Dataset - B2FIND

230Th-normalized opal flux analyses of sediment core MD03-2705

The age model was derived using linear interpolation between radiocarbon dates reported by Jullien et al. (2007).

(Table 1) Age model of sediment core MD03-2705

A reconstruction of northwest African summer monsoon strength during the cold marine isotopic stage (MIS) 6 indicates a link to the seasonal migration of the Intertropical...

(Appendix A) Relative abundance of Emiliania huxleyi in sediment cores of the...

The coccolithophore species Emiliania huxleyi is characterized by a wide range of sizes, which can be easily distinguished in the light microscope. In this study we have...

Geochemical sediment properties of sediment core MD03-2698 from the levee of ...

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Stable isotope record and lithic fragments distribution in sediments of MIS9-...

Stable isotope and ice-rafted debris records from three core sites in the mid-latitude North Atlantic (IODP Site U1313, MD01-2446, MD03-2699) are combined with records of ODP...

Stable isotope record, and abundances of ice rafted debris and Neogloboquadri...

This paper documents the migration of the Polar Front (PF) over the Iberian margin during some of the cold climatic extremes of the last 45 ka. It is based on a compilation of...

Sea surface temperature reconstruction from biomarker in sediments off Portugal

High resolution reconstructions of sea surface temperature (Uk'37-SST), coccolithophore associations and continental input (total organic carbon, higher plant n-alkanes,...

Analytical results from sediment core MD03-2698

It is well established that orbital scale sea-level changes generated larger transport of sediments into the deep-sea during the last glacial maximum than the Holocene. However,...