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One visible volcanic ash layer and 21 non‐visible, cryptotephra horizons have been identified in the M72/5‐25‐GC1 core from the south‐east Black Sea that spans the last ∼60 ka. Glass chemistry suggests that the tephras derive from Italian, Hellenic and Turkish sources. The visible tephra layer is trachytic in composition and has been correlated to the ∼39 ka Campanian Ignimbrite super‐eruption from...
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