-
Coherency (ETP) of δ18O from ODP Site 138-846
Coherency was calculated to a normalized average record of eccentricity, obliquity, and precession for a Pliocene window from 3.0-3.6 Ma. -
Coherency (ETP) of sea surface temperature from ODP Site 138-846
Coherency was calculated to a normalized average record of eccentricity, obliquity, and precession for a Pliocene window from 3.0-3.6 Ma. -
Coherency (ETP) of δ18O from ODP Site 138-849
Coherency was calculated to a normalized average record of eccentricity, obliquity, and precession for a Pliocene window from 3.0-3.6 Ma. -
Coherency (ETP) of sea surface temperature from ODP Site 138-850
Coherency was calculated to a normalized average record of eccentricity, obliquity, and precession for a Pliocene window from 3.0-3.6 Ma. -
Coherency (ETP) of C37 alkenones mass accumulations rate from IODP Site 321-U...
Coherency was calculated to a normalized average record of eccentricity, obliquity, and precession for a Pliocene window from 3.0-3.6 Ma. -
Coherency (ETP) of δ13C from ODP Site 138-849
Coherency was calculated to a normalized average record of eccentricity, obliquity, and precession for a Pliocene window from 3.0-3.6 Ma. -
Coherency (ETP) of sea surface temperature from IODP Site 321-U1338
Coherency was calculated to a normalized average record of eccentricity, obliquity, and precession for a Pliocene window from 3.0-3.6 Ma. -
Coherency (ETP) of C37 alkenones mass accumulations rate from ODP Site 138-850
Coherency was calculated to a normalized average record of eccentricity, obliquity, and precession for a Pliocene window from 3.0-3.6 Ma. -
Coherency (ETP) of C37 alkenones mass accumulations rate from ODP Site 138-849
Coherency was calculated to a normalized average record of eccentricity, obliquity, and precession for a Pliocene window from 3.0-3.6 Ma. -
Coherency (ETP) of sea surface temperature from ODP Site 138-849
Coherency was calculated to a normalized average record of eccentricity, obliquity, and precession for a Pliocene window from 3.0-3.6 Ma. -
Soil greenhouse gas fluxes from 2011 to 2015 measured at the Mt. Kilimanjaro
Ten sites covering six different ecosystems were selected for detailed situ N2O and CH4 exchange measurements. The six different ecosystems represent main (semi) natural forest... -
Concentrations of individual polychlorinated biphenyl congeners in particle p...
We report the levels of airborne individual PCB concentrations of particle (QFF) phases from the City of Chicago in 2009. Seventeen locations were sampled for particle phases,... -
Silicon isotopes in surface waters during POLARSTERN cruise PS94 (ARK-XXIX/3)...
In this study we present dissolved and particulate silicon isotope results in surface waters obtained as part of the GEOTRACES central Arctic Ocean section GN04 (2015) onboard... -
Dole effect in the north of the South China Sea from sediment core PC27 and PC83
Relative intensity proxy (RPI) be constructed using the equation: RPI=NRM/SIRM (20-60)mT * MDFSIRM-CM/MDFSIRM, where MDFSIRM-CM is the center of mass of MDFSIRM.Dole effect was... -
Stacked dole effect in the north of the South China Sea from sediment core PC...
Relative intensity proxy (RPI) be constructed using the equation: RPI=NRM/SIRM (20-60)mT * MDFSIRM-CM/MDFSIRM, where MDFSIRM-CM is the center of mass of MDFSIRM -
Concentrations of individual polychlorinated biphenyl congeners in gas phases...
We report the levels of airborne individual PCB concentrations of gas (XAD-2) phases from the City of Chicago in 2009. Twenty-seven locations were sampled for gas phases, where...
