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. 2017 Aug 29;7:9700. doi: 10.1038/s41598-017-10424-9

Figure 3.

Figure 3

(A) Total and (B) excess concentration profiles of 210Pb in dated mangrove soil cores of Central Red Sea. It was not possible to plot average values for the replicate cores against decompressed depths because replicate cores experienced different degrees of compaction during coring.