321 datasets found

This Firt Order Reversal Curve was measured using the LakeShore Model 8600 vibrating sample magnetometer at the paleomagnetic laboratory of the Institute of Geomechanics,...

This Firt Order Reversal Curve was measured using the LakeShore Model 8600 vibrating sample magnetometer at the paleomagnetic laboratory of the Institute of Geomechanics,...

These First Order Reversal Curves were measured with a Princeton Measurement Corporation (PMC) Micromag M2900 alternating gradient force magnetometer at the Paleo- and Rock-...

Five bivariate abundance analyses investigate, to which extent paleomagnetic interpretability (quantified by the quality indices N/R, NP/RP, NPP/RPP, N?/R? and INT), depend on...

Using the quality rating of polarity, we identified fifteen magnetozones, labeled as R0, N1, R1, …, N7, R7. The well-defined biostratigraphic frame enabled us to correlate the...

Low-temperature magnetic cycling provides complementary information on mineral magnetic properties. We used the Quantum Design MPMS-XL7 Magnetic Property Measurement System at...

End-member unmixing using the algorithm of Heslop and Dillon (2007) (doi:10.1111/j.1365-246X.2007.03432.x) was performed on 65 normalized IRM acquisition curves to quantify...

Measurements of acquisition of isothermal remanent magnetization (IRM) were conducted on a uniformly distributed subset of 65 discrete samples. We applied 22-step IRM...

Detailed alternating field (AF) demagnetization of Natural Remanent Magnetization (NRM) were conducted on discrete samples of IODP Site U1553. Thermal demagnetization were only...

AF demagnetization data of NRM were analyzed using anchored Principal Component Analysis (PCA) to obtain the Characteristic Remanent Magnetization (ChRM). Each sample was...

Sediment cores from the South Pacific (Chile Fracture Zone) obtained during RV SONNE cruise SO213 (SOPATRA) in December 2011 allow us to reconstruct lateral changes in the...

Sediment cores from the South Pacific (Chile Fracture Zone) obtained during RV SONNE cruise SO213 (SOPATRA) in December 2011 allow us to reconstruct lateral changes in the...

Sediment cores from the South Pacific (Chile Fracture Zone) obtained during RV SONNE cruise SO213 (SOPATRA) in December 2011 allow us to reconstruct lateral changes in the...

Sediment cores from the South Pacific (Chile Fracture Zone) obtained during RV SONNE cruise SO213 (SOPATRA) in December 2011 allow us to reconstruct lateral changes in the...

Water temperature is a major abiotic driver, controlling the rates and nature of biochemical reactions and subsequently affecting the physiology of marine organisms. However,...

Sediment depth displays CCSF-B, 143Nd/144Nd values normalized to Jndi, Pb ratios realtive to values of NIST SRM981, all reported errors display propagated 2Sd using internal...

Sediment depth displays CCSF-B, 143Nd/144Nd values normalized to Jndi, Pb ratios realtive to values of NIST SRM981, all reported errors display propagated 2Sd using internal...

Sediment depth displays CCSF-B, 143Nd/144Nd values normalized to Jndi, Pb ratios realtive to values of NIST SRM981, all reported errors display propagated 2Sd using internal...

This dataset comprises planktonic foraminifera assemblages and sea surface temperature (SST) reconstructions generated using the Modern Analogue Technique (MAT). The record...

This dataset contains planktonic foraminifera assemblage groups defined by cluster analysis, alongside sea surface temperature (SST) reconstructions generated with the Modern...