Sea surface temperature anomalies for Pliocene interglacial KM5c (PlioVAR)

• Main Authors: McClymont, Erin L, Ford, Heather L, Ho, Sze Ling, Alonso-Garcia, Montserrat, Bailey, Ian, Berke, Melissa A, Littler, Kate, Patterson, Molly O, Petrick, Benjamin F, Peterse, Francien, Ravelo, Ana Christina, Risebrobakken, Bjørg, De Schepper, Stijn, Swann, George E A, Thirumalai, Kaustubh, Tierney, Jessica E, van der Weijst, Carolien, White, Sarah M
• Format: Dataset
• Language: English
• Published: PANGAEA 2020
• Subjects: 100-625; 104-642; 108-662; 115-709; 117-722; 122-763; 130-806; 138-846; 159-959; 162-907; 162-982; 165-999; 175-1081; 175-1082; 175-1084; 175-1087; 177-1090; 181-1125; 184-1143; 202-1241; 22-214; 306-U1313; 321-U1337; 339-U1387; 341-U1417; 72-516; 90-593; 90-594; 93-603; 94-607; 94-609; Arabian Sea; Benguela Current; South Atlantic Ocean; Calculated from Mg/Ca ratios (this study); Calculated from Mg/Ca ratios using the BAYMAG calibration; Calculated from UK37 (Müller et al; 1998); Calculated from UK37 using the BAYSPLINE calibration; Caribbean Sea; COMPCORE; Composite Core; DRILL; Drilling/drill rig; ELEVATION; Event label; Exp306; Exp321; Exp339; Exp341
• Online Access: https://doi.pangaea.de/10.1594/PANGAEA.911847; https://doi.org/10.1594/PANGAEA.911847

We examine a single interglacial during the late Pliocene (KM5c, ca. 3.205 +/- 0.01 Ma) when atmospheric CO2 concentrations were higher than pre-industrial, but similar to today and to the lowest emission scenarios for this century. As orbital forcing and continental configurations were also similar...