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Autor:
Flake, Ryan Christopher
Previous studies have identified δ¹³C events in the Carboniferous that imply major shifts in the carbon cycle. However, inherent in this interpretation is the assumption that epicontinental seas are chemically representative of the global ocean. O
Externí odkaz:
http://hdl.handle.net/1969.1/ETD-TAMU-2011-05-9365
Autor:
Roark, Andrew, Flake, Ryan, Grossman, Ethan L., Olszewski, Thomas, Lebold, Joseph, Thomas, Debbie, Marcantonio, Franco, Miller, Brent, Raymond, Anne, Yancey, Thomas
Publikováno v:
In Palaeogeography, Palaeoclimatology, Palaeoecology 1 November 2017 485:136-153
