DataSheet3_Eocene-Oligocene southwest Pacific Ocean paleoceanography new insights from foraminifera chemistry (DSDP site 277, Campbell Plateau).DOCX

• Main Authors: F. Hodel, C. Fériot, G. Dera, M. De Rafélis, C. Lezin, E. Nardin, D. Rouby, M. Aretz, P. Antonio, M. Buatier, M. Steinmann, F. Lacan, C. Jeandel, V. Chavagnac
• Format: Dataset
• Language: unknown
• Published: 2022
• Subjects: Solid Earth Sciences; Climate Science; Atmospheric Sciences not elsewhere classified; Exploration Geochemistry; Inorganic Geochemistry; Isotope Geochemistry; Organic Geochemistry; Geochemistry not elsewhere classified; Igneous and Metamorphic Petrology; Ore Deposit Petrology; Palaeontology (incl. Palynology); Structural Geology; Tectonics; Volcanology; Geology not elsewhere classified; Seismology and Seismic Exploration; Glaciology; Hydrogeology; Natural Hazards; Quaternary Environments; Earth Sciences not elsewhere classified; Evolutionary Impacts of Climate Change; paleoceanography; climate; foraminifera; Eocene; Oligocene; southwest Pacific Ocean; Campbell Plateau; Drake Passage; Pacific; Southern Ocean; Antarc*; Antarctica
• Online Access: https://doi.org/10.3389/feart.2022.998237.s003; https://figshare.com/articles/dataset/DataSheet3_Eocene-Oligocene_southwest_Pacific_Ocean_paleoceanography_new_insights_from_foraminifera_chemistry_DSDP_site_277_Campbell_Plateau_DOCX/21569607

Despite its major role in the Earth’s climate regulation, the evolution of high-latitude ocean dynamics through geological time remains unclear. Around Antarctica, changes in the Southern Ocean (SO) circulation are inferred to be responsible for cooling from the late Eocene and glaciation in the ear...