Les cabanes de type « Anosovka-Mézine » du site de Yudinovo : éléments de construction,architecture, classification

The study is focused on comparative analysis of the five dwellings of the Anosov-Mezin type from the East-Epigravettian site of Yudinovo (Bryansk region, Russia). The analysis is based on data on previously unknown structural elements and methods of installation of mammoth skulls in the basement of dwelling N^o 5, which were revealed during excavations in 2015–2018. Apart of this the non-utilitarian actions that accompanied the process of dwellings construction was considered. Based on the revealed differences in structural elements and features, it was suggested that the currently used concept Anosovka-Mezin type of dwellings includes two types of the circular structures made of skulls and large mammoth bones.     

Valbro : un nouveau site à vertébrés de l’Oligocène inférieur (MP 22) de France (Quercy). II – Oiseaux (Aves)

The bird remains from Valbro belong only to three taxa, Paraortyx lorteti, Archaeotrogon venustus, and A. zitteli. This association makes it possible to ascribe to this locality an early Oligocene age, reference-levels MP 22 or MP 23, which is in agreement with the age given by the mammals.     

Une histoire de géométrie et de finesse (ou : comment parler de phylogénétique ?)

The development of phylogenetic methods since the beginning of the 1970s is analyzed through Armand de Ricqlès’ comment, in 1975, on the triumph of the spirit of geometry over the spirit of finesse. Cladistics was then compared to geometry (Hennig's congruence [i.e. congruent character-state trees]). However, the qualitative aspect of anatomy (spirit of finesse) warrants the quality of a taxon × character matrix so that minimal length trees were never devoid of finesse. Statistical approaches, especially maximum likelihood and Bayesian methods, with sophisticated mathematics (more rigorous geometry?), have reached a wide acceptance after years of debates hindered by polemics. The molecular trees based on these approaches are now dominating the phylogenetic literature, although these trees too include some ambiguity so that one can wonder: do evolutionary models belong to geometry or finesse?     

Le cancer différencié de la thyroïde chez les patients de moins de 20 ans : à propos de 20 cas

Papillary thyroid cancer is rare in patients under 20 years and has a good prognosis, although it is often found at the stage of lung metastases. Our multicenter study included 20 patients aged between 5 and 18 years, female predominance, followed for differentiated thyroid cancer with lung metastases. All these patients underwent a whole body scan with I-131, serum thyroglobulin, chest radiography in 4 cases and cervico-thoracic (CT) in 5 cases. Only scintigraphic imaging has shown miliary pulmonary among all patients. The therapeutic efficacy was observed in all patients after treatment with iodine-131, which proves the high sensitivity of these metastases to irathérapie. The differentiated thyroid cancer in child and adolescent is characterized by local aggressiveness and a higher frequency of distant metastases than in the adult. Prognosis does not seem to be influenced by histology alone, but by its association with other prognostic factors: age, metastases and surgery.     

Contexte géographique et géologique du site de Kocabaş, Bassin de Denizli,Anatolie, Turquie

The site of Kocaba? is located in the Denizli Basin, in western Anatolia, 400 km southwest of Ankara, 360 km south of Istanbul, 200 km east-southeast of Izmir and 150 km northwest of Antalya. The Denizli Basin depression, at the junction of the Buyuk Menderes and Gediz grabens, which began to form at the beginning of the Miocene, was filled in around the edges, along fault lines, by significant travertine formations, some of which are still active today. The age of the Kocaba? travertines, which yielded the Kocaba? Homo erectus skullcap, was evaluated by thermoluminescence at 828,000 years, by electron spin resonance (ESR) at 1,110,000 years and by the ²⁶Al/¹⁰Be cosmogenic nuclide method to more than 1.22 Ma and less than 1.5 Ma, a date which has been confirmed by magnetostratigraphy and biochronology.     

Una nueva especie de <Emphasis Type="Italic">Pseudomiltemia</Emphasis> (Rubiaceae) de Chiapas,México

Pseudomiltemia davidsonii is described and illustrated as a new endemic species from the Sierra Madre of Chiapas, Mexico. It is a shrub or small tree characterized by having flowers axillary and solitary or in monochasia and with large yellow corollas. Pseudomiltemia davidsonii differs from P. filisepala, the only other species in this genus, by its opposite leaves with longer petioles, inflorescences with shorter peduncles 5–13 mm long, smaller bracts, longer pedicels 6–15 mm long, and narrower fruits 3.5–4.5 mm in diameter.     

Structure d'adhérencedes grains de pollen en tétrade du genre Classopollis PFLUG, 1953, de l'Hettangien de Saint-Fromont,Manche (France)

Palynological inventory of Saint-Fromont pit 0815 (Manche, France) related to Hettangian seems to show the conspecificity of Classopollis chateaunoviReyre, 1970, Classopollis kieseriReyre, 1970 and Classopollis harisiiMuir & Van Konijnenburg-Van Cittert, 1970. SEM pictures exibit some sculptural elements interpreted as structural attachments of grains in tetrad and compared to those of genus DicheiropollisTrevisan, 1971.     

Études stratigraphique,sédimentologique et paléomagnétique des travertins de Kocabaş, Bassin de Denizli,Anatolie, Turquie,contenant des restes fossiles quaternaires

Stratigraphic, sedimentological and paleomagnetic studies were conducted on the travertine from Denizli Basin, near Kocabas village, in the Denizli region in Turkey, following the paleontological discovery in 2002. The stratigraphic and sedimentological studies show at least two main cycles of mass travertine, separated by a fluvial deposit and overlain by a fluvio-lacustrine deposit. These travertines must have formed in environments with strong hydrodynamics (streams or waterfalls) and are preferentially located at breaks of slopes. The paleomagnetic study shows that all the quarry travertine presents reverse magnetic polarity. On the other hand, the detrital fluvio-lacustrine deposit above the travertine presents normal geomagnetic polarity, except at the top, where it is reversed. Given the presence of an archaic Homo erectus skull and Villafranchian paleontological remains in the upper travertine unit, the whole travertine dates from the upper Matuyama, and is more recent than the Olduvai event (1.78 Ma). The normal polarity recorded in the upper fluvio-lacustrine deposit could correspond to the Cobb Mountain excursion, dated to 1.22 Ma.     

Una nueva especie de Chusquea (Poaceae: Bambusoideae) de la Cordillera de Mérida, Venezuela

A new species of woody bamboo (Poaceae: Bambusoideae),Chusquea guirigayensis, is described and illustrated. This species is placed inChusquea sect.Swallenochloa (McClure) L. G. Clark because of its shrubby habit, short waxy internodes, intravaginal branching, and linearly arranged subsidiary buds/branches. In addition, we discuss related species, and describe the ecology and distribution of the new species. Separate keys based on sterile and fertile material of the Venezuelan species ofC. sect.Swallenochloa are provided.     

Temps et réseaux de l’art paléolithique : la grotte de La Covaciella (Asturies,Espagne)

The study of graphic convergences and divergences in Palaeolithic art is used to understand the culture, territories and interaction systems of human groups. La Covaciella cave has fifteen animal representations and other linear, dots and geometric motifs. The bison stands out; some were executed with complex technical procedures. Two of them were dated by C14 AMS, obtaining a result of 14,260 ± 130 BP (17,733–16,973 cal BP) and 14,060 ± 140 BP (17,503–16,260 cal BP). These correspond chronologically with the beginning of the middle Magdalenian or the very end of the lower Magdalenian. Similar depictions to the bison at La Covaciella are located in other areas of Western Europe. The repertoire of parietal bison displaying graphic similarities with those at La Covaciella is very large; both of the Pyrenean model (Niaux morphotype) and of the Perigordian model (Font-de-Gaume morphotype). A first consideration derived from the search for comparisons involves a new interpretation of the territorial value implied by the term Pyrenean style (Asturias, Cantabria, Basque Country, Navarre, Pyrénées-Atlantiques, Hautes-Pyrénées, Haute-Garonne, Ariège, Dordogne, Lot, Ardèche and Vienne). The Font-de-Gaume parietal morphotype is most common in Dordogne. In addition, in some cases, spatial complementariness has been found, with both graphic morphotypes. This article proposes different chronological and anthropological hypothesis to explain the distribution and coexistence of the two graphic models.     

Conclusion. Bilan des recherches interdisciplinaires effectuées sur le site de l’Homo erectus de Denizli,Kocabaş, Bassin de Denizli,Anatolie, Turquie. L’Homo erectus aux portes de l’Europe

The study of the site of Kocaba?, which yielded an archaic Homo erectus skullcap, was undertaken in 2011 and 2012, at the request of Professor Mehmet Cihat Alçiçek. This interdisciplinary French–Turkish research programme comprised the geochronological, magnetostratigraphic, biochronological and paleoenvironmental study of the site and the paleoanthropological study of the skullcap itself. The association of large mammals enabled us to attribute the travertine formations bearing the skullcap to the second part of the Upper Pleistocene, and more specifically to between 1.5 and 1.2 million years, because of the disappearance or appearance of certain species. This biochronological age is confirmed by the paleomagnetism study, which places the travertines bearing the skullcap in a period of reversed polarity, underlying a normal polarity formation, which could be attributed to the Cobb Mountain paleomagnetic excursion, dated to 1,194,000 years. The dating of these fauna by the ²⁶Al/¹⁰Be cosmogenic nuclide method by Anne-Elisabeth Lebatard yielded an age older than 1.22 Ma and more recent than 1.5 Ma. The Hominid skullcap from this formation can be attributed to a Homo erectus, slightly more evolved than those of Homo ergaster KNM-ER 3733 (1.78 Ma) and KNM-ER 15,000 (1.5 Ma), similar to that of Daka (Bouri), which is about a million years old and older than the Bodo fossil (estimated at 600,000 years) and Kabwe (between 300,000 and120,000 years). The archaic Homo erectus skullcap from Kocaba?, referred to as Denizli Man, proves that Homo erectus was already present in Anatolia, at the crossroads of Africa, Asia and Europe, a little more than 1.2 million years ago.     

Gentelles-Le Mont de l’Evangile (département de la Somme,France) : un site de plateau occupé de l’Acheuléen au Micoquien

The palaeolithic site of Gentelles (Somme, France) is situated on a chalky plateau unlike most Lower and Middle Palaeolithic sites of the Somme basin, which are related to fluvial environments (alluvial and slope deposits). The archaeological material of the site excavated at Gentelles on several thousand square meters is recovered from the infilling of a dolina. The archaeological sequence is attributed to Late Middle and Upper Pleistocene (MIS 10 to MIS 5). The assignment of the loess infilling the dolina to MIS 6 is supported by ESR/U-Th dates obtained on teeth and the IRSL age of the sediment. All lithic assemblages include bifacial production and debitage with cores showing one or several surfaces of debitage. There is no evidence of Levallois flaking methods, which are very common in many Middle Palaeolithic industries of Northern France. The first steps of the reducing sequences are not present in most lithic assemblages. Some faunal remains (equids, bovids) have been discovered in the loess deposits. In most cases, the function of the site corresponds to short occupations of hunters moving on the plateau. In contrast, the CLG assemblage (MIS 8) which shows many phases of the reducing sequence suggests longer occupations.     

Douleurs thoraciques et scintigraphie myocardique : à propos de 171 cas

Study aimTo find a correlation between epidemiological factors, risk factors and history and the results of myocardial scintigraphy according to the type of pain and discuss the role of scintigraphy in the diagnosis and therapeutic care.Patients and methodsOur study is retrospective, on 171 patients with typical chest pain (TCP) or atypical (ACP), addressed for myocardial scintigraphy.ResultsFemale predominance was clear. Average age was 59 years. Frequency of risk factors: smoking, diabetes, hypertension, hyperlipidemia, history of heart disease and hypothyroidism was respectively 21.6%, 39.8%, 73.7%, 25.1%, 11.1% and 6.4%. ACP was found in 57.9% of patients, it was more common among women (59.8%). Scintigraphy was abnormal in 36.8% of patients. Scintigraphy was normal in 59.7% of patients with TCP. In the case of ACP, scintigraphy was normal in 65.7%. This difference is not significant. All patients having abnormal scintigraphy had abnormal coronary angiography with a statistically significant correlation. Normal scintigraphy was more frequent (83.3%) in young patients ( < 40 years) and more common in women (67%) than men (55.9%). The sensitivity of scintigraphy is 100%. Its specificity is 66.6%. Its PPV of 57.1%. Its VPN is 100%.ConclusionMyocardial scintigraphy can help clinicians to identify the etiologic diagnosis and assess the prognosis of chest pain.     

Scolécodontes,assemblage et appareil de vers annelidespolychetes errantes de l'aptien de la région d'Agadir,Maroc

From the Aptian scolecodonts inventory of the Agadir area one jaw apparatus and one joining of polychetes are reconstructed. One is the elementary species Schistomeringos expectatusSzaniawski & Gazdzicki, 1978, the oldest representative of the multielementary family Dorvilleidae Chamberlin 1919. The other is a representative of either the multielementary families Atraktoprionidae Kielan Jaworowska 1966 emend. Kozur, 1970 or Arabellidae Hartman 1944. This joining is considered as an hypothesis since all the necessary criteria, defined by H. Szaniawski & A. Gazdzicki 1978, are not all present.     

Associations de kystes de dinoflagellés des séries du Jurassique supérieur (Oxfordien–Tithonien) du Rif externe (Prérif interne et Mésorif,Maroc) et comparaisons régionales

A biostratigraphic study of dinoflagellate cysts of the Upper Jurassic series from the eastern External Rif Chain, has been achieved for the first time on four outcrop sections : the DM section (Douar Marticha), the TB section (the Tarhchenna “Sof”), the KSD section (the Kef Mallou “Sof”) and the Y section (Douar Lamriene) among which three sections (TB, KSD and Y) are well-dated by ammonites and calpionellids fauna. The DM and TB sections are complementary in terms of stratigraphy and correspond respectively to the upper part of the “Ferrysch” Formation, a thick shaly–silty and sandy sequence assigned to the Callovian-Oxfordian stages and to the El Gouzat limestones Formation (Kimmeridgian - Lower Tithonian age) and to the Tarhchenna marly limestones Formation (Upper Tithonian age) from the EL Gouzat area (Mesorif). The KSD and Y sections are also complementary and correspond to the Kimmeridgian-Lower Tithonian Msila limestones Formation and to the overlying marly limestones Massif Formation of Upper Tithonian age, outcropping in the Msila region (Internal Prerif). These four sections have shown many dinocysts rich levels, which had allowed characterizing the Middle? and Upper Oxfordian substages in the DM section. In the other sections, the dinoflagellate cyst assemblages are nearly similar to those of the Kimmeridgian–Tithonian of many sections from the Boreal, Sub-boreal and North tethyan realms, particularily from England, Russia and South-East France basin. The results of the present work confirm once again, the important value of dinoflagellate cysts, for age dating of ammonites-lacking Mesozoic sedimentary sequences and for biostratigraphic correlations.     

Una nueva especie de <Emphasis Type="Italic">Miconia</Emphasis> (Melastomataceae) de la Sierra Madre del Sur de Guerrero y Oaxaca,México

Miconia rzedowskii, which is characterized by its sharply tetragonal distal branches and its mainly sessile trichotomous inflorescences with many flowers, is described from the Sierra Madre del Sur in Guerrero and Oaxaca, Mexico. The new species is illustrated and compared with M. glaberrima, another Mexican species of section Cremanium.     

Cuatro especies nuevas de <Emphasis Type="Italic">Indigofera</Emphasis> (Leguminosae,Papilionoideae) para la Flora de México

Four new species of Indigofera (Leguminosae, Papilionoideae) for the flora of Mexico are described and illustrated: Indigofera floresii, I. hirsutissima, I. magallanesii and I. sinaloensis. Among the new species, I. sinaloensis, is the second species of the series Platycarpae. Including these four new species, we estimate the existence in Mexico of about 31 wild species of the genus.     

Mammouth et comportements de subsistance à l’Épigravettien : analyse archéozoologique du secteur de la fosse no 7 associée à l’habitation no 1 de Mezhyrich (Ukraine)

Zooarchaeological analyses were carried on new large mammal bone materials, from the Epigravettian (Late Upper Palaeolithic) site Mezhyrich (Ukraine), in the pit n^o 7 area associated with the mammoth bone dwelling n^o 1. The results exhibit a usage of the pit as a dump area of food and technical remains from mainly mammoth, hare and fox processing, and bone fuels. The information about mammoth procurement by the last Palaeolithic hunter–gatherers in Eastern Europe allows to document the hunting activities on the mammoth populations, which were probably already weakened at the end of the Pleistocene.