Search Results - Okinawa SV~

Microbial community in a sediment-hosted CO2 lake of the southern Okinawa Trough hydrothermal system by Inagaki, F., Kuypers, M., Tsunogai, U., Ishibashi, J., Nakamura, K., Treude, T., Ohkubo, S., Nakaseama, M., Gena, Kaul, Chiba, H., Hirayama, H., Nunoura, T., Takai, K., Jorgensen, B., Horikoshi, K., Boetius, A.

“…We report here a biogeochemical and microbiological characterization of a microbial community inhabiting deep-sea sediments overlying a natural CO2 lake at the Yonaguni Knoll IV hydrothermal field, southern Okinawa Trough. …”
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Environmental DNA can act as a biodiversity barometer of anthropogenic pressures in coastal ecosystems by Di Battista, Joey, Reimer, J.D., Stat, Michael, Masucci, G.D., Biondi, P., De Brauwer, Maarten, Wilkinson, S.P., Chariton, A.A., Bunce, Michael

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Cenozoic inversion of the East China Sea Shelf Basin: Implications for reconstructing Cenozoic tectonics of eastern China by Su, J., Zhu, W., Chen, J., Ge, Rongfeng, Zheng, B., Min, B.

“…Structural inversions have superimposed on the Cenozoic extensional rift basin during these compression events, forming regional unconformity reflectors (T4°, T3°, T2°, and T1°). The Changjiang Depression located in the north of the West Rift Region is characterized by a number of NW-, EW-, to NE-trending faults. …”
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Chimneys in Paleozoic massive sulfide mounds of the Urals VMS deposits: Mineral and trace element comparison with modern black, grey, white and clear smokers by Maslennikov, V., Maslennikova, S., Large, R., Danyushevsky, L., Herrington, R., Ayupova, N., Zaykov, V., Lein, A., Tseluyko, A., Melekestseva, I., Tessalina, Svetlana

“…In the same range, the buffering capacity of host rocks decreases in contrast to the increase in ƒS2 and ƒO2. With the exception of the Safyanovskoye deposit, trace element assemblages in chalcopyrite vary to reflect the host rock: ultramafic (high Se, Sn, Co, Ni, Ag and Au) → mafic (high Co, Se, Mo and low Bi, Au and Pb) → bimodal mafic (high Te, Au, Ag, Bi, Pb, Co, moderate Se, and variable As and Sb) → bimodal felsic (high As, Sb, Mo, Pb, moderate Bi, and low Co, Te and Se). …”
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