10.1594/PANGAEA.967343Novak, Joseph BJoseph BNovak0000-0002-8569-2645University of California, Santa CruzCaballero-Gill, Rocio PRocio PCaballero-GillGEORGE MASON UNIVRose, RebeccaRebeccaRoseUNIV WISCONSIN MADISONHerbert, Timothy DTimothy DHerbert0000-0003-1556-4290Brown UniversityDowsett, Harry JHarry JDowsett0000-0003-1983-7524U.S. Geological SurveyPANGAEA2024Age modelAlkenonesBenthic foraminifera assemblagesBenthic foraminiferal stable isotopesCalcium Carbonate contentComposite splicediatomsODP 883ODP 887Stable carbon isotopes δ13Cstable oxygen isotopesSubarctic North PacificUk'37 sst and C37totalEvent labelDatum/eventTie pointMethod commentAge modelSample code/labelDEPTH, sediment/rockSedimentation rateDrilling/drill rigDSDP/ODP/IODP sample designationCalculatedLeg145Joides ResolutionOcean Drilling Program (ODP)1992-08-09T09:40:00/1992-08-13T15:15:00Dataset10.1594/PANGAEA.967342191 data pointstext/tab-separated-valuesCreative Commons Attribution 4.0 InternationalHere we present a new astronomically tuned age model for the late Pliocene section of ODP site 883. The astronomically tuned age model was developed by correlation of benthic foraminiferal δ18O (3000-3385 Ka) to the δ18O probabilistic stack and the 883 GRAPE WBD composite (2.841-3.0 Ma & 3.385-3.465 Ma) to the nearby ODP 882 carbonate weight %, where the age model is based on tuning GRAPE WBD to calculated solar insolation.167.7687167.768851.198551.1987North Pacific OceanNational Science Foundationhttps://doi.org/10.13039/1000000011459280A New View of Pliocene GlaciationsNational Science Foundationhttps://doi.org/10.13039/1000000011545859PIRE: DUST stimulated drawn-down of atmospheric CO2 as a trigger for Northern Hemisphere GlaciationNational Science Foundationhttps://doi.org/10.13039/1000000011602331Collaborative Research: Did the SE Pacific Gyre become a Hot Spot for N2 Fixation during Dusty Glacial Conditions?