Searching the hearts of graphene-like molecules for simplicity, sensitivity and logic

If quantum interference patterns in the hearts of polycyclic aromatic hydrocarbons (PAHs) could be isolated and manipulated, then a significant step towards realizing the potential of single-molecule electronics would be achieved. Here we demonstrate experimentally and theoretically that a simple, parameter-free, analytic theory of interference patterns evaluated at the mid-point of the HOMO-LUMO gap (referred to as M-functions) correctly predicts conductance ratios of molecules with pyrene, naphthalene, anthracene, anthanthrene or azulene hearts. M-functions provide new design strategies for identifying molecules with phase-coherent logic functions and enhancing the sensitivity of molecular-scale interferometers.

Significance of signal transducer and activator of transcription 3 during multistage mouse skin carcinogenesis

Signal transducer and activator of transcription 3 (Stat3) is a signaling molecule that transduces signal from cell surface receptors, itself translocates into the nucleus, binds to consensus promoter sequences and activates gene transcription. Here, we showed that Stat3 is constitutively activated in both premalignant tumors (papillomas) and squamous cell carcinomas of mouse skin that is induced by topical treatment with an initiator 7,12-dimethylbenz[a]anthracene (DMBA) followed by a tumor promoter 12-O-tetradecanoyl-phorbol-13-acetate (TPA). Additional data demonstrated that epidermal growth factor signaling contributes to the activation of Stat3 in this model. Using mice where Stat3 function is abrogated in keratinocytes via the Cre-LoxP system (K5Cre.Stat3 flox/flox), we demonstrated that Stat3 is required for de novo carcinogenesis since Stat3 deficiency leads to a complete abrogation of skin tumor development induced by DMBA and TPA. We subsequently showed that Stat3 plays a role in both the initiation and promotion stages of carcinogenesis. During initiation, Stat3 functions as an anti-apoptotic molecule for maintaining the survival of DNA-damaged keratinocyte stem cells. During promotion, Stat3 functions as a critical regulator for G1 to S phase cell cycle progression to confer selective clonal expansion of initiated cells into papillomas. On the other hand, using transgenic mice over-expressing a constitutively dimerized form of Stat3 (Stat3C) in keratinocytes (K5.Stat3C), we revealed a role for Stat3 in tumor progression. After treatment with DMBA and TPA, K5.Stat3C transgenic mice developed skin tumors with a shorter latency when 100% bypassed the premalignant stage and became carcinoma in situ. Histological and immunohistochemical analysis revealed these tumors as highly vascularized and poorly differentiated. More strikingly, these tumors exhibited invasion into surrounding mesenchymal tissue, some of which metastasized into lung. The tumor-mesenchymal front was characterized by partial loss of E-cadherin and elevation of vimentin, markers characterizing epithelial-mesenchymal transition. On the other hand, inhibition of Stat3 via a decoy oligonucleotide led to a significant reduction of tumor size in approximately 50% of all papillomas tested. In conclusion, we demonstrated that Stat3 plays a critical in all three stages (initiation, promotion and progression) of skin carcinogenesis, and it may potentially become a good target for cancer prevention and anti-cancer therapy. ^

Organic compounds in snow, ice, and sub-ice waters from the mouth of the Severnaya Dvina River and the Kandalaksha Gulf (White Sea)

The paper reports data on concentrations of organic compounds (organic carbon, lipids; aliphatic hydrocarbons, and polycyclic aromatic hydrocarbons) in snow, ice, and sub-ice waters from the mouth of the Severnaya Dvina River in March 2005-2007 and the Kandalaksha Gulf (Chupa Bay) in March 2004. It was established that organic compounds are accumulated in snow and the upper ice layer near Archangelsk city. Distribution of molecular markers indicates that pollutions were mainly caused by local fallouts. In the Chupa Bay organic compounds are concentrated in the lower ice layer; it is typical for Arctic snow-ice cover. High contents of organic compounds in the snow-ice cover of the White Sea are caused by pollution of air and water during the winter season.

Geochemistry of pockmark sediments from the inner Oslofjord

Pockmarks are geological features that are found on the bottom of lakes and oceans all over the globe. Some are active, seeping oil or methane, while others are inactive. Active pockmarks are well studied since they harbor specialized microbial communities that proliferate on the seeping compounds. Such communities are not found in inactive pockmarks. Interestingly, inactive pockmarks are known to have different macrofaunal communities compared to the surrounding sediments. It is undetermined what the microbial composition of inactive pockmarks is and if it shows a similar pattern as the macrofauna. The Norwegian Oslo Fjord contains many inactive pockmarks and they are well suited to study the influence of these geological features on the microbial community in the sediment. Here we present a detailed analysis of the microbial communities found in three inactive pockmarks and two control samples at two core depth intervals. The communities were analyzed using high-throughput amplicon sequencing of the 16S rRNA V3 region. Microbial communities of surface pockmark sediments were indistinguishable from communities found in the surrounding seabed. In contrast, pockmark communities at 40 cm sediment depth had a significantly different community structure from normal sediments at the same depth. Statistical analysis of chemical variables indicated significant differences in the concentrations of total carbon and non-particulate organic carbon between 40 cm pockmark and reference sample sediments. We discuss these results in comparison with the taxonomic classification of the OTUs identified in our samples. Our results indicate that microbial surface sediment communities are affect by the water column, while the 40 cm communities are affect by local conditions within the sediment.

Extractable hydrocarbon and carbon isotope geochemistry of Lower Cretaceous sediments of the Exmouth Plateau

The organic geochemical character of rocks selected from Aptian, Valanginian, and Berriasian clay stone and siltstone sequences encountered in Ocean Drilling Program (ODP) Holes 762C and 763C on the Exmouth Plateau was determined by means of a variety of analytical procedures. These sequences represent distal portions of the Mesozoic Barrow delta, in which petroleum source rocks and reservoirs exist on the Australian continent. The organic matter at the ODP sites is thermally immature type III material. Biomarker hydrocarbon compositions are dominated by long-chain, waxy n-alkanes and by C29 steranes, which reflect the land-plant origin of organic matter. Organic carbon d13C values ranged from -26 per mil to -28 per mil, consistent with a C3 land-plant source. Kerogen pyrolysate compositions and hopane isomerization ratios revealed progressively larger contributions of recycled organic matter as the depth of the deltaic sedimentary layers became greater.

Alkane and hydrocarbon concentrations of ODP Leg 104 sites

Sedimentary extractable organic matter was analyzed at three ODP Leg 104 sites in the Norwegian Sea. Organic carbon content ranged from less than 0.1% to a maximum of 1.8%. Extractable organic matter content and unresolved complex mixture concentrations were low and randomly distributed. Low levels of aliphatic (branched and normal) and aromatic hydrocarbons were detected in all of the sediments analyzed. Total aliphatic and aromatic hydrocarbon concentrations ranged from 176 to 3,214 and 6 to 820 ppb, respectively. The concentrations of individual aliphatic (n-C15 to n-C32) and aromatic (two- to five-ring) hydrocarbons were generally less than 50 ppb and less than 10 ppb, respectively. No significant trend with sub-bottom depth was observed in either bulk organic matter or individual hydrocarbon concentrations. The predominant source of Cenozoic sedimentary hydrocarbons is concluded to be ice-rafted debris from the adjacent continent. All sites contain a mixture of recycled, mature petroleum-related and terrestrially derived hydrocarbons.

Geological, geochemical and biogeochemical data on boundary zones of the Atlantic Ocean

Results of studies in two biogeochemically active zones of the Atlantic Ocean (the Benguela upwelling waters and the region influenced by the Congo River run-off) are reported in the book. A multidisciplinary approach included studies of the major elements of the ocean ecosystem: sea water, plankton, suspended matter, bottom sediments, interstitial waters, aerosols, as well as a wide complex of oceanographic studies carried out under a common program. Such an approach, as well as a use of new methodical solutions led to obtaining principally new information on different aspects of oceanology.