας ὁ Μέγας. Βίος καὶ ἔργα, συγγράμματα και διδασκαλία
No full textConstantin M. Mponès (Bonis), Βασιλειὸς Καισαρείας ὁ Μέγας. Βίος καὶ ἔργα, συγγράμματα και διδασκαλία. In: Revue des études byzantines, tome 34, 1976. p. 359
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