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Collapse of Holocene mangrove ecosystems along the coastline of Oman – Corrigendum

Published online by Cambridge University Press:  24 February 2021

Valeska Decker ,
Michaela Falkenroth ,
Susanne Lindauer ,
Jessica Landgraf ,
Zahra Al-Lawati ,
Huda Al-Rahbi ,
Sven Oliver Franz  and
Gösta Hoffmann
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Abstract

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Information

Type
Corrigendum
Information
Quaternary Research , Volume 100 , March 2021 , pp. 260 - 262
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Copyright
Copyright © University of Washington. Published by Cambridge University Press, 2021

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:

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.)

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.

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.

References

REFERENCE

Decker, V., Falkenroth, M., Lindauer, S., Landgraf, J., Al-Lawati, Z., Al-Rahbi, H., Franz, S. O., Hoffmann, G. Collapse of Holocene mangrove ecosystems along the coastline of Oman. First published online 29 December 2020. Quaternary Research, doi: https://doi.org/10.1017/qua.2020.96.CrossRefGoogle Scholar
Figure 0

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.)

Figure 1

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.

Figure 2

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.