Biochemical investigation of multicorer sediment profile PS74/121-1

To detect and track the impact of large-scale environmental changes in a the transition zone between the northern North Atlantic and the central Arctic Ocean, and to determine experimentally the factors controlling deep-sea biodiversity, the Alfred- Wegener-Institute for Polar and Marine Research (AWI) established the deep-sea long-term observatory HAUSGARTEN, which constitutes the first, and until now only open-ocean long-term station in a polar region. Virtually undisturbed sediment samples have been taken using a video-guided multiple corer (MUC) at 13 HAUSGARTEN stations along a bathymetric (1,000 - 4,000 m water depth) and a latitudinal transect in 2,500 m water depth as well as two stations at 230 and 1,200 m water depth within the framework of the KONGHAU project. Various biogenic sediment compounds were analyzed to estimate the input of organic matter from phytodetritus sedimentation, benthic activities (e.g. bacterial exoenzymatic activity), and the total biomass of the smallest sediment-inhabiting organisms (size range: bacteria to meiofauna).

2-O-methyl-1-methyl adenosine: A new modified nucleoside in ragi (eleusine coracana ) tRNA

A new modified nucleoside 2-²-O-methyl-l-methyl adenosine has been found to be present in the tRNA of (eleusine coracana ) (ragi) seedlings. The sequence of the dinucleotide of which this modified nucleoside is a part suggests its presence in phenylalanine-tRNA. The structural implications of the presence of this new modification are discussed.

Characterization and expression analysis of TNFR-associated factor 1 (TRAF1) in grass carp Ctenopharyngodon idella

TNF receptor associated factor 1 (TRAF1) plays an important role in regulating the TNF signaling and protecting cells from apoptosis. In the present study, a TRAF1 gene has been cloned from grass carp (Ctenopharyngodon idella) by reverse transcription (RT)-PCR and rapid amplification of cDNA ends (RACE). The full-length cDNA is 2235 bp, including a 250 bp 5' UTR (untranslated region), a 1659 bp open reading frame, and a 326 bp 3'UTR. The polyadenylation signal (AATAAA, AATAA) and one mRNA instability motif (AUUUA) were found followed by a poly (A) tail in the 3'UTR. No signal peptide or transmembrane region has been found in the putative amino acids of grass carp TRAF1 (gcTRAF1). The putative amino acids of gcTRAF1 share 72% identity with the homologue in zebrafish. It is characterized by a zinc finger at the N-terminus and a TRAF domain (contains one TRAF-C and one TRAF-N) at the C-terminus. The identity of the TRAF domain among all the TRAF1 homologues in vertebrates varies from 52% to 58%, while the identities of TRAF-C were almost the same as 70%. The recombinant gcTRAF1 has been constructed successfully and expressed in Escherichia coli by using pET-32a expression vector. The polyclonal antibody for rabbit has been successfully obtained. The expression of gcTRAF1 in different organs was examined by real-time quantitative PCR and Western blotting, respectively. It was widely distributed in heart, head kidney, thymus, brain, gill, liver, spleen, and trunk kidney. This is the first report of TRAF1 homologue molecule found in fish. (c) 2007 Elsevier B.V. All rights reserved.

(Table 1) Maceral composition and organic carbon chemistry of ODP Leg 104 samples

The Cenozoic sediments sampled in ODP Leg 104 on the Vøring Plateau show a distinct variability of the total organic carbon content (TOC) and the accumulation rates of TOC. Based on the geochemical and organic-petrographic characterization of the sedimentary organic matter (OM), the allochthonous and autochthonous proportion of the OM could be quantified. The results clearly demonstrate that high TOC percentages and TOC accumulation rates in Cenozoic sediment sections display a generally high input of allochthonous organic matter. Oxidized and partly well-rounded organic particles built up the main portion of OM within the Miocene, TOC-rich sediments. The most probable source of this oxidized OM are reworked sediments from the Scandinavian shelf. Changes in the input of these organic particles are to some degree correlative with sea-level changes. The Cenozoic accumulation of autochthonous OM is low and does not reveal a clear variation during the Miocene and early Pliocene. In spite of a high accumulation rate of biogenic opal during the Early Miocene, the accumulation rate of autochthonous TOC is low. The autochthonous particle assemblage is dominated by relatively inert OM, like dinoflagellate cysts. This points to an intensive biological and/or early diagenetic degradation of the marine OM under well oxidized bottom water conditions during the last 23 Myr. Nevertheless, a continuation of marine OM degradation during later stages of diagenesis cannot be excluded. A prominent dominance of allochthonous OM over autochthonous is documented with the beginning of the Pliocene. At 2.45 Ma the episodic occurrence of ice-rafted, thermally mature OM reflects the onset of the glacial erosion of Mesozoic, coal and black shale bearing sediments on the Scandinavian and Barents Sea shelves. The first occurrence of these, in view of the actual burial depth, thermally overmature OM particles is, therefore, a marker for the beginning of the strong Scandinavian glaciation and the advance of the glacial front toward the shelves.