Abstract
Rates of denitrification below some oceanic upwelling zones reach a maximum during periods when sea level rise was fastest throughout the Pleistocene glacial cycles. Nitrogen isotope data from North American shales deposited 300 million years ago during Palaeozoic glaciations are indicative of a similar pattern.
Full Text 
Sign-in/Register to access full text options
Sign-in/Register to access full text options 
Published version (
Free)
Free) 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a call
