Title: Did the Proterozoic ‘Canfield Ocean’ cause a laughing gas greenhouse?
Abstract: GeobiologyVolume 5, Issue 2 p. 97-100 Did the Proterozoic 'Canfield Ocean' cause a laughing gas greenhouse? R. BUICK, R. BUICK Department of Earth & Space Sciences and Astrobiology Program, University of Washington, Seattle WA 98195-1310, USASearch for more papers by this author R. BUICK, R. BUICK Department of Earth & Space Sciences and Astrobiology Program, University of Washington, Seattle WA 98195-1310, USASearch for more papers by this author First published: 09 May 2007 https://doi.org/10.1111/j.1472-4669.2007.00110.xCitations: 79Read the full textAboutPDF ToolsRequest permissionExport citationAdd to favoritesTrack citation ShareShare Give accessShare full text accessShare full-text accessPlease review our Terms and Conditions of Use and check box below to share full-text version of article.I have read and accept the Wiley Online Library Terms and Conditions of UseShareable LinkUse the link below to share a full-text version of this article with your friends and colleagues. Learn more.Copy URL Share a linkShare onEmailFacebookTwitterLinkedInRedditWechat References Anbar AD, Knoll AH (2002) Proterozoic ocean chemistry and evolution: a bioinorganic bridge? Science 297, 1137–1142. Arnold GL, Anbar AD, Barling J, Lyons TW (2004) Molybdenum isotope evidence for widespread anoxia in mid-Proterozoic oceans. Science 304, 87–90. Barley ME, Groves DI (1992) Supercontinent cycles and the distribution of metal deposits through time. Geology 20, 291–294. Beaumont V, Robert, F (1999) Nitrogen isotope ratios of kerogens in Precambrian cherts: a record of the evolution of atmospheric chemistry? Precambrian Research 96, 63–82. Brocks JJ, Love GD, Summons RE, Knoll AH, Logan GA, Bowden SA (2005) Biomarker evidence for green and purple sulphur bacteria in a stratified Palaeoproterozoic sea. Nature 437, 866–870. Buick R, Des Marais DJ, Knoll AH (1995) Stable isotopic compositions of carbonates from the Mesoproterozoic Bangemall Group, northwestern Australia. Chemical Geology 123, 153–171. Canfield DE (1998) A new model for Proterozoic ocean chemistry. Nature 396, 450–453. Claire MW, Catling DC, Zahnle KJ (2006) Biogeochemical modelling of the rise in atmospheric oxygen. Geobiology 4, 239–269. Granger J, Ward BB (2003) Accumulation of nitrogen oxides in copper-limited cultures of denitrifying bacteria. Limnology and Oceanography 48, 313–318. Haltia T, Brown K, Tegoni M, Cambillau C, Saraste M, Mattila K, Djinovi-Carugo K (2003) The crystal structure of nitrous oxide reductase from Paracoccus denitrificans at 1.6 Å resolution. Biochemical Journal 369, 77–88. Hayes JM (1994) Global methanotrophy at the Archean-Proterozoic transition. In Early Life on Earth (ed. S Bengtson). Columbia University Press, New York, pp. 220–236. Johnston DT, Poulton SW, Fralick PW, Wing BA, Canfield DE, Farquhar J (2006) Evolution of the oceanic sulfur cycle at the end of the Paleoproterozoic. Geochimica et Cosmochimica Acta 70, 5723–5739. Kah LC, Lyons TW, Frank TD (2004) Low marine sulphate and protracted oxygenation of the Proterozoic biosphere. Nature 431, 834–838. Kasting JF (1993) Earth's early atmosphere. Science 259, 920–926. Knoll AH (1992) The early evolution of eukaryotes: a geological perspective. Science 256, 622–627. Morel FMM, Price NM (2003) The biogeochemical cycles of trace metals in the oceans. Science 300, 944–947. Poulton SW, Fralick PW, Canfield DE (2004) The transition to a sulphidic ocean ~1.84 billion years ago. Nature 431, 173–177. Rouxel OJ, Bekker A, Edwards KJ (2005) Iron isotope constraints on the Archean and Paleoproterozoic ocean redox state. Science 307, 1088–1091. Saito MA, Sigman DM, Morel FMM (2003) The bioinorganic chemistry of the ancient ocean: the co-evolution of cyanobacterial metal requirements and biogeochemical cycles at the Archean-Proterozoic boundary? Inorganica Chimica Acta 356, 308–318. Shen Y, Canfield DE, Knoll AH (2002) Middle Proterozoic ocean chemistry: evidence from the McArthur Basin, northern Australia. American Journal of Science 302, 81–109. Shen Y, Knoll AH, Walter MR (2003) Evidence for low sulphate and anoxia in a mid-Proterozoic marine basin. Nature 423, 632–635. Shields G, Veizer J (2002) Precambrian marine carbonate isotope database: version 1.1. Geochemistry Geophysics Geosystems 3, 12 pp. Zahnle KJ, Claire M, Catling D (2006) The loss of mass-independent fractionation in sulfur due to a Palaeoproterozoic collapse of atmospheric methane. Geobiology 4, 271–283. Zerkle AL, House CH, Cox RP, Canfield DE (2006) Metal limitation of cyanobacterial N2 fixation and implications for the Precambrian nitrogen cycle. Geobiology 4, 285–297. Citing Literature Volume5, Issue2June 2007Pages 97-100 ReferencesRelatedInformation
Publication Year: 2007
Publication Date: 2007-05-09
Language: en
Type: article
Indexed In: ['crossref']
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Cited By Count: 101
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