L'intensité lumineuse,son influence sur la teneur en phosphore des carapaces d'Ostracodes

Actual and fossil shells of ostracodes have beenanalyzed with an electronic microprobe: all of them contain phosphorus. X—pictures teach us that the repartition of this chemical element is homogeneous in all the points of the shell. There is no relationship between phosphorus contents in the shells of ostracodes and salinity. In return, there is a relationship between phosphorus contents and temperature and, chiefly, organic phosphorus contents in the environment. However, it is interesting to observe that the analyzed shells of fresh-water ostracodes contain less phosphorus that the generality of the shells of marine ostracodes. The contents of organic phosphorus, in the biotope, depends on the growth of phytoplancton in the upper layers of water which needs a minimum light intensity.     

Paléobiogéographie de quelques Stephanocerataceae (Ammonitina) du Jurassique moyen et supérieur; une confrontation avec la théorie mobiliste

From Bajocian to lower Kimmeridgian, the subfamilyStephanocerataceae represents a large stock of the ammonite fauna. Though it is tributary of author's stratigraphical correlations and systematical interpretations, its geographical distribution with a drifting continents concept gives many teaching about the study of this superfamily, the continental drift and its consequences. Showing a world wide repartition at its apparition this stock then presents branches; the one (Stephanoceratidae) is not envisaged here; the second (Sphaeroceratidae and Cardioceratidae families) characterises rather the «boreal province; the third (Macrocephalitidae family) is chiefly specific of the «tethysian province. A «north-east pacific province with boreal affinities and a «south-east province with tethysian affinities are delimited. It is probably from its fauna that the tethysian macrocephalitid stock appears; first represented by ammonites specifically north american in middle and upper Bathonian stage, they extend during upper Bathonian and lower Callovian and reach South America and the Tethys. The presence of a narrow sea, on Patagonia, West Antarctica, East Africa, Madagascar and India, joining the Tethys and the south edge of Gondwania, is proved at various times, at Bajocian and Callovian stages.     

Discovery of the oldest known Pterygota in the Lower Carboniferous of the Upper Silesian Basin in the Czech Republic (Insecta: Archaeorthoptera)

The earliest pterygote (winged insect), dated from the Lower Carboniferous (Namurian A/E1, circa 324 millions years ago) is described from the Upper Silesian Basin in the Czech Republic. On the basis of its wing venation, it is attributed to the Archaeorthoptera Béthoux and Nel, 2002, crown group of the “Orthoptera”. Besides Apterygota (Collembola and Archaeognatha) known from the Lower Devonian, extremely rare pterygote insects are known from Lower Carboniferous deposits when they first appeared. The present discovery supports the hypothesis of the presence of the ancestor lineage of the orthopteroid in the Lower Carboniferous ecosystems.     

微通道经皮肾镜碎石术治疗感染性结石合并尿液CRPA感染两例

目的:总结一期行微通道经皮肾镜碎石术(microchannel percutaneous nephrolithotripsy,m PCNL)治疗上尿路感染性结石合并尿培养为耐碳青霉烯铜绿假单胞菌(carbapenem resistant pseudomonas aeruginosa,CRPA)的经验。方法:选择我院收治两例左肾结石合并尿培养为CRPA的患者,经积极抗感染治疗后,病例一行左侧经皮肾镜碎石术,病例二先行右肾穿刺造瘘术成功后行左侧经皮肾镜碎石术,观察分析两例患者术后结石清除情况,术中术后出现发热、腰痛、大出血、尿路损伤及肾功能衰竭等并发症情况。结果:两例患者术后复查双J管位置良好,结石基本清除;术中、术后均未出现发热、腰痛、大出血、尿路损伤及肾功能衰竭等并发症。结论:经过合适的围手术期处理,一期微通道经皮肾镜碎石术治疗感染性结石合并尿培养为耐药菌的患者是安全可行的。     

New latest Coniacian to middle Campanian foraminiferal data from the lower Zongshan Formation in the Chaqiela section,Gamba, southern Tibet

A first and detailed foraminiferal biostratigraphic work on the lower part of the Zongshan Formation (Limestone I and Calcareous Marl I sequence) in the Chaqiela section, Gamba, southern Tibet, allows the recognition of three latest Coniacian to middle Campanian planktic foraminiferal biozones: Dicarinella asymetrica Total Range Zone, Globotruncanita elevata Partial-Range Zone, and Contusotruncana plummerae Interval Zone. The base and top of the Santonian Stage in the Chaqiela section were placed at the lowest occurrence (LO) of Globotruncana linneiana and the highest occurrence (HO) of Dicarinella asymetrica, respectively. The deposition of the latest Coniacian to middle Campanian sediments of the lower Zongshan Formation in the Chaqiela section seems to have been continuous or at least without any major gap based on the planktic foraminiferal biozones and events.     

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.     

New advances on the Aurignacian in the central Iberian Mediterranean basin

This study aims to obtain a chronological and cultural framework of the Evolved Aurignacian in the central Iberian Mediterranean basin and find agreement between this framework and other sequences of the Iberian southeast. Over the last few years, there has been remarkable progress in the research of the Evolved Aurignacian sites in the Valencian area, making a review of the main characteristics of the technocomplex on a regional scale necessary. The recent fieldwork carried out in Cova de les Malladetes (Valencia) and in Cova de les Cendres (Alicante) have been key to understanding the lithic, osseous and ornament assemblages ascribed to the Evolved Aurignacian. Several Bayesian modelled ages have been constructed from the large dataset of chronological dates obtained at Malladetes and Cendres, as well as in other sites. The Bayesian models have allowed us to chronologically place the characteristics of the analysed assemblages. The present research supports the importance of the Aurignacian as the first technocomplex of the Upper Palaeolithic in this area of the Iberian Peninsula.     

Parure,pigment et art mobilier du Paléolithique supérieur au Japon

In the Japanese Archipelago, Upper Palaeolithic Accessories, Pigment and Portable Art are discovered, but very few. We introduce the Palaeolithic Art in Japan including new discoveries. The majority of accessories is discovered in Hokkaido, for example the sites of Yunosato 4, Pirika 1, Kashiwadai1 and Obarubetsu 2, but very few in Honshu, the largest island of Japan: Togeyamabokujo 1 in Iwate and Fujiishi in Shizuoka. A lot of pigments are discovered in Hokkaido like Kawanishi C, Kashiwadai 1, Marukoyama and Kiusu 5, without those of Deguchi-Kanezuka in Chiba in Honshu. Kashiwadai 1 in Hokkaido and Kamihikikiri in Chiba are the sites with portable art. In Ehime in Shikoku, one of four large islands of Japan, engraved pebbles called “Kamikuroiwa Venus”, of the Incipient Jomon followed after the Upper Palaeolithic period, before about 14,500 years, are researched again recently. The Palaeolithic art in Japan has a strong relation with Northeast Asia's art, because the lithic materials of Palaeolithic accessories in Hokkaido came from the Continent, and the engraved pebbles have some characters common with Siberian figurines, but also there are accessories and pigment of which the stones are native of the region from the beginning of the Upper Palaeolithic period.