Abstract
Seeliger M, Pint A, Frenzel P et al. (2021) Mid- to late-Holocene sea-level evolution of the northeastern Aegean sea. The Holocene 31(10): 1621–1634. doi: 10.1177/09596836211025967
The authors found some typos, noted below, in the previously published version of the article.
On page 2, last paragraph, the below sentence had an incorrect word ‘settlements’ They show tectonic uplift attested by human settlements of Pleistocene age on Thasos and at Chalkidiki (Figures 1 and 2; Armijo et al., 1999; Brückner et al., 2015; Maravelis et al., 2015; Sakellariou and Galanidou, 2015).
which is now replaced with the word ‘traces’. The new sentence reads as below They show tectonic uplift attested by human traces of Pleistocene age on Thasos and at Chalkidiki (Figures 1 and 2; Armijo et al., 1999; Brückner et al., 2015; Maravelis et al., 2015; Sakellariou and Galanidou, 2015).
On page 3, in Figure 2 caption (below), two words were added after ‘which have their sources in the’ Figure 2. Research area in the northern Aegean between the Island of Thasos and the Gulf of Saros. (a) Overview map with locations mentioned in the text and the four major rivers of the region (Nestos, Kompsatos, Lissos, and Meriç), which have their sources in the Rhodope Mountains and deposit their high sediment load on the shallow shelf of the Samothraki Plateau. (b) Position of Figure 2a on a general map of the Aegean Sea and its bordering countries.
The revised figure caption reads as below Figure 2. Research area in the northern Aegean between the Island of Thasos and the Gulf of Saros. (a) Overview map with locations mentioned in the text and the four major rivers of the region (Nestos, Kompsatos, Lissos, and Meriç), which have their sources in the Rila and Rhodope Mountains and deposit their high sediment load on the shallow shelf of the Samothraki Plateau. (b) Position of Figure 2a on a general map of the Aegean Sea and its bordering countries.
On page 3, first paragraph, in the below sentence, two words were added after ‘Meriç rivers, all sourced in the’ The entire region is fed with fresh water and sediments from the Nestos, Kompsatos, Lissos, and Meriç rivers, all sourced in the Rhodope Mountains, north of the Greek cities Xanthi, Komotini, and Alexandroupoli (Poulos and Kotinas, 2020; Saltogianni et al., 2016; Figures 1 and 2).
The revised paragraph reads as below The entire region is fed with fresh water and sediments from the Nestos, Kompsatos, Lissos, and Meriç rivers, all sourced in the Rila and Rhodope Mountains, north of the Greek cities Xanthi, Komotini, and Alexandroupoli (Poulos and Kotinas, 2020; Saltogianni et al., 2016; Figures 1 and 2).
The online version of the article has now been corrected with immediate effect.