Stable isotopes (δ¹³C, δ¹⁸O) on elevated epifauna from the Pliocene and Holocene

Name: Stable isotopes (δ¹³C, δ¹⁸O) on elevated epifauna from the Pliocene and Holocene
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The presence and high abundances of the benthic foraminiferal group "elevated epifauna" has been proposed as indicator of the existence of Mediterranean Outflow Water (MOW) in...