Evidence of anoxic layers in the Central Tyrrhenian Sea between 29 and 4.2 ka. Alpine and Mediterranean Quaternary, [S. l.], v. 37, n. 1, p. 67–82, 2024. DOI: 10.26382/AMQ.2024.04. Disponível em: https://amq.aiqua.it/index.php/amq/article/view/716. Acesso em: 4 dec. 2024.