Dataset - B2FIND

Biogeochemical proxies analysed on sediment core TAN1106-28

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Concentrations of export production indicators and corrected and non-correcte...

Studying oceanic particle fluxes from sediment records is an important component of paleoceanography. Traditionally, we calculate these fluxes using a combination of linear...

(Appendix A3) Geochemistry of ODP Hole 207-1260A

Sediment depth is given in mbsf. The enrichment factors (EF) are calculated as following: EFx = (X/Al)sample : (X/Al)average shale, where X and Al stand for the weight...

Th fluxes on core PS97/093-2

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Flux of excess barium from ODP Site 202-1240

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Barium concentration in sediments across the PETM, ODP Hole 159-959D

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(Fig. 4) Proxy records for paleoproductivity from subantarctic sediment core ...

Alignment of Fe content records to EDC dust contents on AICC12 time-scale; see Lamy et al., 2014 SOM.

Chemical anorganic composition and TOC and N concentrations of core GeoB12309...

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Geochemical composition of sediment core SO201-2-85

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Geochemical composition of sediment core SO201-2-77

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Geochemical composition of sediment core SO201-2-101

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(Table T3) Ba barite and Ba excess comparison of ODP Site 202-1237 sediments

Depth (sediment) given in mbsf. Ba xs = Ba (total) - [Ti x (Ba/Ti) source material].

(Table T2) Phosphorous components and trace metals from ODP Site 202-1237 sed...

Depth (sediment) given in mbsf. Ba excess defined as total Ba normalized for terrigenous input using molar Ba/Ti upper crust = 0.057 (Rudnick and Gao, 2004). Trace metal EFs for...