Dataset - B2FIND

Hydrocarbon data of the cold-water sponge Halichondria panicea exposure exper...

In this study, inter-tidal cold-water sponge Halichondria panicea samples were exposed to Benzo-A-pyrene for 48h (accumulation phase) and then left to recover for 13 days in...

Temperature and photoperiod effects on sex determination in Leuresthes tenuis...

In some gonochoristic species, sex is influenced not only by genotype at conception but also by the environment that offspring experience during early ontogeny (termed...

(Table 1) Bulk Fe isotope values and pyrite framboids sizes of Cenomanian-Tur...

Organic carbon-rich shales from localities in England, Italy, and Morocco, which formed during the Cenomanian-Turonian oceanic anoxic event (OAE), have been examined for their...

(Table 4) Mean diameter of Orbulina universa d'Orbigny at DSDP Leg 54 Holes

On Deep Sea Drilling Project Leg 54, we recovered upper Pliocene (Globigerinoides obliquus: PL6 zone) to Pleistocene sediments from the equatorial East Pacific Rise (EPR) and...

(Table 1) Oxygen and carbon isotopes and calcium carbonte of bulk carbonate a...

A detailed oxygen and carbon isotope study of the upper Maestrichtian-lower Paleocene section of Hole 516F from the Rio Grande Rise reveals that large isotopic anomalies are...

(Table 1) Isotopic composition of organic compinents of DSDP Hole 24-231

Plant leaf wax hydrogen isotope (dDwax) reconstructions are increasingly being used to reconstruct hydrological change. This approach is based upon the assumption that...

(Table 1) Comparisons of dynamic and static Young's moduli of basalt at DSDP ...

Compressional- and shear-wave velocity logs (Vp and Vs, respectively) that were run to a sub-basement depth of 1013 m (1287.5 m sub-bottom) in Hole 504B suggest the presence of...

Glassy and basaltic fragments within graded volcaniclastic sediments at DSDP ...

Graded volcaniclastic sediments deposited by turbidity currents in the basal section at Site 585 are mixed vitric-lithic tuffs and lapilli-stones with minor Plagioclase and...

(Table T1) Carbon geochemistry and coarse fraction content of ODP Sites 184-1...

The goal during Ocean Drilling Program Leg 184 was to reconstruct the long-term paleoenvironmental variability of the South China Sea (SCS) and the adjacent Asian continent. In...

(Table 1) Strontium isotope ratios of ODP Hole 121-758A

The 87Sr/86Sr ratio of sea water has increased gradually over the past 40 Myr, suggesting a concomitant increase in global chemical weathering rates (Raymo et al., 1988,...

Tab. 2: Grain-sizes of cobble on the surface of sanderwurzel

yResults of 13 field investigations between 1966 and 1990 of the southwestern to eastern margin of Kötlujökull and its proglacial area are summarized with respect to sandar and...

(Table 1) Luminescence datings from Varchushka and Pyoza rivers, Russia

The Pyoza River area in the Arkhangelsk district exposes sedimentary sequences suitable for study of the interaction between consecutive Valdaian ice sheets in Northern Russia....

(Table 1) Luminescence age determination of sediments from the Arkhangelsk area

The Arkhangelsk area lies in the region that was reached by the northeastern flank of the Scandinavian ice sheet during the last glaciation. Investigations of Late Pleistocene...