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Paleomagnetic directions and intensities of 572 sediment samples from IODP Si...
AF demagnetization data of NRM were analyzed using anchored Principal Component Analysis (PCA) to obtain the Characteristic Remanent Magnetization (ChRM). Each sample was... -
Relative abundance of pollen-derived vegetation record from MIS 1 at IODP Hol...
Pollen-based vegetation reconstruction from IODP Hole 339-U1385A, drilled on the SW Iberian margin during IODP Expedition 339 (37°34.285′ N, 10°7.562′ W; 2578 m water depth).... -
Pollen-derived vegetation record from MIS 1 at IODP Hole 339-U1385A, SW Iberi...
Pollen-based vegetation reconstruction from IODP Hole 339-U1385A, drilled on the SW Iberian margin during IODP Expedition 339 (37°34.285′ N, 10°7.562′ W; 2578 m water depth).... -
Miocene stable isotope record of benthic foraminifera from IODP Site 320-U1336
Stable carbon and oxygen isotopes (d13C and d18O) of foraminiferal tests are amongst the most important tools in paleoceanography but the extent to which recrystallization can... -
First order reversal curve (FORC) analysis of IODP sample U1553E-26X-3-W 43/4...
This Firt Order Reversal Curve was measured using the LakeShore Model 8600 vibrating sample magnetometer at the paleomagnetic laboratory of the Institute of Geomechanics,... -
First order reversal curve (FORC) analysis of IODP sample U1553B-22X-2-W 77/...
This Firt Order Reversal Curve was measured using the LakeShore Model 8600 vibrating sample magnetometer at the paleomagnetic laboratory of the Institute of Geomechanics,... -
First order reversal curve (FORC) analysis of IODP sample U1553B-5H-2-W 61/6...
This Firt Order Reversal Curve was measured using the LakeShore Model 8600 vibrating sample magnetometer at the paleomagnetic laboratory of the Institute of Geomechanics,... -
First order reversal curve (FORC) analysis of IODP sample U1553E-1H-4-W 114/...
These First Order Reversal Curves were measured with a Princeton Measurement Corporation (PMC) Micromag M2900 alternating gradient force magnetometer at the Paleo- and Rock-... -
Magnetozone boundaries and assigned geomagnetic chrons of IODP Site 378-U1553...
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 thermomagnetic measurements of 11 sediment samples from IODP ...
Low-temperature magnetic cycling provides complementary information on mineral magnetic properties. We used the Quantum Design MPMS-XL7 Magnetic Property Measurement System at... -
Endmember analysis of IRM acquisition curves of 65 sediment samples of IODP S...
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... -
Isothermal remanent magnetization (IRM) acquisition curves of 65 sediment sam...
Measurements of acquisition of isothermal remanent magnetization (IRM) were conducted on a uniformly distributed subset of 65 discrete samples. We applied 22-step IRM... -
Stepwise NRM demagnetization data of 572 sediment samples from IODP Site 378-...
Detailed alternating field (AF) demagnetization of Natural Remanent Magnetization (NRM) were conducted on discrete samples of IODP Site U1553. Thermal demagnetization were only... -
Benthic foraminiferal (Cibicidoides grimsdalei) stable isotope stratigraphy f...
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Stable isotope (δ13C and δ18O) of bulk sediment from ODP Hole 199-1217A
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Stable isotope (δ13C and δ18O) of bulk sediment from ODP Site 199-1219
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Stable isotope (δ13C and δ18O) of bulk sediment from ODP Hole 199-1220B
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Stable isotope (δ13C and δ18O) of bulk sediment from IODP Hole 320-U1331B
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Stable isotope (δ13C and δ18O) of bulk sediment from IODP Site 320-U1332
This dataset has no description
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Stable isotope (δ13C and δ18O) of bulk sediment from IODP Site 320-U1333
This dataset has no description
