Zobrazeno 1 - 10
of 758
pro vyhledávání: '"Grasby SE"'
Autor:
Li M; School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China., Xu Y; School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China., Sun L; School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China., Chen J; Institute of Surface-Earth System Science, School of Earth System Science, Tianjin University, Tianjin 300350, China., Zhang K; Institute of Surface-Earth System Science, School of Earth System Science, Tianjin University, Tianjin 300350, China., Li D; School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China., Farquhar J; Department of Geology and ESSIC, University of Maryland, College Park, MD 20742, USA., Zhang X; School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China., Sun R; Institute of Surface-Earth System Science, School of Earth System Science, Tianjin University, Tianjin 300350, China., Macdonald FA; Department of Earth Science, University of California-Santa Barbara, Santa Barbara, CA 93106, USA., Grasby SE; Geological Survey of Canada, Natural Resources Canada, Calgary, Alberta T2L 2A7, Canada., Fu Y; College of Resource and Environmental Engineering, Guizhou University, Guiyang 550012, China., Shen Y; School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China.
Publikováno v:
Science advances [Sci Adv] 2023 Sep 08; Vol. 9 (36), pp. eadh9502. Date of Electronic Publication: 2023 Sep 06.
Publikováno v:
Frontiers in Astronomy and Space Sciences
Elliptical sulfate-rich features, stained red by the presence of iron oxides, are set within permafrost and carbonate rock at Borup Fiord Pass in the Canadian High Arctic. These features, which vary in diameter from ∼0.5 to 3 m, exhibit the co-loca
Microbially induced sedimentary structures (MISS) are reportedly widespread in the Early Triassic and their occurrence is attributed to either the extinction of marine grazers (allowing mat preservation) during the Permo-Triassic mass extinction or t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=core_ac_uk__::168f8d39b9feb01fdb1eea2339b85ebd
https://eprints.whiterose.ac.uk/162282/1/918.pdf
https://eprints.whiterose.ac.uk/162282/1/918.pdf
Until recently, the biotic crisis that occurred within the Capitanian Stage (Middle Permian, ca. 262 Ma) was known only from equatorial (Tethyan) latitudes, and its global extent was poorly resolved. The discovery of a Boreal Capitanian crisis in Spi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=core_ac_uk__::717c705395702baff0214c693ccef6d0
Autor:
Foster WJ; Institute for Geology, Universität Hamburg, Hamburg, Germany.; Nagoya University, Nagoya, Japan., Godbold A; University of Southern California, Los Angeles, United States.; University of Tokyo, Tokyo, Japan., Brayard A; Université de Bourgogne, Bourgogne, France., Frank AB; Institute for Geology, Universität Hamburg, Hamburg, Germany., Grasby SE; Geological Survey of Canada, Calgary, Canada., Twitchett RJ; Natural History Museum, London, United Kingdom., Oji T; Nagoya University, Nagoya, Japan.
Publikováno v:
PeerJ [PeerJ] 2022 Dec 19; Vol. 10, pp. e14357. Date of Electronic Publication: 2022 Dec 19 (Print Publication: 2022).
Autor:
Ruhl IA; Department of Biological Sciences, University of Calgarygrid.22072.35, Calgary, Canada., Sheremet A; Department of Biological Sciences, University of Calgarygrid.22072.35, Calgary, Canada., Smirnova AV; Department of Biological Sciences, University of Calgarygrid.22072.35, Calgary, Canada., Sharp CE; Department of Geoscience, University of Calgarygrid.22072.35, Calgary, Canada., Grasby SE; Department of Geoscience, University of Calgarygrid.22072.35, Calgary, Canada.; Geological Survey of Canadagrid.470085.e, Calgary, Canada., Strous M; Department of Geoscience, University of Calgarygrid.22072.35, Calgary, Canada., Dunfield PF; Department of Biological Sciences, University of Calgarygrid.22072.35, Calgary, Canada.
Publikováno v:
MSystems [mSystems] 2022 Feb 22; Vol. 7 (1), pp. e0099121. Date of Electronic Publication: 2022 Feb 15.
Autor:
Ruhl IA; Department of Biological Sciences, University of Calgary, Calgary, AB, Canada., Sheremet A; Department of Biological Sciences, University of Calgary, Calgary, AB, Canada., Furgason CC; Department of Biological Sciences, University of Calgary, Calgary, AB, Canada., Krause S; Department of Biological Sciences, University of Calgary, Calgary, AB, Canada., Bowers RM; U.S. Department of Energy Joint Genome Institute, Berkeley, CA, United States., Jarett JK; U.S. Department of Energy Joint Genome Institute, Berkeley, CA, United States., Tran TM; Department of Biological Sciences, University of Calgary, Calgary, AB, Canada., Grasby SE; Department of Geoscience, University of Calgary, Calgary, AB, Canada.; Geological Survey of Canada, Calgary, AB, Canada., Woyke T; U.S. Department of Energy Joint Genome Institute, Berkeley, CA, United States., Dunfield PF; Department of Biological Sciences, University of Calgary, Calgary, AB, Canada.
Publikováno v:
Frontiers in microbiology [Front Microbiol] 2022 Jan 11; Vol. 12, pp. 787651. Date of Electronic Publication: 2022 Jan 11 (Print Publication: 2021).
Autor:
Hedhli M; Geological Survey of Canada, 3303-33rd Street NW, Calgary, AB T2L 2A7 Canada.; Department of Geoscience, University of Calgary, 2500 University Drive NW, Calgary, AB T2N 1N4 Canada., Dewing K; Geological Survey of Canada, 3303-33rd Street NW, Calgary, AB T2L 2A7 Canada., Beauchamp B; Department of Geoscience, University of Calgary, 2500 University Drive NW, Calgary, AB T2N 1N4 Canada., Grasby SE; Geological Survey of Canada, 3303-33rd Street NW, Calgary, AB T2L 2A7 Canada.; Department of Geoscience, University of Calgary, 2500 University Drive NW, Calgary, AB T2N 1N4 Canada., Meyer R; Department of Geoscience, University of Calgary, 2500 University Drive NW, Calgary, AB T2N 1N4 Canada.
Publikováno v:
Facies [Facies] 2022; Vol. 68 (4), pp. 15. Date of Electronic Publication: 2022 Jul 25.
Autor:
Li M; School of Earth and Space Sciences, University of Science and Technology of China, Hefei, China., Grasby SE; Geological Survey of Canada, Natural Resources Canada, Calgary, Alberta, Canada.; Department of Geoscience, University of Calgary, Calgary, Alberta, Canada., Wang SJ; State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing, China., Zhang X; School of Earth and Space Sciences, University of Science and Technology of China, Hefei, China., Wasylenki LE; School of Earth & Sustainability, Northern Arizona University, Flagstaff, AZ, USA., Xu Y; School of Earth and Space Sciences, University of Science and Technology of China, Hefei, China., Sun M; Department of Earth Sciences, ETH Zürich, Zürich, Switzerland., Beauchamp B; Department of Geoscience, University of Calgary, Calgary, Alberta, Canada., Hu D; School of Earth and Space Sciences, University of Science and Technology of China, Hefei, China., Shen Y; School of Earth and Space Sciences, University of Science and Technology of China, Hefei, China. yashen@ustc.edu.cn.
Publikováno v:
Nature communications [Nat Commun] 2021 Apr 01; Vol. 12 (1), pp. 2024. Date of Electronic Publication: 2021 Apr 01.