Dear Paleonetters: A colleague sent me a paleoclimatology query recently, as follows:
"All the fuss over 395 ppm or 398 ppm CO2, but not a word about what happens to O2 and its increase or decline. If late K O2 was 30-34%, where did it all go and is anyone looking at O2 over the last 10 MY for example ad obviously if O2 drops to 15-18% what happens. Just wondering." Any illumination welcomed directly to blayjo...@gmail.com Apologies for potential duplicate emails. Sincerely, Jorge Jorge A. Santiago-Blay, PhD blaypublishers.com 1. Positive experiences for authors of papers published in *LEB* http://blaypublishers.com/testimonials/ 2. Free examples of papers published in *LEB*: http://blaypublishers.com/category/previous-issues/. 3. *Guidelines for Authors* and page charges of *LEB*: http://blaypublishers.com/archives/ *.* 4. Want to subscribe to *LEB*? http://blaypublishers.com/subscriptions/ http://blayjorge.wordpress.com/ http://paleobiology.si.edu/staff/individuals/santiagoblay.cfm
