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. 2011 May 16;108(24):9776–9781. doi: 10.1073/pnas.1018670108

Fig. 4.

Fig. 4.

Core photograph from ODP site 959 showing the abrupt transition in TOC and MSA of the siliciclastic fraction compared to the evident bioturbated and laminated intervals. The laminated intervals are interpreted as the onset of anoxia and precede the rise in TOC and MSA.