The haemocytes of the salp Thalia democratica (Tunicata,Thaliacea): an ultrastructural and histochemical study in the oozoid

In comparative immunology and evolution of the chordate immune system, tunicates hold an important phylogenetic position as sister group of vertebrates. However, knowledge of the tunicate immune system is limited to the class Ascidiacea, in which some species are now considered model organisms. In the class Thaliacea, represented by fragile pelagic species, the few studies on their haemocytes go back to several decades ago and do not consider comparative aspects with ascidian haemocytes. In this study, we identified various haemocyte types and their distribution in the common salp Thalia democratica by comparative observations under light and electron microscopy and by histochemical, histoenzymatic and immunohistochemical techniques. By comparing specialisations with those of ascidian haemocytes, we detected an undifferentiated cell type (lymphocyte‐like cell) and three categories with four cell types, that is, (i) phagocytic line (hyaline amoebocyte and amoebocyte with large vacuoles), (ii) mast cell‐like line (granular cell) and (iii) storage cells (nephrocyte). Both phagocytes and granular cells appear to migrate in the tunic. Phagocytes adhere to the tunic which internally covers the oral siphon, where they probably function as sentinel cells of the pharynx. Results show the variety of haemolymph cells in the salp similar to phlebobranch ascidians.     

Fixation of a vacuole-associated network of channels in protein-storing pea cotyledon cells

Summary In cells of developing pea cotyledons fixed at ambient temperature, electron-dense cisternae often encircle vacuoles and occasionally are continuous with vacuolar protein deposits. In cotyledons chilled prior to fixation, the cisternae are present as an anastomosing network of channels that make multiple contacts with vacuolar protein. It is suggested that during fixation at ambient temperature, many of the contacts with vacuoles are lost and that much of the complexity of the network is lost, giving way to a system of largely unbranched cisternae. The network may be a mobile phase involved in reserve protein accumulation and concentration within the vacuole.     

Geochronology of cave deposits at Liang Bua and of adjacent river terraces in the Wae Racang valley, western Flores, Indonesia: a synthesis of age estimates for the type locality of Homo floresiensis

A robust timeframe for the extant cave deposits at Liang Bua, and for the river terraces in the adjoining Wae Racang valley, is essential to constrain the period of existence and time of extinction of Homo floresiensis and other biota that have been excavated at this hominin type locality. Reliable age control is also required for the variety of artifacts excavated from these deposits, and to assist in environmental reconstructions for this river valley and for the region more broadly. In this paper, we summarize the available geochronological information for Liang Bua and its immediate environs, obtained using seven numerical-age methods: radiocarbon, thermoluminescence, optically- and infrared-stimulated luminescence (collectively known as optical dating), uranium-series, electron spin resonance, and coupled electron spin resonance/uranium-series. We synthesize the large number of numerical age determinations reported previously and present additional age estimates germane to questions of hominin evolution and extinction.     

Facies and diagenetic evaluation of the Permian–Triassic boundary interval and basal Triassic carbonates: shallow and deep ramp sections,Hungary

The Permian–Triassic boundary and basal Triassic shallow-marine successions were studied and correlated in sections of two structural units in Hungary (Transdanubian Range and Bükk units). Core sections in the Transdanubian Range unit recovered inner ramp deposits whereas outcrops in the Bükk unit expose deposits of the deeper ramp area of the western Tethys. The inner ramp section (studied ca. 10 m in thickness) is characterized by a succession of dolomites overlain by bioclastic limestones, peloidal grainstones (which recorded the biotic decline) and oolites with finely crystalline limestone interlayers. The deeper ramp section (studied ca. 15 m in thickness) is characterized by a succession of bioclastic limestones and marlstones, mudstone beds (recording the first biotic decline), the ‘boundary shales’ (recording the second biotic decline and the stable carbon isotope marker), mudstones with wackestone laminae, and stromatolite boundstones. Accordingly, oolite formation and microbial micrite precipitation represent carbonate sedimentary responses of end-Permian mass extinction on the carbonate shelf. In both successions, mudstones predominate the upsection, suggesting a relative sea-level rise. The succession of the deep ramp area exhibits a continuous sediment accumulation and the diagenesis here was influenced by marine and marine-derived pore water. The δ¹³C curve shows a continuous change towards more negative values, starting in bioclastic limestones, followed by a sharp symmetric negative peak at the second biotic decline that is a chemostratigraphic marker of the boundary event. Facies and microfacies trend of the inner ramp carbonates in the Transdanubian Range unit exhibits close similarities to that found in many South Alpine sections. Relict peloidal deposits, formed cemented submarine hardground substrate, indicate the extinction level. Sedimentary and diagenetic features of the overlying oolite bedset revealed slightly different depositional environments in the two studied Transdanubian Range unit sections. Petrography of the oolites highlighted shallow burial diagenetic alterations which includes marine cementation, marine-burial replacement and dolomitization. A lack of the specific negative peak in the δ¹³C values is most likely due to the multiple redeposition events of the sedimentary grains. This led to the conclusion that the deeper ramp deposits (e.g., in Bükk unit) have greater potential for recognizing trends in processes, affecting the marine environments and related to the end-Permian mass extinction, at the western Tethys.     

昆明盐矿古老岩盐沉积中可培养细菌多样性研究

为了了解昆明盐矿古老岩盐沉积中可培养细菌的多样性,用MBA和ISP2分离和培养了昆明盐矿卤水和盐晶中的细菌44株。发现盐晶中的可培养好氧细胞数量(3·1×103~3·7×106CFU/g)远远高于卤水中的数量(1·3~6·3×103CFU/L)。分离所得纯培养物的16SrDNA序列系统发育分析结果表明,44株菌可分为4大类群34个不同的分类单元(16SrDNA序列相似性大于97%为同一分类单元)。24株属于厚壁菌门(Firmicutes,54·6%),2株属于变形菌门α亚群(α-Proterbacteria,4·6%),4株属于变形菌门γ亚群(γ-Proterbacteria,9·1%),14株属于放线细菌门(Actinobacteria,31·7%)。卤水和盐晶中的优势菌都是Bacillus属菌(26·1%和59·9%)。据16SrDNA序列相似性分析发现7株菌为可能的新种或属。此外,还筛选到7株抗菌活性菌株。研究表明,昆明盐矿古老岩盐沉积中,不仅含有较为丰富的微生物物种多样性,并且存在许多未被认识的新物种和生物活性菌株,为古老岩盐沉积中微生物的深入研究奠定了基础。     

Towards industrially-feasible delignification and pitch removal by treating paper pulp with Myceliophthora thermophila laccase and a phenolic mediator

The ability of two natural phenols to act as mediators of the recombinant Myceliophthora thermophila laccase (MtL) in eucalypt-pulp delignification was investigated. After alkaline peroxide extraction, the properties of the enzymatically-treated pulps improved with respect to the control. The pulp brightness increased (3.1 points) after the enzymatic treatment with MtL alone, but the highest improvements were obtained after the MtL treatment using syringaldehyde (4.7 points) and especially methyl syringate (8.3 points) as mediators. Likewise, a decrease in kappa number up to 2.7 points was obtained after the MtL-methyl syringate treatment, followed by decreases of 1.4 and 0.9 points after the treatments with MtL-syringaldehyde and MtL alone, respectively. On the other hand, removal of the main lipophilic extractives present in eucalypt pulp was observed after the above laccase-mediator treatments. Finally, the doses of both MtL and methyl syringate were reduced, and results compatible with industrial implementation were obtained.     

A new peculiar dinosaur egg,Sankofa pyrenaica oogen. nov. oosp. nov. from the Upper Cretaceous coastal deposits of the Aren Formation,south‐central Pyrenees,Lleida, Catalonia,Spain

Abstract: A new type of small, ovoid dinosaur egg, Sankofa pyrenaica oogen. nov. oosp. nov., with a prismatic type eggshell is described from upper Cretaceous (upper Campanian–Maastrichtian) deposits of the Montsec area, South Pyrenean Central Unit, Lleida, Catalonia, Spain. This egg type was sub‐vertically laid in only two rich monospecific sites of a single stratigraphic layer from coastal deposits of the Aren Formation, interpreted as an emerged beach ridge of a barrier island – lagoon depositional system. The size and shape of these eggs with their asymmetric poles are roughly similar to modern hen eggs, which is unusual in the Cretaceous fossil egg record. Its phylogenetic position clusters with bird and Troodontid eggs. A morphospace analysis of egg shapes shows the similarity of the new egg to a Campanian fossil bird egg from Argentina, both being intermediate between modern‐bird eggs and extinct nonavian theropod eggs. However, the eggshell microstructure of Sankofa pyrenaica differs from that of bird eggs in its incipient squamatic texture. It has a peculiar pattern of interlocking small crystals in the middle of the palisade layer, instead of the thick squamatic structure commonly present in modern avian eggshells. This new egg type is attributed to a small theropod, probably with a single oviduct like birds and whose mosaic distribution of features is a combination between that of birds and nonavian theropods. This enhances the arguments supporting the close phylogenetic relationships between both groups.     

A possible billion-year-old holozoan with differentiated multicellularity

1. Download : Download high-res image (269KB)
2. Download : Download full-size image

     

A new species of fossil Mus (Rodentia, Muridae) from the Indian Himalaya: Evolutionary and phylogenetic implications

A new species of fossil Mus (Rodentia, Mammalia) is reported from the Late Pleistocene fluvio-lacustrine deposits of the Kumaun sector of Indian Himalaya. The fossiliferous horizon, medium-coarse grained sand lenses embedded in the massive carbonaceous mud, is exposed at locality Dulam and is Late Pleistocene (ca. 30 ka) in age. A new species, Mus dulamensis n. sp., is proposed. Characterized by strongly distorted and moderately elongated M¹ (about 170% of M² length) with prominent conules in front of the t₂, higher magnitude of stephanodonty (between the t₁ and t₄ and between the t₃ and t₆), moderately reduced M³ (about 56% of M² length) and stronger connection between the cusps, this species is distinct from all other species of the genus and is included in the “booduga group”. I suggest that M. dulamensis n. sp. is comparatively more derived than M. auctor, M. flynni, M. jacobsi and Mus sp. and it may have given rise to M. booduga or M. dunni. It is further suggested that presently living M. booduga and M. dunni are more specialized than Mus dulamensis n. sp.