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==Untitled==
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I created this page based on a recent seminar that I gave on paleosalinity. The vast majority of statements in the article can a ascribed to the Sigman & Boyle 2000 paper and the Adkins 2002, but I haven't had time to dig out references for smaller things, such as 120m sea level drop, the changes in glabal salinity and so on; these are featured in the respective texts so they're certain to be accurate. <small><span class="autosigned">—Preceding [[Wikipedia:Signatures|unsigned]] comment added by [[User:Oliverjknevitt|Oliverjknevitt]] ([[User talk:Oliverjknevitt|talk]] • [[Special:Contributions/Oliverjknevitt|contribs]]) 20:40, 17 May 2010 (UTC)</span></small><!-- Template:Unsigned --> <!--Autosigned by SineBot-->
The vast majority of statements in the article can a ascribed to the Sigman & Boyle 2000 paper and the Adkins 2002, but I haven't had time to dig out references for smaller things, such as 120m sea level drop, the changes in glabal salinity and so on; these are featured in the respective texts so they're certain to be accurate. <small><span class="autosigned">—Preceding [[Wikipedia:Signatures|unsigned]] comment added by [[User:Oliverjknevitt|Oliverjknevitt]] ([[User talk:Oliverjknevitt|talk]] • [[Special:Contributions/Oliverjknevitt|contribs]]) 20:40, 17 May 2010 (UTC)</span></small><!-- Template:Unsigned --> <!--Autosigned by SineBot-->

Revision as of 11:38, 26 November 2010

Untitled

The vast majority of statements in the article can a ascribed to the Sigman & Boyle 2000 paper and the Adkins 2002, but I haven't had time to dig out references for smaller things, such as 120m sea level drop, the changes in glabal salinity and so on; these are featured in the respective texts so they're certain to be accurate. —Preceding unsigned comment added by Oliverjknevitt (talkcontribs) 20:40, 17 May 2010 (UTC)[reply]