Quantitatively comparing morphological trends to environment in the fossil record (Cincinnatian series; Upper Ordovician)

Determining whether morphological trends in fossil species represent evolution within a lineage or lateral shifts in morphologically variable populations through time requires a thorough examination of the details of both morphology and paleoenvironment in time and space. The purpose of this study is to explore at high resolution the relationship between morphology of the trilobite Flexicalymene granulosa and paleoenvironmental conditions in Upper Ordovician deposits of southwestern Ohio and northern Kentucky. This is achieved by using geometric morphometrics to measure high-resolution morphological changes and by using gradient analysis to capture environmental gradients underlying faunal distribution patterns. Quantitatively comparing the outcomes of these two techniques provides an assessment of whether shape changes relates to environment. Results indicate that a significant amount of shape change, seen as an anteromedial movement of the eye region over time, corresponds to ordination scores. This suggests a relationship between certain aspects of morphology and environment. The combination of these quantitative techniques has provided the foundation for determining whether morphological trends within F. granulosa represent evolution or temporal shifts in geographic variation. Future work will involve examining this relationship in greater detail both geographically and stratigraphically.     

不同体位下输尿管硬镜对输尿管上段结石患者的疗效及安全性分析

摘要 目的：对比不同体位下输尿管硬镜对输尿管上段结石患者的疗效及安全性。方法：2018年8月到2021年1月选择在本院诊治的输尿管上段结石的患者88例作为研究对象,根据随机信封抽签1:1原则把患者分为头高臀低组与水平位组各44例。所有患者均给予输尿管硬镜手术治疗,头高臀低组给予头高臀低截石位,水平位组给予水平截石位,记录与随访疗效及安全性。结果：所有患者顺利完成手术,头高臀低组碎石时间等围手术指标少于水平位组（P<0.05）。头高臀低组术后14 d的总有效率为97.7 %,高于水平位组的86.4 %（P<0.05）。头高臀低组术后14 d的假道形成、输尿管穿孔、粘膜撕脱、感染等总发生率为4.5 %,低于水平位组的25.0 %（P<0.05）。两组术后14 d的血清同型半胱氨酸（Hcy）和β2-微球蛋白（β2-MG）含量较术前1 d低（P<0.05）,头高臀低组低于水平位组（P<0.05）。所有患者术后随访6个月,头高臀低组的复发率为2.3 %,低于水平位组的13.6 %（P<0.05）。结论：相对水平截石位,头高臀低截石位在输尿管上段结石患者输尿管硬镜手术患者的应用能提高总体治疗效果,促进患者康复,也可降低血清同型半胱氨酸和β2-微球蛋白,减少并发症的发生,降低复发率。     

Le site Paléolithique supérieur de Yudinovo : résultats des recherches archéologiques des années 2004–2016

The Upper Palaeolithic site of Yudinovo is one of the reference sites, located in the Desna River Basin. Multidisciplinary field studies, organized by the Desna mission (MAE RAS) and conducted between 2004 and 2016, have changed the vision existed so far on the structure and character of the Yudinovo site as well as on the duration of its occupations. The researchers found an ancient ford used by mammoths and other big mammals to cross the river, and a water source was one of the main factors in explaining the location of the Yudinovo site. The site has been occupied in a cyclical way for stays of varied duration. It was frequented by Prehistoric Men during the different seasons, and periods of occupation were apparently of different duration. The stratigraphy of the Yudinovo site reveals two major episodes in the evolution of the site. The dating of the lower archaeological layer dates back to 15,000–13,500 BC. J.C., while the upper layer is attributed to the period of 12,500–12,000 BC. The lower layer, which was formed during the major episode of occupation of the site, is rather thin and shows the complex stratigraphic structure. Various areas of activities, evacuation structures, storage areas with mammoth bones are discovered. Some elements of the lower archaeological layer are perfectly correlated with different episodes of sporadic occupation.     

L’exploitation de la faune par les groupes humains du Pléniglaciaire supérieur à Eliseevichi 1 (Russie)

The archaeological site of Eliseevichi 1, located in the Dnieper River Basin, was discovered in 1930 by K.M. Polikarpovich. It is contemporary of Epigravettian occupations of the end of the second half of the upper Pleniglacial (20,000–14,000 years BP). As for the sites of the culture of Mezine (Mezine, Mezhirich, Gontsy and Dobranitchevka), it was interpreted as a specialized camp of hunters, mainly for slaughtering woolly mammoths and fur exploitation. Moreover, mammoth bones have been used to build larger structures than in mezinian sites associated with storage pits, as in Timonovka I, Yudinovo, Yourevitchi, Suponevo and Chulatovo. However, Eliseevichi 1 differs from all other sites by the presence of ivory engraved pieces with zigzag patterns and multiple linear features and the presence of platelets with decorations in the form of fish scales (“churingas”) and the high number of chisels. These features make it a unique case in the Desna Valley. To better understand the activities that have been implemented within the site by human groups, particularly the role of different species, we processed to the zooarchaeological study of the faunal remains from the 1935–1936 excavations. The faunal spectrum is restricted, typical of a cold and dry environment, with Mammuthus primigenius, Rangifer tarandus, Canis lupus, Alopex lagopus rossicus and Ursus arctos. Two skulls were previously identified as being those of dogs. According to the taphonomical study we highlighted a quick and deep burying of bones, which were affected by freeze-thaw alternating, without being highly altered and moved by phenomena of cryoturbation. The woolly mammoth was used for its meat and for its ivory. The many remains of canids are characterized by skinning marks and long bones were sawed. The presence of ocher, ashy areas, crude lithic fragments, could be linked to the treatment of skins. The site of Eliseevichi 1 was probably occupied during winter and summer seasons, several times during a long period. It could have two main functions, not as a habitat but as a specialized site of furskin and bone production.     

Humanizing European Paleolithic art: A new visual evidence of human/bird interactions at L’Hort de la Boquera site (Margalef de Montsant,Tarragona, Spain)

This paper reports the discovery of a new example of portable art in North-eastern Iberia dating to the Late Upper Palaeolithic (12.250 ± 60 BP). The piece is analysed in relation to the European Palaeolithic art assemblage to determine its significance and how it contributes to our understandings of Palaeolithic artistic practices. Both the motifs depicted (birds and humans) and the patterns of composition (a narrative scene) are unusual in Palaeolithic assemblages. In addition, this new find contributes to filling a geographic gap in the artistic record as evidence of Palaeolithic art is rare in Catalonia. The anatomical features of one of the birds suggest that it is a crane, a species that has been depicted in a limited number of sites, as summarized in this paper. Moreover, there are only three known example of birds and humans interacting in a narrative scene in Palaeolithic art. Exhibiting innovations in media, subject matter and compositional norms, this new find has the potential to change the classic definition of European Upper Palaeolithic art and integrate the region in the artistic trends circulating along Mediterranean Iberia during the Upper Magdalenian.     

Upper Cenomanian bivalves from the Guir Basin (southwestern Algeria): Order Veneroida

The Upper Cretaceous rocks are widely distributed and well exposed in south Algeria and consist in beds rich in macrofauna. For the first time, twenty veneroid species (Bivalvia) are systematically described from the upper Cenomanian deposits of the Guir Basin. While three species were reported since long before [Granocardium desvauxi (Coquand), G. productum (J. de C. Sowerby) and Glossus aquilinus (Coquand)]; Lucina fallax Forbes, Crassatella (Rochella) tenuicostata (Seguenza), Protocardia hillana (J. Sowerby), G. productum (J. de C. Sowerby) var. byzacenica (Pervinquière), Arctica cordata (Sharpe), A. humei (Cox), A. inornata (d’Orbigny), A. picteti (Coquand), Tenea delettrei (Coquand), Paraesa faba (J. de C. Sowerby), Meretrix desvauxi (Coquand) were previously unknown from the Cretaceous of Algerian Sahara. Because of reduced degree of preservation, Sphaera cf. corrugata J. Sowerby, Maghrebella cf. forgemoli (Coquand), Maghrebella sp., Granocardium cf. carolinum (d’Orbigny), Protocardia sp. and Meretrix sp. are tentatively determined. The studied material, found in the lower part of the “Calcaires de Sidi Mohamed Ben Bouziane” Formation, evidences palaeobiogeographic affinities occurring over a wide geographical area: from North Africa, southern Europe to Middle East and India. The present study provides new information to the knowledge of the upper Cenomanian palaeobiology of the studied region.     

青海曲麻莱-治多地区巴颜喀拉山群(上三叠统)遗迹化石

首次对青海南部曲麻莱-治多地区巴颜喀拉山群上部(上三叠统)遗迹化石进行了系统采集,共采获遗迹化石33属54种。据遗迹化石的形态、习性、水深等环境成因特征,可划分为两类组合:一类以Cosmorhaphe,Helminthopsis,Helminthoida,Megagrapton,Paleodictyon等为主,产生于浊流事件前;另一类以Chondrites,Neo-nereites,Palaeophycus,Phycosiphon,Planolites,Zoophycos等为主,产生于浊流事件后,两者均为半深海-深海Nereites遗迹相的典型代表,反映晚三叠世研究区应为浊流沉积发育的复理石相沉积。     

A new species of the marattialean fern Scolecopteris (Zenker) Millay from the uppermost Permian of Guizhou Province, south-western China

Several isolated marattialean synangia and sporangia are reported from coal balls collected from Coal Seam No.1 (C605) in the uppermost Permian Wangjiazhai Formation in Guizhou Province, south-western China. The synangia are radially symmetrical with diameters between 0.8 and 1.2 mm and are 1.7 mm long, consisting of 3–4 elongate sporangia that are fused basally, free distally and possess a pointed apex. The outer-facing sporangial wall is 4–5 cells thick and conspicuously differentiated. Spores are trilete, have a granular ornamentation and are nearly round equatorially with a diameter of 55–60 µm. Comparisons with other anatomically preserved Palaeozoic marattialean synangia from the Euramerican and Cathaysian floras permit their assignment to the genus of Scolecopteris (Zenker) Millay. In this species the thick, outer-facing sporangial walls and large trilete spores are features consistent with those of the Oliveri Group within Scolecopteris , a group that has previously been considered primitive within this genus. Distinctions from all other previously recognized species within the Oliveri Group lead to the creation of a new species, S. guizhouensis sp. nov. This species is the youngest of the reported species of Scolecopteris recognized from the Euramerican and Cathaysian floras, and provides important evidence on the organization of marattialean ferns from the Upper Permian strata of south China.  © 2006 The Linnean Society of London, Botanical Journal of the Linnean Society , 2006, 151 , 279–288.     

皖南休宁新元古界-下寒武统沉积岩的有机碳同位素记录

皖南休宁县蓝田地区震旦系皮园村组和下寒武统荷塘组主要由硅质岩和黑色页岩组成。皮园村组硅质岩的分析结果表明:δ13Corg分析值落在-36.39‰—-31.45‰范围之内,而且从该剖面的底部到顶部呈现出逐步下降的趋势,可能归之于大气和海洋中O2/CO2比值上升,生物氧化作用增强所致;有机碳(TOC)含量<1%,有机氮(TON)含量<1‰,两者均处于蓝田地区埃迪卡拉系—下寒武统地层的最低值,证明晚震旦世时期该地区海洋生物产量比前期(蓝田期)海洋产量显著下降,可能归之于海水加深,不利于海洋生物的繁殖。荷塘组黑色页岩的δ13Corg分析值落在-33‰—-31‰范围之内,TOC和TON含量与皮园村组比较有大幅度提高,尤其黑色页岩下段TOC含量达到13.85%,证明早寒武世海洋生物得到了大发展。由于新元古代冰期后海洋藻类的大量涌现和早寒武世海洋生物得到大发展,生物光合作用产生大量的O2,导致大气和海水中O2/CO2比值进一步升高,可能是引发“寒武纪生物大爆发”的重要因素。     

A new Bennettitalean trunk with unilacunar five-trace nodal structure from the Upper Cretaceous of Hokkaido, Japan

A new species of Bucklandia is described based on a permineralized fossil trunk that was obtained from sediments of Upper Cretaceous age from Hokkaido, Japan. The quality of preservation is exquisite, and anatomical and morphological features are preserved at the cellular level. The specimen is clearly bennettitalean because of the cycadeoidean-type arrangement of vascular bundles in the petiole. However, this specimen is unique among previously described progymnosperms and gymnosperms in possessing a unilacunar five-trace type of nodal structure. The fossil thus contributes to a more complete understanding of the variation of nodal structure in bennettitalean trunks.