Zobrazeno 1 - 10
of 4 308
pro vyhledávání: '"T. W. Lyons"'
Autor:
N. Kemnitz, W. M. Berelson, D. E. Hammond, L. Morine, M. Figueroa, T. W. Lyons, S. Scharf, N. Rollins, E. Petsios, S. Lemieux, T. Treude
Publikováno v:
Biogeosciences, Vol 17, Pp 2381-2396 (2020)
The Southern California Bight is adjacent to one of the world's largest urban areas, Los Angeles. As a consequence, anthropogenic impacts could disrupt local marine ecosystems due to municipal and industrial waste discharge, pollution, flood control
Externí odkaz:
https://doaj.org/article/c4b83577f36c4e8799a28282f502fa3b
Publikováno v:
Nature Communications, Vol 10, Iss 1, Pp 1-9 (2019)
The nature of the microbial reactions occurring during cap rock formation is poorly understood. Here the authors find that sulfur and carbon isotope signatures indicate sulfate-dependent anaerobic oxidation of methane (AOM) as a primary driver of cap
Externí odkaz:
https://doaj.org/article/9ee8445be4044640891cfa69a18b4ac9
Publikováno v:
Biogeosciences, Vol 12, Iss 7, Pp 2131-2151 (2015)
Long-term secular variation in seawater sulfate concentrations ([SO42−]SW) is of interest owing to its relationship to the oxygenation history of Earth's surface environment. In this study, we develop two complementary approaches for quantification
Externí odkaz:
https://doaj.org/article/bdf18b53fb6d4d2898949db41bfb949b
Publikováno v:
Geobiology. 10(3)
Mahoney Lake, British Columbia, Canada, is a stratified, 15-m deep saline lake with a euxinic (anoxic, sulfidic) hypolimnion. A dense plate of phototrophic purple sulfur bacteria is found at the chemocline, but to date the rest of the Mahoney Lake mi
Autor:
Oard, Michael J.
Publikováno v:
Creation Research Society Quarterly. Summer2024, Vol. 61 Issue 1, p16-31. 16p.
Publikováno v:
Geobiology. 7(5)
Autor:
Matsu'ura F; International Center for Isotope Effects Research, Nanjing University, Nanjing, Jiangsu, China.; Department of Earth and Planetary Sciences, Tokyo Institute of Technology, Tokyo, Japan.; Earth-Life Science Institute (WPI-ELSI), Tokyo Institute of Technology, Tokyo, Japan., Sawaki Y; Department of Earth Science and Astronomy Graduate School of Arts and Sciences, The University of Tokyo, Tokyo, Japan., Komiya T; Department of Earth Science and Astronomy Graduate School of Arts and Sciences, The University of Tokyo, Tokyo, Japan., Han J; Early Life Institute and Department of Geology and State Key Laboratory of Continental Dynamics, Northwest University, Xi'an, China., Maruyama S; Department of Earth and Planetary Sciences, Tokyo Institute of Technology, Tokyo, Japan., Ushikubo T; Kochi Institute for Core Sample Research, Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Nankoku, Kochi, Japan., Shimizu K; Kochi Institute for Core Sample Research, Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Nankoku, Kochi, Japan., Ueno Y; Department of Earth and Planetary Sciences, Tokyo Institute of Technology, Tokyo, Japan.; Earth-Life Science Institute (WPI-ELSI), Tokyo Institute of Technology, Tokyo, Japan.; Institute for Extra-Cutting-Edge Science and Technology Avant-Garde Research (X-Star), Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Yokosuka, Kanagawa, Japan.
Publikováno v:
Geobiology [Geobiology] 2024 Sep-Oct; Vol. 22 (5), pp. e12617.
Publikováno v:
Nature. 365:538-540
RECENT studies1–8 have documented significant short-term vertical fluctuations in the position of the oxic–anoxic interface (chemocline) in the waters of the Black Sea, the world's largest anoxic basin. Natural5,9 and anthropogenic3,4,8,10 influe
Autor:
Chonglong He1,2, Min Wang1,2, Bowu Dong1,2, Yaqiong Su1,2, Xin-Hua Duan1,2, Le Liu1,2 le.liu@xjtu.edu.cn
Publikováno v:
Green Synthesis & Catalysis. May2024, Vol. 5 Issue 2, p117-121. 5p.