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Publikováno v:
Rivista Italiana di Paleontologia e Stratigrafia, Vol 89, Iss 3 (2020)
Oxygen and carbon isotope data of several benthic and planktonic species of Foraminifera from a regressive sequence in northeastern Italy indicate a watermass change during the Late Eocene, In the middle of zone P 16 the Belluno Basin Was temporari/y
Externí odkaz:
https://doaj.org/article/be8cc0455ffd45199a52d66c4b157b26