Dataset - B2FIND

(Table 1) Major zones of ice-rafted detritus accumulation in DSDP Holes 71-51...

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(Table 4) Chromalytics MP-3 pyrolysis from selected South Atlantic DSDP Holes

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(Figure 8) Distribution of benthic foraminifers in the Pliocene-Quaternary of...

Psammosphaera fusca, Reophax nodulosus and Cyclammina pusilla were present only in sample 71-511-1-CC.

Age model of DSDP Hole 71-514

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Early Cretaceous sea water and detrial Nd isotope signatures at DSDP Sites 25...

This data set comprises radiogenic neodymium (Nd) isotope signatures of past deep water masses and detrital matter in the Early Cretaceous (Barremian-Albian) South Atlantic...

Carbon isotope records from seven globally distributed marine sediment cores

Stable carbon isotope values of higher-plant leaf wax lipids were extracted, isolated, and measured from seven sediments cores. Sediment cores from DSDP/ODP Sites 94, 354, 511,...

Age model parameters from seven globally distributed marine sediment cores

Stable carbon isotope values of higher-plant leaf wax lipids were extracted, isolated, and measured from seven sediments cores. Sediment cores from DSDP/ODP Sites 94, 354, 511,...

Total calcareous nannofossils abundance and accumulation rates over the past ...

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(Table 1) Textural characteristics of sediments at DSDP Leg 71 Holes

In conjunction with a study of ice-rafted detritus (IRD), textural analyses were carried out on Miocene to Quaternary sediments at Sites 511, 512, 513, and 514. Grain-size...

(Table 1) Carbon and carbonate at DSDP Leg 71 Holes

Leg 71 sediments were analyzed for total carbon and acid-insoluble (organic) carbon, using the Leco WR-12 analyzer, according to the standard technique outlined below. The 3...

(Table 1) Composition of ice-rafted debris and quartz grain concentration at ...

The surficial few meters of sediment at Sites 511 and 512 on Maurice Ewing Bank consist of a lag deposit of icerafted sands and gravels ranging from lower Pliocene to Quaternary...

(Table S1) Diatom species richness from the Early Pleistocene to present

The extent to which the spatial distribution of marine planktonic microbes is controlled by local environmental selection or dispersal is poorly understood. Our ability to...