Here we present relative paleointensity (RPI) proxies for the 100-248 meters composite depth (1.3-3.2 Ma) interval from Integrated Ocean Drilling Program (IODP) Site U1308 (49° 53'N, 24° 14'W; water depth 3871 m). Methods are described in Channell et al. (2016) (Quaternary Science Reviews, 131, 1-19, 2016, doi:10.1016/j.quascirev.2015.10.011). The magnetic records for 0-1.3 Ma at Site U1308 were published in Channell et al. 2008 (Earth and Planetary Science Letters, 274, 59-71, 2008, doi:10.1016/j.epsl.2008.07.005) and have been archived at: https://doi.org/10.1594/PANGAEA.808942, https://doi.org/10.1594/PANGAEA.808945, https://doi.org/10.1594/PANGAEA.808946. Benthic oxygen isotope stratigraphy for the 0- 3.2 Ma interval are archived at (ht...
To reconstruct the climate history of the equatorial Pacific, one major objective of the Pacific Equ...
During Ocean Drilling Program Leg 199 a high-resolution (~1-2 cm/k.y.) biogenic sediment record from...
Paleoceanography research is always limited by the accuracy of age-depth relationships. For sediment...
© 2015 Elsevier Ltd. Integrated Ocean Drilling Program (IODP) Site U1308 (49°53'N, 24°14'W; water de...
Here we present volume susceptibility and anhysteretic susceptibility divided by susceptibility for ...
Integrated Ocean Drilling Program (IODP) Site 303-U1308 (49° 53'N, 24° 14'W; water depth 3871 m) pro...
Integrated Ocean Drilling Program (IODP) Site U1308 (central North Atlantic) records paleomagnetic d...
Integrated Ocean Drilling Program (IODP) Site U1308 (central North Atlantic) records paleomagnetic d...
High-quality relative paleointensity (RPI) is important for the study of Earth Interior and sediment...
Integrated Ocean Drilling Program (IODP) Site U1332 (11°54.722?N, 141°02.743?W; 4924 meters below se...
Relative paleointensity (RPI) records can reflect the evolution of the Earth’s axial dipole field an...
This dataset lists the oxygen isotope ratios used to update the age model of Integrated Ocean Drilli...
During Ocean Drilling Program Leg 199 a high-resolution (~1–2 cm/ k.y.) biogenic sediment record fro...
The data comprise meters composite depth (mcd) versus component declination, inclination and maximum...
Ocean Drilling Program Sites 883 and 884 were cored as part of a three-site depth transect down the ...
To reconstruct the climate history of the equatorial Pacific, one major objective of the Pacific Equ...
During Ocean Drilling Program Leg 199 a high-resolution (~1-2 cm/k.y.) biogenic sediment record from...
Paleoceanography research is always limited by the accuracy of age-depth relationships. For sediment...
© 2015 Elsevier Ltd. Integrated Ocean Drilling Program (IODP) Site U1308 (49°53'N, 24°14'W; water de...
Here we present volume susceptibility and anhysteretic susceptibility divided by susceptibility for ...
Integrated Ocean Drilling Program (IODP) Site 303-U1308 (49° 53'N, 24° 14'W; water depth 3871 m) pro...
Integrated Ocean Drilling Program (IODP) Site U1308 (central North Atlantic) records paleomagnetic d...
Integrated Ocean Drilling Program (IODP) Site U1308 (central North Atlantic) records paleomagnetic d...
High-quality relative paleointensity (RPI) is important for the study of Earth Interior and sediment...
Integrated Ocean Drilling Program (IODP) Site U1332 (11°54.722?N, 141°02.743?W; 4924 meters below se...
Relative paleointensity (RPI) records can reflect the evolution of the Earth’s axial dipole field an...
This dataset lists the oxygen isotope ratios used to update the age model of Integrated Ocean Drilli...
During Ocean Drilling Program Leg 199 a high-resolution (~1–2 cm/ k.y.) biogenic sediment record fro...
The data comprise meters composite depth (mcd) versus component declination, inclination and maximum...
Ocean Drilling Program Sites 883 and 884 were cored as part of a three-site depth transect down the ...
To reconstruct the climate history of the equatorial Pacific, one major objective of the Pacific Equ...
During Ocean Drilling Program Leg 199 a high-resolution (~1-2 cm/k.y.) biogenic sediment record from...
Paleoceanography research is always limited by the accuracy of age-depth relationships. For sediment...