2023
DOI: 10.21203/rs.3.rs-2619917/v1
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Deep-sea benthic foraminiferal response to the early Oligocene cooling: A study from the Southern Ocean ODP Hole 1138A

Abstract: Ongoing rapid climate change has a major effect on marine fauna, and understanding these faunal changes analogous to future climatic periods is crucial. The Oligocene is commonly considered a critical transition period, linking the archaic world of the tropical Eocene and the more modern ecosystems of the Miocene. Here, we show the response of marine benthic foraminifera to the early Oligocene climatic changes at Ocean Discovery Program (ODP) Hole 1138A of the Southern Ocean (Indian Sector). We made use of the… Show more

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