Mechanism of translationally coupled mRNA turnover mediated by c-fos protein-coding-region determinant

Proto-oncogene c-fos is a member of the class of early-response genes whose transient expression plays a crucial role in cell proliferation, differentiation, and apoptosis. Degradation of c- fos mRNA is an important mechanism for controlling c-fos expression. Rapid mRNA turnover mediated by the protein-coding-region determinant (mCRD) of the c-fos transcript illustrates a functional interplay between mRNA turnover and translation that coordinately influences the fate of cytoplasmic mRNA. It is suggested that mCRD communicates with the 3′ poly(A) tail via an mRNP complex comprising mCRD-associated proteins, which prevents deadenylation in the absence of translation. Ribosome transit as a result of translation is required to alter the conformation of the mRNP complex, thereby eliciting accelerated deadenylation and mRNA decay. To gain further insight into the mechanism of mCRD-mediated mRNA turnover, Unr was identified as an mCRD-binding protein, and its binding site within mCRD was characterized. Moreover, the functional role for Unr in mRNA decay was demonstrated. The result showed that elevation of Unr protein level in the cytoplasm led to inhibition of mRNA destabilization by mCRD. In addition, GST pull-down assay and immuno-precipitation analysis revealed that Unr interacted with PABP in an RNA-independent manner, which identified Unr as a novel PABP-interacting protein. Furthermore, the Unr interacting domain in PABP was characterized. In vivo mRNA decay experiments demonstrated a role for Unr-PABP interaction in mCRD-mediated mRNA decay. In conclusion, the findings of this study provide the first evidence that Unr plays a key role in mCRD-mediated mRNA decay. It is proposed that Unr is recruited by mCRD to initiate the formation of a dynamic mRNP complex for communicating with poly(A) tail through PABP. This unique mRNP complex may couple translation to mRNA decay, and perhaps to recruit the responsible nuclease for deadenylation. ^

Geochemistry of bulk samples and various minerals of sediment core CRP-1 from the Ross Sea, Antarctica

Thirty-nine medium and fine grained sandstones from between 19,26 and 147,23 mbsf in the Cape Roberts-l core (CRP-1) were analysed for 10 major and 16 trace elements. Using whole-lock compositions, 9 samples were selected for analyses of mineral and glass grains by energy dispersive electron microscope. Laser-Ablation Mass-Spectrometry was used to determine rare earth elements and 14 additional trace elements in glass shards, pyroxenes and feldspars in order to examine their contribution to the bulk rock chemistry. Geochemical data reveal the major contribution played by the Granite Harbour Intrusives to the whole rock composition, even if a significant input is supplied by McMurdo volcanics and Ferrar dolerite pyroxenes McMurdo volcanics were studied in detail; they appeal to derive from a variety of litologies, and a dominant role of wind transpoitation from exposures of volcanic rocks may be inferred from the contemporary occurrence of different compositions at all depths. Only at 116.55 mbsf was a thin layer of tephra found, linked to an explosive eruption McMurdo volcanic rocks exhibit larger abundances at depths above 62 mbsf, in correspondence with the onset of volcanic activity in the McMurdo Sound area. From 62 mbsf to the bottom of the core, McMurdo volcanics are less abundant and probably issued from some centres in the McMurdo Sound region. However, available data do not allow the exclusion of wind transport from some eruptive centres active in north Victoria Land at the beginning of the Miocene Epoch.

A relationship between aerosol transport and compound-specific d13C land plant biomarker and pollen records

We examined near-surface, late Holocene deep-sea sediments at nine sites on a north-south transect from the Congo Fan (4°S) to the Cape Basin (30°S) along the Southwest African continental margin. Contents, distribution patterns and molecular stable carbon isotope signatures of long-chain n-alkanes (C27-C33) and n-alkanols (C22-C32) are indicators of land plant vegetation of different biosynthetic types, which can be correlated with concentrations and distributions of pollen taxa in the same sediments. Calculated clusters of wind trajectories and satellite Aerosol Index imagery afford information on the source areas for the lipids and pollen on land and their transport pathways to the ocean sites. This multidisciplinary approach on an almost continental scale provides clear evidence of latitudinal differences in lipid and pollen composition paralleling the major phytogeographic zonations on the adjacent continent. Dust and smoke aerosols are mainly derived from the western and central South African hinterland dominated by deserts, semi-deserts and savannah regions rich in C4 and CAM plants. The northern sites (Congo Fan area and northern Angola Basin), which get most of their terrestrial material from the Congo Basin and the Angolan highlands, may also receive some material from the Chad region. Very little aerosol from the African continent is transported to the most southerly sites in the Cape Basin. As can be expected from the present position of the phytogeographic zones, the carbon isotopic signatures of the n-alkanes and n-alkanols both become isotopically more enriched in 13C from north to south. The results of the study suggest that this combination of pollen data and compound-specific isotope geochemical proxies can be effectively applied in the reconstruction of past continental phytogeographic developments.