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1584 K. Lambeck et al. / Quaternary Science Reviews 23 (2004) 1567–1598

Fig. 3. Comparisons of observed (points with error bars) and predicted sea levels at tectonically stable sites. The upper and lower limits of the latter
are shown by the dashed lines. For Argentarola, both the terrestrial and marine ages for the speleothems are indicated. The inset in (d) is for the S.
Vito Lo Capo data points. Where results from several sites have been grouped into a single panel for illustrative convenience only, the predicted sea
levels for the time interval of observations vary by much less than their uncertainties and the predicted values shown correspond to representative
sites within each group: Gravisca in (c), S. Vito Lo Capo in (d), and northern Sardinia in (e).