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Assessing the viability of using foraminifera from Mersey Estuary saltmarsh sediments to reconstruct former sea level

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Figure

Figure 1.2 Distortion of tidal wave propagating up a schematic estuary. The tidal amplitude varies as a result of changes in width (taken from Woodroffe (2003))
Figure 1.5 Summary of foraminifera assemblages relative to altitude of from British Isle and Ireland
Figure 2.9 Decoy Marsh from 1849 map.
Figure 4.6 Relative percentages of dead foraminifera abundance for OBSS3. Ordered by elevation from high (1) to low (22), with constrained cluster analysis based upon unweighted Euclidean distance
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