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I would like to remove the mention of Peter Ward in this article. The work by Peter Ward is not relevant in explaining the Canfield Ocean. This page should instead focus on the hypothesis put forward by Daniel Canfield and explain what his theory suggested.- SeaMonsterFromTheDeep 10:30 PM, 1 March 2016 (UTC)
The leading reference on page 452 (top paragraph) describes the euxinic conditions, which lead to the mass extinction - based on an anoxic and sulfidic ocean.
http://ebme.marine.rutgers.edu/HistoryEarthSystems/HistEarthSystems_Fall2008/Week5b/Canfield_Nature_1998.pdf
Explanation
https://en.wiktionary.org/wiki/euxinic
There are 3 main studies in this page which all relate to euxinic conditions, after renaming to Euxinia, the studies could be listed under "Models".
Prokaryotes (
talk)
01:15, 21 September 2013 (UTC)
Definition of Euxinia = the presence of free sulfide (Kemp et al., 2009) http://geology.gsapubs.org/content/41/4/523.full ) Prokaryotes ( talk) 03:26, 21 September 2013 (UTC)
This study connects Strangelove Ocean to Euxinia
http://siberia.mit.edu/sites/siberia.mit.edu/files/articles_news_press/Meyer-Payne-EPSL-2011.pdf Quote = Two contrasting scenarios could relate euxinia to the associated state of marine productivity during the Permian and Triassic. Climate warming at the end of the Permian could have reduced rates of physical circulation, leading to oceanic anoxia and to a collapse of the biological pump (Rampino and Caldeira, 2005)
Above study points to this study, which gives more insights on Strangelove Ocean, Major perturbation of ocean chemistry and a ‘Strangelove Ocean’ after the end-Permian mass extinction Though maybe Strangelvoe Ocean should become an article on it's own, but given the short page here and possible renaming to a more general term like Euxinia could be enough to have 1 section for the Strangelove Ocean model. There is also the article on Anoxic events in general, /info/en/?search=Anoxic_event Prokaryotes ( talk) 03:12, 21 September 2013 (UTC)
I have decided to classify this article as a stub. After removing the peacock words highlighted by others, there remained no indication, in particular in secondary sources, of the notability or acceptance of this theory. The coverage is simply not encyclopedic. Hairy Dude ( talk) 16:53, 12 February 2021 (UTC)
This article was the subject of a Wiki Education Foundation-supported course assignment, between 11 January 2023 and 21 April 2023. Further details are available on the course page. Student editor(s): Dclark57 ( article contribs). Peer reviewers: Sdenviogeo.
— Assignment last updated by MethanoJen ( talk) 20:04, 13 January 2023 (UTC)
This article is rated Start-class on Wikipedia's
content assessment scale. It is of interest to the following WikiProjects: | |||||||||||
|
I would like to remove the mention of Peter Ward in this article. The work by Peter Ward is not relevant in explaining the Canfield Ocean. This page should instead focus on the hypothesis put forward by Daniel Canfield and explain what his theory suggested.- SeaMonsterFromTheDeep 10:30 PM, 1 March 2016 (UTC)
The leading reference on page 452 (top paragraph) describes the euxinic conditions, which lead to the mass extinction - based on an anoxic and sulfidic ocean.
http://ebme.marine.rutgers.edu/HistoryEarthSystems/HistEarthSystems_Fall2008/Week5b/Canfield_Nature_1998.pdf
Explanation
https://en.wiktionary.org/wiki/euxinic
There are 3 main studies in this page which all relate to euxinic conditions, after renaming to Euxinia, the studies could be listed under "Models".
Prokaryotes (
talk)
01:15, 21 September 2013 (UTC)
Definition of Euxinia = the presence of free sulfide (Kemp et al., 2009) http://geology.gsapubs.org/content/41/4/523.full ) Prokaryotes ( talk) 03:26, 21 September 2013 (UTC)
This study connects Strangelove Ocean to Euxinia
http://siberia.mit.edu/sites/siberia.mit.edu/files/articles_news_press/Meyer-Payne-EPSL-2011.pdf Quote = Two contrasting scenarios could relate euxinia to the associated state of marine productivity during the Permian and Triassic. Climate warming at the end of the Permian could have reduced rates of physical circulation, leading to oceanic anoxia and to a collapse of the biological pump (Rampino and Caldeira, 2005)
Above study points to this study, which gives more insights on Strangelove Ocean, Major perturbation of ocean chemistry and a ‘Strangelove Ocean’ after the end-Permian mass extinction Though maybe Strangelvoe Ocean should become an article on it's own, but given the short page here and possible renaming to a more general term like Euxinia could be enough to have 1 section for the Strangelove Ocean model. There is also the article on Anoxic events in general, /info/en/?search=Anoxic_event Prokaryotes ( talk) 03:12, 21 September 2013 (UTC)
I have decided to classify this article as a stub. After removing the peacock words highlighted by others, there remained no indication, in particular in secondary sources, of the notability or acceptance of this theory. The coverage is simply not encyclopedic. Hairy Dude ( talk) 16:53, 12 February 2021 (UTC)
This article was the subject of a Wiki Education Foundation-supported course assignment, between 11 January 2023 and 21 April 2023. Further details are available on the course page. Student editor(s): Dclark57 ( article contribs). Peer reviewers: Sdenviogeo.
— Assignment last updated by MethanoJen ( talk) 20:04, 13 January 2023 (UTC)