How does rising atmospheric CO2 affect marine organisms?

Click to locate material archived on our website by topic

Voring Plateau, Eastern Norwegian Sea
Andersson, C., Risebrobakken, B., Jansen, E. and Dahl, S.O.  2003.  Late Holocene surface ocean conditions of the Norwegian Sea (Voring Plateau).  Paleoceanography 18: 10.1029/2001PA000654.

August surface temperatures of the eastern Norwegian Sea's Voring Plateau (66.97N, 7.64E) were derived from planktic stable isotopes and foraminiferal assemblage concentrations.  The Medieval Warm Period occurred between AD 1200 and 1500 and was as much as 3.3C warmer than the Current Warm Period.