Relative paleointensity (RPI) proxies for the 100-248 meters composite depth (1.3-3.2 Ma) interval from Integrated Ocean Drilling Program (IODP) Site 303-U1308
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| Natura: | Dataset Open Access |
| Lingua: | en |
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PANGAEA
2021
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| _version_ | 1867172167582482432 |
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| author | Channell, James E T |
| author_facet | Channell, James E T |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | 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Channell et al. 2008 (Earth and Planetary Science Letters, 274, 59-71, 2008, doi:10.1016/j.epsl.2008.07.005) and have been archived at: https://doi.org/10.1594/PANGAEA.808942, https://doi.org/10.1594/PANGAEA.808945, https://doi.org/10.1594/PANGAEA.808946.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 (https://doi.org/10.1594/PANGAEA.871936) and are the basis for the age model. The mean sedimentation rate for the 1.3-3.2 Ma interval is 8.5 cm/kyr. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_931820 |
| institution | PANGAEA |
| language | en |
| publishDate | 2021 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Relative paleointensity (RPI) proxies for the 100-248 meters composite depth (1.3-3.2 Ma) interval from Integrated Ocean Drilling Program (IODP) Site 303-U1308 Channell, James E T 303-U1308; COMPCORE; Composite Core; Depth, composite; Exp303; Intercore correlation; IODP Site U1308; Joides Resolution; Magnetization directions; Natural remanent magnetization/anhysteretic remanent magnetization ratio; Natural remanent magnetization/isothermal remanent magnetization ratio; North Atlantic; North Atlantic Climate 1; North Atlantic Ocean; see Channell et al. (2016) 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 (https://doi.org/10.1594/PANGAEA.871936) and are the basis for the age model. The mean sedimentation rate for the 1.3-3.2 Ma interval is 8.5 cm/kyr. |
| title | Relative paleointensity (RPI) proxies for the 100-248 meters composite depth (1.3-3.2 Ma) interval from Integrated Ocean Drilling Program (IODP) Site 303-U1308 |
| topic | 303-U1308; COMPCORE; Composite Core; Depth, composite; Exp303; Intercore correlation; IODP Site U1308; Joides Resolution; Magnetization directions; Natural remanent magnetization/anhysteretic remanent magnetization ratio; Natural remanent magnetization/isothermal remanent magnetization ratio; North Atlantic; North Atlantic Climate 1; North Atlantic Ocean; see Channell et al. (2016) |
| url | https://doi.org/10.1594/PANGAEA.931820 |