Mid-Holocene changes in the geochemical and biotic conditions of an aquatic ecosystem, in Eastern Mediterranean

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Fig. 8

Downcore variations of the PC1 and PC2 scores, with organic paleoenvironmental proxies (C/N and δ¹⁵N) measured in Omalos MTP. Dashed lines correspond to the core base (176–170 cm) and middle (96–80 cm) dated sediment layers at 16.7 and 4.7 cal. ka BP, respectively.

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