In the original publication of Decker et al. (Reference Decker, Falkenroth, Lindauer, Landgraf, Al-Lawati, Al-Rahbi, Franz and Hoffmann2020), Figures 6, 7, and 8 were incorrectly labelled. The correct figures and their captions are reproduced below:
![](https://static.cambridge.org/binary/version/id/urn:cambridge.org:id:binary:20210322012955584-0650:S0033589421000065:S0033589421000065_fig1.png?pub-status=live)
Figure 6. The shell midden south of Ras ar Ru'ays showing the underlying fluvial deposits. The stars mark the 14C dates of molluscs; the blue triangle indicates the D-GPS measured height a msl. (For interpretation of the references to color in this figure legend, the reader is referred to the web version of this article.)
![](https://static.cambridge.org/binary/version/id/urn:cambridge.org:id:binary:20210322012955584-0650:S0033589421000065:S0033589421000065_fig2.png?pub-status=live)
Figure 7. (color online) Bivalve shells were the most abundant species found in the shell midden of Ras ar Ru'ays (exterior shown at left, interior shown at right): 1, Anadara cf. antiquata; 2, Marcia sp.; 3–5, oyster; 3, imprint of a Terebralia palustris shell in an oyster shell; 6, Marcia sp.; 7, Chlamys townsendi; 8, Strombus sp.; 9, Terebralia palustris; 10, Cerithidea cingulata; 11, broken Conus sp.; 12, Cerithidium sp.; 13, broken Strombus sp.; 14, Nerita sp.
![](https://static.cambridge.org/binary/version/id/urn:cambridge.org:id:binary:20210322012955584-0650:S0033589421000065:S0033589421000065_fig3.png?pub-status=live)
Figure 8. (color online) Coastal cliff outcrops near As Sulayb and Al Haddah showing a succession of radiolarian chert unconformly overlain by coastal deposits. The sediments indicate that the last sea-level highstand was before 43.5 ka.