Marine carbon sinking rates confirm importance of polar oceans
Monday, July 25, 2016 - 17:31
in Earth & Climate
Results show that the transfer efficiency of organic carbon from the surface to the deep ocean About the same amount of atmospheric carbon that goes into creating plants on land goes into the bodies of tiny marine plants known as plankton. When these plants die and sink, bacteria feed on their sinking corpses and return their carbon to the seawater. When plankton sink deep enough before being eaten, this carbon is taken out of circulation as a greenhouse gas to remain trapped in the deep ocean for centuries.