Dataset - B2FIND

Exploring the potential of clumped isotope thermometry on coccolith-rich sedi...

Understanding past changes in sea surface temperatures (SSTs) is crucial; however, existing proxies for reconstructing past SSTs are hindered by unknown ancient seawater...

Deciphering the state of the late Miocene to early Pliocene equatorial Pacific

The late Miocene-early Pliocene was a time of global cooling and the development of modern meridional thermal gradients. Equatorial Pacific sea surface conditions potentially...

Paleoceanographic evolution of the Japan Sea over the last 460 kyr - a coccol...

A series of surface sediment samples recovered from the Japan Sea (JS) and the East China Sea were analysed using electron microscopy to assess the recent distribution of...

Alkenone and coccolith abundance records at IODP Expedition 361 Site U1475

In the southern Indian Ocean, the position of the subtropical front – the boundary between colder, fresher waters to the south and warmer, saltier waters to the north – has a...

Authigenic clay formation and secular variability in the global Li cycle

Lithium isotopic (δ7Li) and elemental concentrations of pore fluids and carbonates from IODP Site U1338 Hole A (eastern equatorial Pacific Ocean) suggest that clay authigenesis...

Sulfur isotope rations in oceanic basement samples

Low temperature alteration of oceanic basement rocks is characterized by net gain of sulfur, which commonly yields low d34S values, suggesting involvement of microbial sulfate...

Heavy mineral and bulk mineral compositions of cores from Kumano Basin

Coring during Integrated Ocean Drilling Program Expeditions 315, 316, and 333 recovered turbiditic sands from the forearc Kumano Basin (Site C0002), a Quaternary slope basin...

Quantifying potassium (K), uranium (U) and thorium (Th) of IODP Holes

A new MATLAB algorithm for the quantification of NGR spectra that is transparent and accessible to future NGR users. Here, we share the results of this MATLAB algorithm for all...

Different Mid-Pleistocene transition analysis from IODP Site 306-U1314

Marine sediments from the Integrated Ocean Drilling Project (IODP) Site U1314 (56.36°N, 27.88°W), in the subpolar North Atlantic, were studied for their planktonic foraminifera,...

Radiolarian abundances from IODP Holes 349-U1431D, 349-U1432C and 349-U1433A

We studied radiolarian abundances in 303 samples from International Ocean Discovery Program Expedition 349 in the South China Sea (SCS), which cored five deep-sea sites. Three...

A multiproxy record of IODP Site 341-U1421

The uncertain response of marine terminating outlet glaciers to climate change at time scales beyond short-term observation limits models of future sea level rise. At temperate...

Microbial abundance and activity at IODP Site C0023, Nankai Trough subduction...

This data set documents data for a publication currently under consideration at Science. It documents data obtained for IODP Site C0023 during IODP Expedition 370. The data...

A multi-proxy record of IODP Site 341-U1417

By means of a multiproxy data set combining biomarker (alkenones, n-alkanes), microfossil (diatoms) and sedimentological (ice rafted debris, XRF) data obtained from sediments...