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

Abstract

In the original publication of Decker et al. (2020), 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 14 C dates of molluscs; the blue triangle indicates the D-GPS measured height a msl.

New Model of Coastal Evolution in the Ria de Vigo (NW Spain) from MIS2 to Present Day Based on the Aeolian Sedimentary Record

“…Therefore, this aeolisation stage could be extended to the whole southern half of the European Atlantic coast, also suggesting that the absolute ages of the aeolianites preserved in SW France [67,96,97] together with SW Iberia, Gibraltar and Canary Islands [22,62,68,69] are from MIS2 to Late Holocene. Based on the chronology established for other coastal aeolianite outcrops in Galicia [21], the model can also be applied to the penultimate glacial episode and the Eemian transgression, and could also be extended to other coastal areas worldwide where coastal aeolianites have been dated [80,[98][99][100][101][102][103][104][105].…”