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.     

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.     

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.     

黑龙江省甘南县旧石器地点发现的新材料

黑龙江省的旧石器考古发掘与研究始于上世纪30年代,迄今为止已有正式报道或发表的遗址和地点100余处,分布在黑龙江省境内各处,年代上均属于旧石器时代晚期。2017年初,根据齐齐哈尔市查哈阳农场群众提供的线索,笔者等在甘南县环太平湖水库周边发现多处旧石器地点以及原料产地。经对该地区的踏勘调查和对一处地点的小规模剖面清理发现,环太平湖地区分布着面积广大的旧石器时代晚期地层,其中石制品数量丰富,同时还发现了疑似的半地穴遗迹。这些遗存代表了当时该地区较大的古人类活动规模,周边出产的优质石制品原料为古人类的生产生活提供了良好的生产力要素,使这一地区孕育出了成熟的石叶、细石叶技术产品。对广合屯第1地点下部风化壳中炭屑的¹⁴C测年结果表明,这些石制品的年代应晚于距今3万年。     

河北泥河湾盆地下卜庄遗址端刮器功能的实验分析

端刮器常见于旧石器时代晚期的细石器工业中,形制比较固定,在探讨人类行为、生计以及环境适应等方面具有重要的研究价值。国外的研究涉及制作工艺、使用方式与功能等多个方面,而国内的研究多为类型学分析,对其功能的研究相对薄弱。河北泥河湾盆地下卜庄遗址出土了一定数量的端刮器遗存,本文通过模拟打制与使用实验,结合微痕分析方法,对它们的功能进行了探索,结果表明：1）下卜庄遗址的端刮器可能主要用来加工兽皮,且加工湿皮的现象较多;2）端刮器也可能直接被用来加工木材;3）部分端刮器微痕之间的关系表明,一些端刮器在使用过程中存在对刃缘的重新修理,当它们不再适合处理兽皮时会被用来加工木材,而后废弃。     

A NEW TRISTICHOPTERID (SARCOPTERYGII, TETRAPODOMORPHA) FROM THE UPPER FAMENNIAN EVIEUX FORMATION (UPPER DEVONIAN) OF BELGIUM

Abstract:  Additional material of a large specimen of tristichopterid fish from the Upper Famennian Evieux Formation of Belgium is described. This large fish was previously assigned to Tristichopteridae gen. et sp. indet. due to the lack of diagnostic anatomical data. New available material consists of the internal surface of the parietal shield, vomers and anterior part of the parasphenoid, subopercular and submandibulo-branchiostegal bones, and an internal view of the anterior part of the mandible. A possible autapomorphy of the new form from Belgium, Langlieria socqueti gen. nov. et sp. nov., is the absence of marginal teeth on the vomer except on its most lateral part. Apart from these features, it only differs from the genus Mandageria from Australia in the absence of marginal teeth between the dentary fang and the mandibular symphysis, in the presence of a raised marginal crest lateral to the anterior coronoid fang, and in the presence of numerous small marginal teeth on the premaxilla. It differs from the cosmopolitan genus Eusthenodon in a number of respects: the supratemporal, tabular, and postparietal bones are superficially fused, as are the intertemporal and parietal bones, the dermal ornament is proportionally very fine, and the denticulated field of the parasphenoid stands proud rather than being recessed into the body of the bone.     

ULTRASTRUCTURE OF DISPERSED AND IN SITU SPECIMENS OF THE DEVONIAN SPORE RHABDOSPORITES LANGII: EVIDENCE FOR THE EVOLUTIONARY RELATIONSHIPS OF PROGYMNOSPERMS

Abstract: The spore Rhabdosporites (Triletes) langii (Eisenack) Richardson, 1960 is abundant and well preserved in Middle Devonian (Eifelian) ‘Middle Old Red Sandstone’ deposits from the Orcadian Basin, Scotland. Here it occurs as dispersed individual spores and in situ in isolated sporangia. This paper reports on a detailed light microscope (LM), scanning electron microscope (SEM) and transmission electron microscope (TEM) analysis of both dispersed and in situ spores. The dispersed spores are pseudosaccate with a thick walled inner body enclosed within an outer layer that was originally attached only over the proximal face. The inner body has lamellate/laminate ultrastructure consisting of fine lamellae that are continuous around the spore and parallel stacked. Towards the outer part of the inner body these group to form thicker laminate structures that are also continuous and parallel stacked. The outer layer has spongy ultrastructure. In situ spores preserved in the isolated sporangia are identical to the dispersed forms in terms of morphology, gross structure and wall ultrastructure. The sporangium wall is two‐layered. A thick coalified outer layer is cellular and represents the main sporangium wall. This layer is readily lost if oxidation is applied during processing. A thin inner layer is interpreted as a peritapetal membrane. This layer survives oxidation as a tightly adherent membranous covering of the spore mass. Ultrastructurally it consists of three layers, with the innermost layer composed of material similar to that comprising the outer layer of the spores. Based on the new LM, SEM and TEM information, consideration is given to spore wall formation. The inner body of the spores is interpreted as developing by centripetal accumulation of lamellae at the plasma membrane. The outer layer is interpreted as forming by accretion of sporopollenin units derived from a tapetum. The inner layer of the sporangium wall is considered to represent a peritapetal membrane formed from the remnants of this tapetum. The spore R. langii derives from aneurophytalean progymnosperms. In light of the new evidence on spore/sporangium characters, and hypotheses of spore wall development based on interpretation of these, the evolutionary relationships of the progymnosperms are considered in terms of their origins and relationship to the seed plants. It is concluded that there is a smooth evolutionary transition between Apiculiretusispora‐type spores of certain basal euphyllophytes, Rhabdosporites‐type spores of aneurophytalean progymnosperms and Geminospora‐/Contagisporites‐type spores of heterosporous archaeopteridalean progymnosperms. Prepollen of basal seed plants (hydrasperman, medullosan and callistophytalean pteridosperms) are easily derived from the spores of either homosporous or heterosporous progymnosperms. The proposed evolutionary transition was sequential with increasing complexity of the spore/pollen wall probably reflecting increasing sophistication of reproductive strategy. The pollen wall of crown group seed plants appears to incorporate a completely new developmental mechanism: tectum and infratectum initiation within a glycocalyx‐like Microspore Surface Coat. It is unclear when this feature evolved, but it appears likely that it was not present in the most basal stem group seed plants.     

MICROVERTEBRATE BIOSTRATIGRAPHY OF UPPER DEVONIAN (FRASNIAN) CARBONATE ROCKS IN THE CANNING AND CARNARVON BASINS OF WESTERN AUSTRALIA

Abstract:  Shark teeth and scales from the Gneudna Formation type section, Carnarvon Basin are rare, but they represent a diverse fauna as well as being the first Frasnian chondrichthyan remains found in Western Australia. In contrast numerous shark teeth and scales have been obtained from coeval sections in the Canning Basin. Teeth referred to as Phoebodus bifurcatus, Phoebodus fastigatus, Phoebodus cf. fastigatus, Phoebodus latus , Phoebodus sp. C and Protacrodus sp. 1 are described from two Canning Basin localities: Horse Spring Range and McIntyre Knolls. The phoebodont species described here have a global distribution and can, therefore, be placed within the standard Frasnian phoebodont zonation. The shark remains from the Gneudna Formation type section include one new genus Emerikodus ektrapelus gen. et sp. nov., described along with Helodontidae indet and Elasmobranchii gen. et sp. indet. It is proposed that the faunal differences observed between the localities are a result of environmental differences. In addition to shark remains, scales from the thelodont Australolepis seddoni were also recovered from each locality. The well-dated Zone 6–10 conodont faunas at Horse Spring constrain the range of A. seddoni with which they occur, and importantly indicate that the Gneudna Formation type section is wholly Frasnian.     

New Frasnian conodonts of the genus Palmatolepis from the Central Tajikistan

New Lower-Middle Frasnian conodonts of the genus Palmatolepis Ulrich et Bassler, 1926 are described from the Kalagach and Kulyali formations of the Sishkat key section of Central Tajikistan. Palmatolepis manzuri sp. nov. descends from Pa. punctata (Hinde) and is an ancestor of Pa. kireevae Ovnatanova, Pa. salibaevi sp. nov., and also of the Pa. rhenana Bischoff branch.