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= Article Edited: [[Triassic–Jurassic extinction event|Triassic-Jurassic Extinction Event]] = |
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EDITS to page are <u>Underlined</u> |
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=== Written Critique: === |
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This article does have some strong elements, while some sections of the article need to be edited. Firstly, the article contains a general clear overview, however it is very short and needs more detail to be added. For example, the duration of the extinction needs to be added, more information needs to be added about the species affected and more information needs to given on the differentiation between the extinction within the marine, terrestrial and plant species. Likewise, there is no information given on the poor fossil record and issues in dating the times of extinction and the time of the T-J boundaryAdditionally, there is no chronological flow to the article, it is very scattered. For example, it only includes two sections other than the introduction, therefore more sections need to be added to better organize the article. Moreover, the wikipedia page only discusses one of the theories in depth for the extinction of Triassic period which is volcanism, but it did not explain the others possible theories in detail such as an asteroid impact, climate change, and the change in sea level. Furthermore, the article contains only 10 citations, however they do come from good reputable sources such as Nature and Science. Additionally, when following some of the links for the citations, they cannot be found so they need to be updated. One of these citations are the Origination, extinction, and mass depletions of marine diversity article. Likewise, one article is written in German and as such needs to be removed. Additionally, more updated articles need to be used instead of some of the dated ones. The article also includes some images which are useful and make the article more appealing, such as the image showing the ranges of families tetrapods through the Triassic and Early Jurassic. However, the image at the bottom of the article should be moved to the introduction section. Lastly, there is no apparent bias shown in the article, which is good. Overall, this article is a good starting point when learning about the Triassic-Jurassic extinction, however much more information needs to be added about the extinction and by following the suggestions made in the critique, the article will be polished. |
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= Suggested section headings: = |
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== Section title: Hypothesized Causes of Extinction == |
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Subheadings for diff. hypotheses: |
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=== Sea level fluctuations === |
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=== Bolide impact === |
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=== CAMP Volcanism === |
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Subsections on Effects of Volcanism: |
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==== Greenhouse warming and ocean acidification ==== |
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==== Sulfur dioxide outgassing and effects ==== |
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== Section title: Atmospheric shifts from carbon injection (re: massive carbon injection - Ruhl et al., 2011) == |
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== Section title: Classification of Triassic-Jurassic Extinction (re: whether or not the ETE is a mass extinction) == |
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== Section title: Current Research == |
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== Section title: Future Directions for Research == |
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'''Edits to Introduction:''' |
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The Triassic–Jurassic extinction event <u>which occurred approximately</u> [http://tools.wmflabs.org/timescale/?Ma=201.3 201.3] [[Myr|million years ago]],marks the boundary between the Triassic and [[Jurassic]] periods. <u>It lasted for an estimated duration of 40,000 to 500,000 years</u> and is one of the major [[Extinction event|extinction events]] of the [[Phanerozoic]] eon, which profoundly affected life on land and in the oceans (Stanley S.M. 1992). <u>An estimated 76% of all marine and terrestrial species and about 20 % of all taxonomic families went extinct</u> (Benton M.J. 1993). Additionally, in the seas, a whole [[Class (biology)|class]] ([[Conodont|conodonts]]) and 34% of marine genera disappeared.Whereas, on land, all [[Pseudosuchia|pseudosuchians]] (non-dinosaurian [[Archosaur|archosaurs]]) other than [[Crocodylomorpha|crocodylomorphs]] ([[Sphenosuchia]] and [[Crocodyliformes]]), some remaining [[Therapsid|therapsids]], and many of the large [[Amphibia|amphibians]] became extinct. <u>Lastly, close examinations of the Triassic–Jurassic extinction event show that the extinction was much more serious at the specific/species level than at generic and family levels</u><ref>{{Cite journal|last = Benton|first = M.J.|date = 1993|title = Late Triassic Extinctions and the Origin of the Dinosaurs|url =|journal = Science|doi =|pmid =|access-date =}}</ref> (Benton M.J. 1993). |
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Revision as of 16:59, 7 April 2016
Article Edited: Triassic-Jurassic Extinction Event
EDITS to page are Underlined
Written Critique:
This article does have some strong elements, while some sections of the article need to be edited. Firstly, the article contains a general clear overview, however it is very short and needs more detail to be added. For example, the duration of the extinction needs to be added, more information needs to be added about the species affected and more information needs to given on the differentiation between the extinction within the marine, terrestrial and plant species. Likewise, there is no information given on the poor fossil record and issues in dating the times of extinction and the time of the T-J boundaryAdditionally, there is no chronological flow to the article, it is very scattered. For example, it only includes two sections other than the introduction, therefore more sections need to be added to better organize the article. Moreover, the wikipedia page only discusses one of the theories in depth for the extinction of Triassic period which is volcanism, but it did not explain the others possible theories in detail such as an asteroid impact, climate change, and the change in sea level. Furthermore, the article contains only 10 citations, however they do come from good reputable sources such as Nature and Science. Additionally, when following some of the links for the citations, they cannot be found so they need to be updated. One of these citations are the Origination, extinction, and mass depletions of marine diversity article. Likewise, one article is written in German and as such needs to be removed. Additionally, more updated articles need to be used instead of some of the dated ones. The article also includes some images which are useful and make the article more appealing, such as the image showing the ranges of families tetrapods through the Triassic and Early Jurassic. However, the image at the bottom of the article should be moved to the introduction section. Lastly, there is no apparent bias shown in the article, which is good. Overall, this article is a good starting point when learning about the Triassic-Jurassic extinction, however much more information needs to be added about the extinction and by following the suggestions made in the critique, the article will be polished.
Suggested section headings:
Section title: Hypothesized Causes of Extinction
Subheadings for diff. hypotheses:
Sea level fluctuations
Bolide impact
CAMP Volcanism
Subsections on Effects of Volcanism:
Greenhouse warming and ocean acidification
Sulfur dioxide outgassing and effects
Section title: Atmospheric shifts from carbon injection (re: massive carbon injection - Ruhl et al., 2011)
Section title: Classification of Triassic-Jurassic Extinction (re: whether or not the ETE is a mass extinction)
Section title: Current Research
Section title: Future Directions for Research
Edits to Introduction:
The Triassic–Jurassic extinction event which occurred approximately 201.3 million years ago,marks the boundary between the Triassic and Jurassic periods. It lasted for an estimated duration of 40,000 to 500,000 years and is one of the major extinction events of the Phanerozoic eon, which profoundly affected life on land and in the oceans (Stanley S.M. 1992). An estimated 76% of all marine and terrestrial species and about 20 % of all taxonomic families went extinct (Benton M.J. 1993). Additionally, in the seas, a whole class (conodonts) and 34% of marine genera disappeared.Whereas, on land, all pseudosuchians (non-dinosaurian archosaurs) other than crocodylomorphs (Sphenosuchia and Crocodyliformes), some remaining therapsids, and many of the large amphibians became extinct. Lastly, close examinations of the Triassic–Jurassic extinction event show that the extinction was much more serious at the specific/species level than at generic and family levels[1] (Benton M.J. 1993).
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- ^ Benton, M.J. (1993). "Late Triassic Extinctions and the Origin of the Dinosaurs". Science.