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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-... -
Statistical analysis of sedimentary and diagenetic factors for NRM Interpreta...
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... -
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... -
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... -
Calcareous nannofossil abundance of IODP Site 378-U1553
999 means cf: taxonomic note: 'cf.' (= 'confer', in Latin: compare) -
Hyperthermals and the bulk sediment δ13C tie points from IODP Site U1553 corr...
Age model. Hyperthermals (Hyp) and the bulk sediment δ13C records from ODP Site1258 and 1262 were correlated to our record. This table provides the tie points in order to... -
d13C and d18O stable isotope records of IODP Site 378-U1553
This dataset has no description
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Magnetostratigraphic and rock magnetic results from postcruise investigation ...
We present the rock magnetic and paleomagnetic data set from Site U1553 (including Holes A, B & E) recovered during IODP Expedition 378 in the southern Campbell Plateau... -
Late Paleocene - early Eocene calcareous nannofossil relative abundance count...
In this dataset, we show the raw relative abundance count data for calcareous nannofossils observed in sediment samples from International Ocean Discovery Program (IODP)... -
Calcareous nannofossil biostratigraphy of IODP Site 378-U1553
*shipboard data, Röhl, U., Thomas, D.J., Childress, L.B., Anagnostou, E., Ausín, B., Borba Dias, B., Boscolo-Galazzo, F., Brzelinski, S., Dunlea, A.G., George, S.C., Haynes,... -
Late Paleocene to early Eocene stable isotope records and calcareous nannofos...
In this study, we create a new age model for the high-latitude South Pacific during the late Paleocene to early Eocene (50.5 to 57.5 Ma). We present a bulk sediment δ13C and...
