Dataset - B2FIND

Accumation rates of manganese in a pelagic sediment core using 231Pa activity

For a pelagic sediment core taken in the Atlantic Ocean, The decrease of unsupported 231Pa was used for the determination of the accretion rate. Because CaCO3 is a Mn-free...

Accumation rates of manganese in pelagic sediments using Ericson paleontologi...

For 4 pelagic sediment cores taken in the Atlantic Ocean, Ericson's paleontologic boundaries X-Y (75 000 yr) and Y-Z (11 000 yr) were used. The age of the upper boundary was...

Accumation rates of manganese in pelagic sediments using 130Th activity

For 7 pelagic sediment cores, the decrease in unsupported 130Th activity with depth in the core was used to establish the mean accumulation rate over the last 300 000 years....

Accumation rates of manganese in pelagic sediments using Brunnes-Matuyama mag...

For 27 pelagic sediment cores, the Brunnes-Matuyama magnetic reversal boundary (700 000 yr) was used to establish the mean sedimentation rate between this level and the core...

(Table 1) Sedimentation and mass accumulation rates at DSDP Site 85-572

This dataset has no description

A new helium isotope recored of the Paleocene-Eocene Thermal Maximum from ODP...

The Paleocene-Eocene Thermal Maximum (PETM; around 56 Ma ago) is arguably the most intensively studied event of rapid greenhouse warming of the geological past. The duration and...

A new helium isotope recored of the Paleocene-Eocene Thermal Maximum from ODP...

The Paleocene-Eocene Thermal Maximum (PETM; around 56 Ma ago) is arguably the most intensively studied event of rapid greenhouse warming of the geological past. The duration and...

A new helium isotope recored of the Paleocene-Eocene Thermal Maximum from ODP...

The Paleocene-Eocene Thermal Maximum (PETM; around 56 Ma ago) is arguably the most intensively studied event of rapid greenhouse warming of the geological past. The duration and...