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Tie points for IODP Hole 344-U1381C
The age model for the upper 49 m of Hole U1381C is based on radiocarbon dates, graphical tuning of the benthic δ18O record and biostratigraphic and paleomagnetic events. The age... -
Major and minor elements from IODP Hole 344-U1381C
The sedimentary concentrations of major (Ca, Fe, Ti, Al, K) and minor (Mn, Ba, Sr) elements were measured by X-ray Fluorescence using Mo as the X-ray source on a spectrometer... -
Planktonic foraminifera from IODP Hole 344-U1381C
Sediment samples destined for the analysis of planktic assemblages were wet-sieved over a 63 μm fraction and then oven-dried. Planktonic foraminifera were identified and counted... -
Stable isotopes in benthic foraminifera from IODP Hole 344-U1381C
Stable isotopic analyses were carried out on the benthic foraminifera species Uvigerina auberiana from the 250-300 µm size fraction. They were performed on a ThermoFinnigan MAT... -
Content of organic and inorganic carbon, nitrogen and opal for IODP Hole 344-...
The total weight percent of sedimentary carbon (% C) and nitrogen (% N), as well as inorganic carbon (% Cinorg) and organic carbon (% Corg) were measured using a macro elemental... -
Benthic foraminifera counts of IODP Hole 344-U1381C
Benthic foraminifera (>125 µm fraction) were analysed in sediment samples from Hole U1381C (08°25.7027′N; 84°09.48′W, 2064.6 m water depth) located off Costa Rica (East... -
Quantifying potassium (K), uranium (U) and thorium (Th) of IODP Site 344-U1414A
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