10.1594/PANGAEA.937303Stow, Dorrik A VDorrik A VStowSmillie, ZeinabZeinabSmillie0000-0002-0089-1793Wilkin, JonathanJonathanWilkinPan, JiaweiJiaweiPanEsegbue, OnoriodeOnoriodeEsegbueBahr, AndréAndréBahrDucassou, EmmanuelleEmmanuelleDucassouPANGAEA2024contouriteContouritesgrain size analysisIODP 339isotope analysisU1389ASample code/labelDEPTH, sediment/rockSize fraction < 0.004 mm, claySize fraction 0.004-0.002 mm, 8.0-9.0 phi, very fine siltSize fraction 0.008-0.004 mm, 7.0-8.0 phi, fine siltSize fraction 0.016-0.008 mm, 6.0-7.0 phi, medium siltSize fraction 0.064-0.032 mmSize fraction 0.125-0.064 mmSize fraction 0.250-0.125 mm, 2.0-3.0 phi, fine sandSize fraction 0.500-0.250 mm, 1.0-2.0 phi, medium sandSize fraction 1.000-0.500 mmSize fraction 2.000-1.000 mmDrilling/drill rigDSDP/ODP/IODP sample designationCalculated, see abstractExp339Joides ResolutionDataset10.1594/PANGAEA.93730710.1016/j.margeo.2023.10702610.2204/iodp.pr.339.2012528 data pointstext/tab-separated-valuesCreative Commons Attribution 4.0 InternationalGrain-size statistical parameters were calculated using Gradistat software (Blott and Pye, 2001) and based on the geometric graphical method (Folk and Ward, 1957). The same samples were then treated to remove the biogenic carbonate and siliceous components, and re-analysed with the laser micro-granulometer, with a view to determining the sortable silt component.-7.278178333333336.425305