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of 453
pro vyhledávání: '"Turchyn AV"'
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Bioturbation enhances mixing between the seafloor and overlying ocean due to changes the redox state of the sediment and influences the biogeochemical cycling of redox-sensitive elements such as sulfur. Before the widespread
Bioturbation enhances mixing between the seafloor and overlying ocean due to changes the redox state of the sediment and influences the biogeochemical cycling of redox-sensitive elements such as sulfur. Before the widespread
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2a85a213d1746721db67c18499806d15
Autor:
Halevy I; Earth and Planetary Sciences, Weizmann Institute of Science, Rehovot 76100, Israel., Fike DA; Earth and Planetary Sciences, Washington University in St. Louis, St. Louis, MO 63130-4899, USA., Pasquier V; Earth and Planetary Sciences, Weizmann Institute of Science, Rehovot 76100, Israel., Bryant RN; Earth and Planetary Sciences, Washington University in St. Louis, St. Louis, MO 63130-4899, USA.; Earth, Atmospheric and Planetary Sciences, Purdue University, W. Lafayette, IN 47907, USA., Wenk CB; Earth and Planetary Sciences, Weizmann Institute of Science, Rehovot 76100, Israel., Turchyn AV; Earth Sciences, University of Cambridge, Cambridge CB2 3EQ, UK., Johnston DT; Earth and Planetary Sciences, Harvard University, Cambridge, MA 02138, USA., Claypool GE; 8910 West Jewell Avenue, Unit 209, Lakewood, CO 80232, USA.
Publikováno v:
Science (New York, N.Y.) [Science] 2023 Nov 24; Vol. 382 (6673), pp. 946-951. Date of Electronic Publication: 2023 Nov 23.
Autor:
Lomakina AV; Limnological Institute, SB RAS, Irkutsk, Russia., Bukin SV; Limnological Institute, SB RAS, Irkutsk, Russia., Pogodaeva TV; Limnological Institute, SB RAS, Irkutsk, Russia., Turchyn AV; Department of Earth Sciences, University of Cambridge, Cambridge, UK., Khlystov OM; Limnological Institute, SB RAS, Irkutsk, Russia., Khabuev AV; Limnological Institute, SB RAS, Irkutsk, Russia., Ivanov VG; Limnological Institute, SB RAS, Irkutsk, Russia., Krylov AA; Limnological Institute, SB RAS, Irkutsk, Russia.; VNIIOkeangeologia, St. Petersburg, Russia.; Institute of Earth Science, St Petersburg State University, St. Petersburg, Russia., Zemskaya TI; Limnological Institute, SB RAS, Irkutsk, Russia.
Publikováno v:
Geobiology [Geobiology] 2023 Nov; Vol. 21 (6), pp. 770-790. Date of Electronic Publication: 2023 Sep 12.
During the Early Toarcian, volcanic gases released by the Karoo-Ferrar large igneous province are widely believed to have caused severe environmental disturbances, including ocean acidification. Here we show records of δ Ca and δ Sr through the Ear
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c896b3145602027829516a099084d8c6
Autor:
Bradbury, HJ, Turchyn, AV
Previous attempts to quantify the amount of sedimentary carbonate precipitation in modern marine sediments have been derived from the flux of calcium into the sediments due to diffusion under assumed steady state, the application of Fick's first law,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::74543d5c310cfb7283e634a8032ffbce
https://www.repository.cam.ac.uk/handle/1810/292210
https://www.repository.cam.ac.uk/handle/1810/292210
The measurement of isotope ratios in sedimentary rocks deposited over geological time can provide key insights to past environmental change over important intervals in the past. However, it is important to be aware that secondary alteration can overp
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::2fea34f207b097100ac16d6c9a31c27f
An accurate description of the carbonate system in porewaters is valuable in studies involving the degradation of sedimentary organic matter, recrystallization of calcium carbonate minerals, calculations of mineral saturation state and cycling of ion
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::94d9058b7d74e473feafc19b20f9a4ab
Autor:
Levy EJ; Department of Earth and Environmental Sciences, Ben-Gurion University of the Negev, Beer Sheva, Israel.; Geological Survey of Israel, Jerusalem, Israel.; Department of Climate Geochemistry, Max Planck Institute for Chemistry, Mainz, Germany., Thomas C; Department of Earth Sciences, University of Geneva, Geneva, Switzerland., Antler G; Department of Earth and Environmental Sciences, Ben-Gurion University of the Negev, Beer Sheva, Israel.; The Interuniversity Institute for Marine Sciences in Eilat, Eilat, Israel., Gavrieli I; Geological Survey of Israel, Jerusalem, Israel., Turchyn AV; Department of Earth Sciences, University of Cambridge, Cambridge, UK., Grossi V; Laboratoire de Géologie de Lyon, Univ. Lyon 1, CNRS, ENSL, Villeurbanne, France., Ariztegui D; Department of Earth Sciences, University of Geneva, Geneva, Switzerland., Sivan O; Department of Earth and Environmental Sciences, Ben-Gurion University of the Negev, Beer Sheva, Israel.
Publikováno v:
Geobiology [Geobiology] 2022 Jul; Vol. 20 (4), pp. 518-532. Date of Electronic Publication: 2022 Apr 05.
Autor:
Góngora, Esteban1 (AUTHOR) esteban.gongora@mail.mcgill.ca, Lirette, Antoine-O.1 (AUTHOR), Freyria, Nastasia J.1 (AUTHOR), Greer, Charles W.1,2 (AUTHOR), Whyte, Lyle G.1 (AUTHOR)
Publikováno v:
Environmental Microbiome. 9/18/2024, Vol. 19 Issue 1, p1-17. 17p.
We studied one cycle (Cycle 6) of gypsum-marl deposition from the Messinian Yesares Member in Sorbas Basin, Spain. The objective was to reconstruct the changing environment of deposition and its relation to astronomically-forced climate change. The
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______109::274a61e86dbaf5dacbd1545bf55c967c
https://www.repository.cam.ac.uk/handle/1810/249212
https://www.repository.cam.ac.uk/handle/1810/249212