Talk:Cretaceous Thermal Maximum

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Wiki Education Foundation-supported course assignment

This article is or was the subject of a Wiki Education Foundation-supported course assignment. Further details are available on the course page. Student editor(s): Stillr. Peer reviewers: Twright71.

Above undated message substituted from Template:Dashboard.wikiedu.org assignment by PrimeBOT (talk) 18:38, 16 January 2022 (UTC)[reply]

Error messages in infobox

I don't think that this article should use {{Geological period}}, because that calls {{period start}} and {{Period end}} neither of which recognise "Cretaceous Thermal Maximum" as a period name. They're expecting something like "Cretaceous" on its own. --Redrose64 (talk) 17:13, 26 January 2010 (UTC)[reply]

Agreed, removed. There may be an alternative, but I haven't been able to find one. Mikenorton (talk) 18:34, 26 January 2010 (UTC)[reply]

Greetings

Hello,

My name is Stillr and I will be working on helping to improve this page for my Earth and Atmospheric Science class. I would appreciate any advice, notes, or general knowledge anyone has on the subject they would like to add or edit to. In addition, if anyone who has previously worked on the article before me has input or suggestions, feel free to contact me. Thank you for your time and I hope to contribute to this article to reflect the importance of this era on the development of life. While the article presents the topic in a straightforward manner, I believe adding more substance and ideas greatly enhances both the reader experience and takeaway.

Signed, Stillr (talk) 00:32, 5 September 2018 (UTC)[reply]

Source Bibliography

Sources to use for future reference.

1. Huber, Brian T; Hodell, David A; Hamilton, Christopher P. (1995). Middle-Late Cretaceous climate of the Southern High latitudes: Stable isotopic evidence for minimal equator-to-pole thermal gradients. Geology World. 107 (10): 1164-1191. https://pubs.geoscienceworld.org/gsa/gsabulletin/article/107/10/1164/182984/middle-late-Cretaceous-climate-of-the-southern

2. Jahren, A. Hope; Arens, Nan Crystal; Sarmiento, Gustavo; Guerrero, Javier; Amundson, Ronaldo (2001). Terrestrial record of methane hydrate dissociation in the Early Cretaceous. Geology. 29 (2): 159-162. https://pubs.geoscienceworld.org/gsa/geology/article/29/2/159/192003/terrestrial-record-of-methane-hydrate-dissociation.

3. Poulsen, Christopher J; Gendaszek, Andrew S; Jacob, Robert L (2003). Did the rifting of the Atlantic Ocean cause the Cretaceous thermal maximum? Geology. 31 (2): 115-118. https://pubs.geoscienceworld.org/gsa/geology/article/31/2/115/192533/did-the-rifting-of-the-atlantic-ocean-cause-the

4. McInerney, Francesca A; Wing, Scott L. (2011). The Paleocene-Eocene Thermal Maximum: A Perturbation of Carbon Cycle, climate, and biosphere with implications for the future. Annual Reviews of Earth and Atmospheric Science.39: 489-516. https://doi.org/10.1146/annurev-earth-040610-133431.

5. Puceat, Emmanuelle; Lecuyer, Christophe; Sheppard, Simon M.F; Dromart, Gilles; Reboulet, Stephane; Grandjean, Patricia (2003). Thermal evolution of Cretaceous Tethyan marine waters inferred from oxygen isotope composition of fish tooth enamels. Paleoceanography. 18 (2): 1029. https://doi.org/10.1029/2002PA000823.

Stillr (talk) 02:25, 17 September 2018 (UTC)[reply]