The world’s largest gharialsGryposuchus: description ofG. croizati n. sp. (Crocodylia, Gavialidae) from the Upper Miocene Urumaco Formation, Venezuela

A new fossil gharialGryposuchus species is described from the Upper Miocene Urumaco Formation, Venezuela.Gryposuchus croizati new species can be distinguished from other gavialoids, includingGryposuchus colombianus andGryposuchus neogaeus by the following combination of diagnostic characters: 1) slenderness of the parietal interfenestral bar; 2) dental formula, mainly the lesser number of maxillary teeth, with four premaxillary, 19 maxillary and 22 mandibular teeth; 3) large width of palatines between the reduced palatine fenestrae; 4) medial hemicondyle of the quadrate smaller but detached and much more posteriorly elongated than the lateral one and projected ventromedially; 5) pterygoid morphology, with two posterior vacuities. The polymorphism in the contour of the external naris inGryposuchus was evaluated for taxonomic significance. The body size ofG. croizati n. sp. was estimated in 10.15 m (9.67–10.67 m) using the dorsal skull length and the estimation of the body mass was 1,745 kg (1,280–2,379 kg) based on the braincase length. These maximal values placeG. croizati n. sp. among the world’s largest gharials and even Crocodyliforms as a whole.      

Additions to the knowledge ofUrumaquia robusta (Xenarthra, Phyllophaga, Megatheriidae) from the Urumaco Formation (Late Miocene), Estado Falcön, Venezuela

We describe new remains ofUrumaquia robusta Carlini, Brandoni &; Sänchez, 2006, which significantly improve the knowledge of the species and allow a more precise discussion about the relationships with the rest of the South American Megatheriinae. The new remains (ulna, phalanx, femora, patella, tibia, astragalus, navicular, metatarsals IV–V) described here suggest close affinities of this taxon with the species ofPyramiodontherium and withMegatheriops rectidens, based on morphological similarities of the ulna (length, gracility), femur (general morphology, shape of the medial margin), and astragalus (angle between the discoidal and odontoid facets). In fact, the shape of femoral medial margin is a shared derived character amongUrumaquia, Pyramiodontherium andMegatheriops. However, and despite the increasing information concerning Tertiary species, their phylogenetic relationships are only partially understood.     

Quaternary fossil fish from the Kibish Formation, Omo Valley, Ethiopia

The late Quaternary Kibish Formation of the Omo Valley, southwestern Ethiopia, preserves environments reflecting a history of fluctuations in the level of nearby Lake Turkana over the past 200,000 years. The Kibish Formation has yielded a diverse mammalian fauna (as well as birds and crocodiles), stone tools, and the oldest anatomically modern Homo sapiens. Fish, the most common vertebrate fossils in this unit, are reported in this study. Catfish (especially clariids and Synodontis) and Nile perch (Lates niloticus) predominate, but the gymnarchid Gymnarchus, a cyprinid (Barbus), tigerfish (Hydrocynus), pufferfish (Tetraodon), and other catfish are also present. In total, nine teleost genera are found in the Kibish Formation, representing a subset of the 37 genera that constitute the modern Omo-Turkana ichthyofauna. Several taxa present in the modern fauna, including Polypterus and members of the family Cichlidae, are not found in the Kibish deposits. Most specimens are preserved as disarticulated or broken skeletal elements, but some preservation of articulated elements (e.g., sets of vertebrae, crania with lower jaws or cleithra) also occurs. Many of the catfish and Nile perch specimens are larger than the largest reported from the modern river or lake. Faunas of Kibish Members I and III closely resemble one another; the fauna from Member IV contains only the three most common taxa (Clarias, Synodontis, Lates), though this may result from insufficient sampling. Barbed bone points have been collected from the upper part of the formation, indicating a long association between the human inhabitants and the fish fauna of the Omo Valley.     

Sapropels and the age of hominins Omo I and II, Kibish, Ethiopia

The provenance and age of two Homo sapiens fossils (Omo I and Omo II) from the Kibish Formation in southern Ethiopia have been much debated. Here we confirm that Omo I and the somewhat more primitive-looking Omo II calvariae are from similar stratigraphic levels in Member I of the Kibish Formation. Based on (40)Ar/(39)Ar age measurements on alkali feldspar crystals from pumice clasts in the Nakaa'kire Tuff, a tuffaceous bed in Member I just below the hominin levels, we place an older limit of 198+/-14ka (weighted mean age=196+/-2ka) for the hominins. A younger limit of 104+/-7ka (weighted mean age=104+/-1ka) is provided by feldspars separated from pumice clasts in the Aliyo Tuff in Member III. Geological evidence indicates rapid deposition of each member of the Kibish Formation, concurrent with deposition of sapropels in the Mediterranean Sea. The (40)Ar/(39)Ar age measurements, together with correlations with sapropels, indicate that the hominin fossils are close in age to the older limit. Our preferred estimate of the age of the hominins is 195+/-5ka, making them the earliest well-dated anatomically modern humans yet described.     

湖北保康陡山沱组磷酸盐化微体化石组合

中国南方震旦系陡山沱组磷块岩、燧石和页岩中陆续发现的精美保存的化石生物群,为我们提供了一个栩栩如生的新元古代晚期生物演化的图景,表明多细胞真核生物在新元古代冰期之后发生了非常显著的分异。其中磷块岩化石库以生物细胞结构的完好保存而著称。继在贵州瓮安、陕西勉县茶店和江西上饶朝阳之后,湖北保康白竹磷矿陡山沱组磷块岩中也发现了类似的磷酸盐化化石生物群。保康化石组合中包括多细胞藻类Wengania,Paramecia和原地保存的Thallophyca;大型复杂疑源类Meghystrichosphaeridium,Echinosphaeridium和目前仅在保康发现的Bacatisphaera;球状蓝菌化石Archaeophycus,丝状蓝菌化石Siphonophycus和在陡山沱组磷块岩中首次发现的Obruchevella;同时,内部保存不同数量小球体的球状化石在保康也大量产出。古地理分析表明中国南方扬子地台陡山沱组磷块岩中保存的磷酸盐化化石库大都形成于浅水台地边缘地带。     

保加利亚乳杆菌原生质体的制备与回复研究

目的:通过对保加利亚乳杆菌的原生质体的制备和回复的方法学探讨,为乳杆菌的基因操作和其相关研究提供技术思路和实验条件.方法:用酶浓度分别为1 μg/ml、4 μg/ml、10μg/ml Mutanolysin(变溶菌素)对保加利亚乳杆菌进行处理,脱去细胞壁以探讨其原生质体形成与时间和酶浓度的关系;并选用较为适宜的酶浓度制备其原生质体,在自制的双层再生培养基上观察其原生质体在普通培养、CO2培养、厌氧培养时的回复生长情况.结果:保加利亚乳杆菌对Mutanolysin较敏感,酶浓度为1 μg/ml时只需40min大部分菌体形成原生质体.经1μg/ml Mutanolysin处理后制得的保加利亚乳杆菌原生质体倾入自制的双层再生培养基中,置于CO2和厌氧环境条件下培养能很好的回复生长.结论:本文的研究为乳杆菌的基因工程方面的研究提供了相关的技术条件和实验基础.     

A C-terminal Membrane Anchor Affects the Interactions of Prion Proteins with Lipid Membranes

Membrane attachment via a C-terminal glycosylphosphatidylinositol anchor is critical for conversion of PrP^C into pathogenic PrP^Sc. Therefore the effects of the anchor on PrP structure and function need to be deciphered. Three PrP variants, including full-length PrP (residues 23–231, FL_PrP), N-terminally truncated PrP (residues 90–231, T_PrP), and PrP missing its central hydrophobic region (Δ105–125, ΔCR_PrP), were equipped with a C-terminal membrane anchor via a semisynthesis strategy. Analyses of the interactions of lipidated PrPs with phospholipid membranes demonstrated that C-terminal membrane attachment induces a different binding mode of PrP to membranes, distinct from that of non-lipidated PrPs, and influences the biochemical and conformational properties of PrPs. Additionally, fluorescence-based assays indicated pore formation by lipidated ΔCR_PrP, a variant that is known to be highly neurotoxic in transgenic mice. This finding was supported by using patch clamp electrophysiological measurements of cultured cells. These results provide new evidence for the role of the membrane anchor in PrP-lipid interactions, highlighting the importance of the N-terminal and the central hydrophobic domain in these interactions.     

Electron microscopic studies on the uptake of colloidal thorium dioxide particles by isolated fetal guinea-pig chondrocytes and the distribution of labeled lysosomes in cartilage formed by transplanted chondrocytes

Summary Chondrocytes isolated from fetal, guinea-pig epiphyses were grown in monolayer culture, exposed to thorium dioxide particles, and studied ultrastructurally after varying intervals. The exogenous marker was ingested by endocytosis and subsequently accumulated in lysosomes. After intramuscular injection into young guinea pigs, the thorium dioxidelabeled chondrocytes formed a typical hyaline cartilage. This consisted mainly of rounded or polygonal cells with large, eccentrically located nuclei. The cytoplasm showed an extensive granular endoplasmic reticulum and a well-developed Golgi complex, suggesting active synthesis and secretion of matrix components. Among the other cytoplasmic organelles, lysosomes containing variable amounts of marker particles were observed. After 2–3 weeks the transplants showed signs of cellular degeneration and disintegration. During these processes, lysosomes remained structurally intact and, furthermore, retained the incorporated marker. Thus, thorium dioxide-labeled bodies were found in former chondrocyte lacunae and in the intercellular substance proper. In the latter location labeled bodies could be observed in close proximity to early mineral deposits. These results are discussed with special reference to the cellular origin and lysosomal nature of matrix vesicles in calcifying cartilages.The skilled technical assistance of Mrs. Eva Lundberg and Miss Karin Askfors and the secretarial assistance of Mrs. Ingrid Wäälma are gratefully acknowledged.Financial support was obtained from the Swedish Medical Research Council (proj. no. 12X-3355), the Swedish Cancer Society (proj. no. 100-K71-05XK), the King Gustaf V 80th Birthday Fund, the Harald and Greta Jeansson Foundations, the C. B. Nathhorst Foundation, the A. O. Swärd Foundation, and from the Funds of Karolinska Institutet.     

First titanosaur (Saurischia,Sauropoda) axial remains from the Uberaba Formation,Upper Cretaceous,Bauru Group,Brazil

The Adamantina and Marília formations are considered to be the richest vertebrate-bearing units in the Bauru Group, Upper Cretaceous, Brazil. In contrast, the fossil content from the Uberaba Formation, which only outcrops in Minas Gerais State, is scarce and poorly understood. In this essay the first taxonomically informative titanosaur remains unearthed from this unit are reported. They comprise anterior caudal vertebrae from two different individuals corresponding to a probably basal titanosaur (CPP-360) and a derived titanosaur (CPP-217). Although these remains can be clearly distinguished from other titanosaurs on the basis of their unique association of characteristics like the presence of mildly procoelous centra, lateral pits in the anterior caudal vertebrae, and prezygapophyses with a dorsal protuberance in anterior caudals in CPP-360 and the presence of strongly developed prespinal, spinopostzygapophyseal and centropostzygapophyseal laminae in CPP-217, more complete materials are needed to propose them new names.     

Oligocene larger foraminifera from United Arab Emirates,Oman and Western Desert of Egypt

An early Oligocene (Rupelian) diagnostic larger foraminiferal assemblage is described and illustrated from marls and limestones of the Asmari Formation, at Jabals Hafit and Malaqet in the UAE. An equivalent assemblage is identified in the mudstones of the Tahwah Formation, Wadi Suq, Oman. Although Nummulites intermedius (D'Archiac 1846) and N. fichteli are fully synonymous (e.g. Roveda 1970; Schaub 1981; Sirel 2003), in this study both species are biometrically differentiated, distinct and both names are valid. N. fichteli Michelotti 1841, N. intermedius (D'Archiac 1846) and N. emiratus n. sp., which are index for the early Oligocene (Rupelian), and they are replacing each others competitively and environmentally.

The presence of Blondeauina bouillei n.gen., N. emiratus n.sp., N. intermedius, N. fichteli, Planoperculina complanata (Defrance 1822) and Austrotrillina asmariensis Adams 1968 ascribed the section of the Asmari Formation to the early Oligocene (Rupelian). The studied marls and limestones were deposited in outer and inner shelf environments, respectively. The Asmari Formation in the area studied consists mainly of marl in its lower portion and reefal limestone in its upper part, indicating a major marine regression. The Tahwah Formation in Oman is composed of bioturbated silty and muddy marls and is a facies equivalent to the Asmari Formation marls. The Asmari Formation facies change probably relates to a mid-Oligocene fall in global sea level.

In this study, the Dabaa Formation, a subsurface unit of late Eocene–Oligocene marine shales in the north Western Desert of Egypt, was chosen to correlate with the Oligocene of Emirates and Oman. The Dabaa Formation comprises Spiroclypeus ornatus (Henson 1937) and Eulepidina dilatata (Michelotti 1861). The environment of deposition was inner shelf to littoral, which become estuarine towards the top in many areas. This Oligocene Dabaa sequence is correlatable with Wadi El Arish sequence recently discovered by Kuss and Boukhary (2008) from Risan Aneiza, Northern Sinai, Egypt.