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Well, all of the major glaciations are now in the Pleistocene, but there was plenty of higher latitude glaciation in the Piacenzian (Late Pliocene) from 3.2 to 2.8 mya. See, for example, [http://books.google.co.uk/books?id=KJBKC4qvV8AC&pg=RA1-PA275 page 275, column 2], in ''Applied Palaeontology'' by Robert Wynn Jones, who cites Thompson, R. S. and Fleming, R. F. (1996) "Middle Pliocene vegetation: reconstructions, paleoclimatic inferences, and boundary conditions for climate modeling" ''Marine Micropaleontology'' 27(1): pp. 27-49. --[[User:Bejnar|Bejnar]] ([[User talk:Bejnar|talk]]) 05:06, 29 August 2009 (UTC) |
Well, all of the major glaciations are now in the Pleistocene, but there was plenty of higher latitude glaciation in the Piacenzian (Late Pliocene) from 3.2 to 2.8 mya. See, for example, [http://books.google.co.uk/books?id=KJBKC4qvV8AC&pg=RA1-PA275 page 275, column 2], in ''Applied Palaeontology'' by Robert Wynn Jones, who cites Thompson, R. S. and Fleming, R. F. (1996) "Middle Pliocene vegetation: reconstructions, paleoclimatic inferences, and boundary conditions for climate modeling" ''Marine Micropaleontology'' 27(1): pp. 27-49. --[[User:Bejnar|Bejnar]] ([[User talk:Bejnar|talk]]) 05:06, 29 August 2009 (UTC) |
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== Blocked for one lol == |
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[[Image:Blokd no moar plz!.png|150px]] |
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You haz bin blocked for 1lol upon your request. ;-). Just kidding of course, that thread was hilarious. — <small><span style="border:1px solid #000000;padding:1px;"><b>[[User:Ched Davis|Ched]]</b> : [[User_talk:Ched Davis|<font style="color:#FFFFFF;background:#0000fa;"> ? </font>]]</span></small> 15:01, 31 August 2009 (UTC) |
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Please leave messages here for me - thanks!
If you leave me a message here, I will reply here. If I leave a message on your talk page, I will watch it, and continue the conversation there. When I reply to comments by newer users here, I'll typically leave a talkback tag on your talk page.
Diffs
Those diffs you wanted have been added to the ANI discussion. Factsontheground (talk) 22:41, 3 August 2009 (UTC)
- Thank you. They are very useful. As you are currently blocked, I will be watching your user talk page in case you wish to reply to this. Awickert (talk) 19:30, 5 August 2009 (UTC)
thanks
For reverting the spam on my talk. I haven't been on as much as I used to be. :D Wikifan12345 (talk) 18:34, 16 August 2009 (UTC)
- Always happy to wield the pooper scooper. Awickert (talk) 22:52, 16 August 2009 (UTC)
Ping! Satellite Temperature Graphic
You wanted a reminder....SunSw0rd (talk) 15:30, 18 August 2009 (UTC)
- Argh, yes, thanks, I need these. Just did it, will comment on the appropriate talk page. Awickert (talk) 19:35, 18 August 2009 (UTC)
A matter of opinion
I have come to the conclusion that editors with less than, say, 20% article space edits, without good reason (e.g., categorising, sysoping, tagging articles for wikiprojects) are a waste of time and mainly cause unnecessary drama that reduces our communal effectiveness at making information freely available. I am thereby roughly restricting myself to making at least 2-3 article space edits for every non-article-space edit (including useful ones, e.g., categorisation, AfD, and the rare productive talk page discussion). Awickert (talk) 17:46, 28 August 2009 (UTC)
Revised Pliocene glaciation
Well, all of the major glaciations are now in the Pleistocene, but there was plenty of higher latitude glaciation in the Piacenzian (Late Pliocene) from 3.2 to 2.8 mya. See, for example, page 275, column 2, in Applied Palaeontology by Robert Wynn Jones, who cites Thompson, R. S. and Fleming, R. F. (1996) "Middle Pliocene vegetation: reconstructions, paleoclimatic inferences, and boundary conditions for climate modeling" Marine Micropaleontology 27(1): pp. 27-49. --Bejnar (talk) 05:06, 29 August 2009 (UTC)
Blocked for one lol
You haz bin blocked for 1lol upon your request. ;-). Just kidding of course, that thread was hilarious. — Ched : ? 15:01, 31 August 2009 (UTC)