PANGAEA_937303 Bulk analysis from IODP Core 339-U1389A-25X Stow, Dorrik A V; Smillie, Zeinab; Wilkin, Jonathan; Pan, Jiawei; Esegbue, Onoriode; Bahr, André; Ducassou, Emmanuelle Bulk analysis from IODP Core 339-U1389A-25X 2024-12-14 PANGAEA Dataset https://doi.pangaea.de/10.1594/PANGAEA.937303 Investigator Zeinab Smillie z.smillie@hw.ac.uk Earth Science Sample code/label DEPTH, sediment/rock Size fraction < 0.004 mm, clay Size fraction 0.004-0.002 mm, 8.0-9.0 phi, very fine silt Size fraction 0.008-0.004 mm, 7.0-8.0 phi, fine silt Size fraction 0.016-0.008 mm, 6.0-7.0 phi, medium silt Size fraction 0.064-0.032 mm Size fraction 0.125-0.064 mm Size fraction 0.250-0.125 mm, 2.0-3.0 phi, fine sand Size fraction 0.500-0.250 mm, 1.0-2.0 phi, medium sand Size fraction 1.000-0.500 mm Size fraction 2.000-1.000 mm geoscientificInformation 339-U1389A contourite Contourites Drilling/drill rig Exp339 grain size analysis IODP 339 isotope analysis U1389A DSDP/ODP/IODP sample designation Calculated, see abstract Joides Resolution Complete 36.425305 36.425305 -7.2781783333333 -7.2781783333333 220.05 m (DEPTH, sediment/rock) 224.52 m (DEPTH, sediment/rock) unrestricted CC-BY-4.0: Creative Commons Attribution 4.0 International English PANGAEA Data Publisher for Earth & Environmental Science https://www.pangaea.de/ Data Center Contact Michael Diepenbroek info@pangaea.de

Leobener Str.

Bremen Bremen 28359 Germany online 528 data points text/tab-separated-values Stow, Dorrik A V; Smillie, Zeinab; Wilkin, Jonathan; Pan, Jiawei; Esegbue, Onoriode; Bahr, André; Ducassou, Emmanuelle (2023): Anatomy of the bi-gradational contourite sequence: Case study from the Gulf of Cadiz. Marine Geology, 458, 107026, https://doi.org/10.1016/j.margeo.2023.107026 IODP Expedition 339 Scientists (2012): Environmental significance of the Mediterranean Outflow Water and its global implications. IODP Preliminary Report, Integrated Ocean Drilling Program, https://doi.org/10.2204/iodp.pr.339.2012

Grain-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. ** For all details see the full metadata description at "https://doi.pangaea.de/10.1594/PANGAEA.937303"!

https://doi.org/10.1016/j.margeo.2023.107026 Anatomy of the bi-gradational contourite sequence: Case study from the Gulf of Cadiz https://doi.org/10.2204/iodp.pr.339.2012 Environmental significance of the Mediterranean Outflow Water and its global implications https://hdl.handle.net/10013/epic.27914.d001 DSDP/ODP/IODP sample designation https://www-odp.tamu.edu:443/resolutn.html Joides Resolution PANGAEA_937307 DIF 9.4 2024-12-14 2026-04-30