SULCIPENTAMERUS (PENTAMERIDA, BRACHIOPODA) FROM THE LOWER SILURIAN WASHINGTON LAND GROUP, NORTH GREENLAND

Abstract:  The brachiopod Sulcipentamerus , previously considered a common endemic pentameride genus in the Lower Silurian (Aeronian) of South China, is reported from largely coeval strata in the Hauge Bjerge, Ymers Gletcher and Odins Fjord formations (Washington Land Group) of North Greenland. Two species are present. In eastern North Greenland, S . cf. dorsoplanus occurs in carbonate strata of Aeronian – early Telychian age, whereas in the western region, a new species, S . lunatus sp. nov., is described. The identification of both forms as Sulcipentamerus is indicated by their relatively long ventral median septum and dorsal inner hinge plates. The new species, Sulcipentamerus lunatus sp. nov., is characterized by a nonlobate shell, a narrow but sharply defined interarea bordering the delthyrium and a deeply concave pseudodeltidium. Despite the two known occurrences of the genus in South China and Greenland, the Sulcipentamerus -bearing Harpidium Fauna of North Greenland (northeastern part of Laurentia) was quite distinct from both the Aeronian–Telychian brachiopod faunas of South China and the southern half of Laurentia. In general, the Aeronian pentameride brachiopod faunas of these three regions are strongly endemic, in contrast to their more tightly clustered counterparts from Avalonia, Baltica, Siberia, Kazakhstan, Tadzhikistan, Kolyma and Novaya Zemlya.     

A NEW PARASEMIONOTID-LIKE FISH FROM THE LOWER TRIASSIC OF JURONG, JIANGSU PROVINCE, SOUTH CHINA

Abstract:  Based on a well-preserved specimen from the Early Triassic Lower Qinglong Formation exposed at Qingshan Quarry, Jurong, Jiangsu Province of China, the new taxon Peia jurongensis gen. et sp. nov. is named and described with anatomical details of its dermal skull, neurocranium and postcranial skeleton. The new taxon is characterized by the following set of characters: shallow V-shaped, tuber-like rostral; anterior part of frontal widened to roughly same width as its posterior part; roughly squared parietal; supraorbital absent; wide and slightly posteriorly inclined preopercle; five small ossifications present in dorsal half of preopercle; preopercular canal shifting anteriorly in ventral half of the preopercle, and reaching the anteroventral corner of this bone; dermosphenotic joining the skull roof and with a descending lamina; numerous branchiostegal rays. Comparisons are made between the new taxon and several parasemionotids from the same locality; a discussion is carried out on the distribution and evolution of several characters in halecomorphs and other closely related neopterygians.     

WUCHIAPINGIAN (LOPINGIAN, LATE PERMIAN) BRACHIOPODS FROM THE EPISKOPI FORMATION OF HYDRA ISLAND, GREECE

Abstract:  Twenty-three species of silicified brachiopods are described from four samples in the middle and upper parts of the Episkopi Formation from Hydra Island, Greece. These brachiopods are newly recorded from the region and together with previously described brachiopods from the same localities constitute the most diverse Lopingian (Late Permian) brachiopod fauna reported in southern Europe. The brachiopod fauna is Wuchiapingian as indicated by the associated conodonts. The fauna from Hydra exhibits strong palaeobiogeographical links with the faunas from South China. In addition, palaeobiogeographical affinities with the faunas of Thailand and the northern peri-Gondwanan region are also present, which implies a peri-Gondwanan origin for Hydra. Palaeoecologically, the brachiopod assemblage from sample EP in the middle part of the Episkopi Formation is dominated by pedically-attached and cementing genera and reflects moderate energy conditions above storm wave base and an abundance of hard substrates provided by sponges in the biohermal habitat. By contrast, the brachiopod assemblage in the other three samples from the upper part of the Episkopi Formation is dominated by spinose genera with a free-resting life habit, suggesting soft substrates in a quiet water environment below storm wave base on the outer part of the shelf. New taxa are Petinospiriferina gen. nov., Hustedia episkopiensis sp. nov., Waterhouseiella hydraensis sp. nov. and Xenosaria tenuis sp. nov.     

A NEW OXFORDIAN PLIOSAURID (PLESIOSAURIA, PLIOSAURIDAE) IN THE CARIBBEAN SEAWAY

Abstract:  A new pliosaurid, Gallardosaurus iturraldei gen nov. et sp. nov., was found in the Viñales area, western Cuba, in sediments of the Jagua Formation, middle–late Oxfordian. This new taxon is characterized by: wide participation of the premaxilla in the outer margin of the external naris; frontal not participating in the orbital margin; postorbital in contact with the jugal and squamosal; presence of anterior pterygoid vacuity; cultriform process of parasphenoid convex and exposed in palatal view; pterygoid flanges high; jaw articulation low relative to tooth row; trihedral teeth in cross-section and with smooth ridges at least in the labial face. A phylogenetic analysis suggests that Gallardosaurus forms a clade with Peloneustes , the most common pliosaurid genus occurring in the Oxford Clay. The Caribbean Seaway was, at least since the Oxfordian, a corridor that permitted the interchange for marine biota between Western Tethys and Eastern Pacific realms. Among vertebrates, bony fish and long-necked plesiosaurs prevailed. However, marine pleurodiran turtles, metriorhynchid crocodilians, ophthalmosaurian ichthyosaurs, and pliosaurids ( G. iturraldei gen. nov. et sp. nov.) have also been found, as well as at least two species of pterosaurs, and one camarasaurian dinosaur. Among these reptiles there were off-shore pelagic forms such as the ichthyosaurs and metriorhynchids, together with the pliosaurid G. iturraldei gen. nov. et sp. nov.; other taxa were presumably less pelagic, such as the pleurodiran turtles and the cryptoclidid plesiosauroids. Gallardosaurus iturraldei gen. nov. et sp. nov. would have played the role of an active predator taking advantage of nectonic fish recorded in the area.     

Methyl-Deficient Transfer Ribonucleic Acid and Macromolecular Synthesis in Methionine-Starved Saccharomyces cerevisiae

Haploid methionine auxotrophs of Saccharomyces cerevisiae continue to multiply for several hours after withdrawal of a required amino acid from the medium. Macro-molecular synthesis continues during this period of residual growth, although the net ribonucleic acid (RNA) and protein content is constant during the later part of this period. In this study, growth after withdrawal of methionine was in some cases accompanied by accumulation of transfer RNA (tRNA), which was shown by methylation in vitro to be deficient in methyl groups. This phenomenon was shown by only four of nine methionine auxotrophs tested, but no evidence could be found that these four strains had "relaxed" control of RNA synthesis. The nine methionine-requiring strains represent mutations in five different positions in the methionine biosynthesis pathway, and only mutants blocked at two of these five positions accumulated methyl-deficient tRNA. This accumulation therefore appears to be correlated with the position of the strain's block in the pathway of methionine biosynthesis.     

Influence of Methionine Pool Composition on the Formation of Methyl-Deficient Transfer Ribonucleic Acid in Saccharomyces cerevisiae

Methionine auxotrophs of Saccharomyces cerevisiae continue to synthesize ribonucleic acid (RNA) after methionine withdrawal. The newly synthesized transfer RNA (tRNA) is methyl-deficient in some strains, but not in all. Whether such tRNA will accumulate depends on the position of the block in the methionine pathway that is carried by the mutant strain. Free methionine rapidly decreases in the intracellular pool of all strains after its removal from the medium. Certain metabolites derived from methionine are removed from the pool relatively slowly after methionine withdrawal. Notable among these is S-adenosylhomocysteine, which is depleted less rapidly from those strains that accumulate methyl-deficient tRNA than from others. S-adenosylhomocysteine is a potent inhibitor of tRNA-methylating enzymes in vitro.     

汽车尾气对路旁琵琶柴的影响

琵琶柴(Reaumuria soongorica)广布于我国新疆、内蒙、宁夏、甘肃、青海等干旱、半干旱地区,为泌盐的超旱生小灌木。在平缓干燥的砾质、砂砾质荒漠区,常成为优势种。作为牧草,它品质中等,耐牧性很强,不仅是草原化荒漠相典型荒漠地区骆驼和羊等家畜的主要度荒饲草,而且还是新疆卡拉麦里山有蹄类野生动物保护区内食性单调的国家一级保护动物蒙古野驴(Equus hemionus)和国家二级保护动物鹅喉羚(Gezella subgutturosa)所啃食的种类。琵琶柴在蒙古野驴和鹅喉羚粪便     

Effect of shift work on the night-time secretory patterns of melatonin, prolactin, cortisol and testosterone

In a study of the internal desynchronization of circadian rhythms in 12 shift workers, 4 of them, aged 25-34 years, agreed to be sampled every 2 h during their night shift (0000 hours to 0800 hours). They were oil refinery operators with a fast rotating shift system (every 3-4 days). We found marked changes in the secretory profiles of melatonin, prolactin and testosterone. Melatonin had higher peak-values resulting in a four-times higher amplitude than in controls. With respect to prolactin and testosterone, peak and trough times were erratic and the serum concentrations were significantly decreased in shift workers. Serum cortisol presented a decreased rhythm amplitude together with higher concentrations at 0000 hours in shift workers. This study clearly shows that fast rotating shift-work modifies peak or trough values and rhythm amplitudes of melatonin, prolactin, testosterone and cortisol without any apparent phase shift of these hormones. Whether the large rhythm amplitude of melatonin may be considered as a marker of tolerance to shift work, as reported for body temperature and hand grip strength, since it would help the subjects to maintain their internal synchronization, needs further investigation.     

Identity elements for N2-dimethylation of guanosine-26 in yeast tRNAs.

N2,N2-dimethylguanosine (m2(2)G) is a characteristic nucleoside that is found in the bend between the dihydro-uridine (D) stem and the anticodon (AC) stem in over 80% of the eukaryotic tRNA species having guanosine at position 26 (G26). However, since a few eukaryotic tRNAs have an unmodified G in that position, G26 is a necessary but not a sufficient condition for dimethylation. In yeast tRNA(Asp) G26 is unmodified. We have successively changed the near surroundings of G26 in this tRNA until G26 became modified to m2(2)G by a tRNA(m2(2)G26)methyltransferase in Xenopus laevis oocytes. In this way we have identified the two D-stem basepairs C11-G24, G10-C25 immediately preceding G26 as major identity elements for the dimethylating enzyme modifying G26. Furthermore, increasing the extra loop in tRNA(Asp) from four to the more usual five bases influenced the global structure of the tRNA such that the m2(2)G26 formation was drastically decreased even if the near region of G26 had the two consensus basepairs. We conclude that not only are the two consensus base pairs in the D-stem a prerequisite for G26 modification, but also is any part of the tRNA molecule that influence the 3D-structure important for the recognition between nuclear coded tRNAs and the tRNA(m2(2)G26)methyltransferase.