Skip to main content
. 2013 Sep 30;110(42):16736–16741. doi: 10.1073/pnas.1315570110

Fig. 1.

Fig. 1.

Distribution of the elements and isotopes in Francevillian sediments used to reconstruct depositional environment (see also Fig. S1 for additional data), as also indicated on the figure. There may be a thin ferruginous interval near the top of the FB1b subunit as indicated. A reconstruction of relative sea-level trends is also shown as well as available chronological constraints.