Fujita, Kazuhiko; Omori, Akitoshi; Yokoyama, Yusuke; Sakai, Saburo; Iryu, Yasufumi (2010): (Table SD2, Fig. 3) Sea level reconstructions of the Pleistocene sequence from IODP Hole 310-M0005D [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.763765, In supplement to: Fujita, K et al. (2010): Sea-level rise during Termination II inferred from large benthic foraminifers: IODP Expedition 310, Tahiti Sea Level. Marine Geology, 271(1-2), 149-155, https://doi.org/10.1016/j.margeo.2010.01.019
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Project(s):
Coverage:
Latitude: -17.766520 * Longitude: -149.550790
Date/Time Start: 2005-10-10T22:55:00 * Date/Time End: 2005-10-12T03:33:00
Minimum DEPTH, sediment/rock: 106 m * Maximum DEPTH, sediment/rock: 134 m
Event(s):
310-M0005D (TAH-03A-4C) * Latitude: -17.766520 * Longitude: -149.550790 * Date/Time Start: 2005-10-10T22:55:00 * Date/Time End: 2005-10-12T03:33:00 * Elevation: -59.6 m * Penetration: 102.17 m * Recovery: 51.35 m * Location: Tahiti, offshore Maraa * Campaign: Exp310 (Tahiti Sea Level) * Basis: DP Hunter * Method/Device: Drilling/drill rig (DRILL) * Comment: Coordinate system: WGS84, Time zone: UTC -10
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Sample code/label | Sample label | Fujita, Kazuhiko | DSDP/ODP/IODP sample designation | ||
| 2 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 3 | Paleoelevation | Paleoelevation | m a.s.l. | Fujita, Kazuhiko | Calculated | A mid-point value of estimated depth range with upper and lower limits. |
| 4 | Paleoelevation, standard deviation | Paleoelevation std dev | ± | Fujita, Kazuhiko | A mid-point value of estimated depth range with upper and lower limits. | |
| 5 | Sea level, relative | Sea lev rel | m | Fujita, Kazuhiko | Sea-level positions estimated by adding paleo water depth to the core depth. | |
| 6 | Sea level, relative standard deviation | Sea level std dev | ± | Fujita, Kazuhiko | Sea-level positions estimated by adding paleo water depth to the core depth. | |
| 7 | Subsidence | Subs | m | Fujita, Kazuhiko | Termination II (MIS 6/5e transition). Subsidence since Terminations II, III, and IV was calculated from reported subsidence rates of Tahiti (~0.25 mm yr-1; Bard et al., 1996, doi:10.1038/382241a0), multiplied by the mid-point age of the MIS 6/5e transition (ca. 130 ka; e.g., Thompson and Goldstein, 2006, doi:10.1126/science.1104035), the MIS 8/7 transition (ca. 245 ka; Imbrie et al., 1984), and the MIS 10/9 transition (ca. 340 ka; Imbrie et al., 1984). | |
| 8 | Sea level, corrected | Sea lev corr | m | Fujita, Kazuhiko | Termination II (MIS 6/5e transition). The positions of past sea levels were calculated by correcting the positions of relative sea levels for subsidence since the time of deposition. | |
| 9 | Sea level, corrected, standard deviation | Sea lev corr std dev | ± | Fujita, Kazuhiko | Termination II (MIS 6/5e transition). The positions of past sea levels were calculated by correcting the positions of relative sea levels for subsidence since the time of deposition. | |
| 10 | Subsidence | Subs | m | Fujita, Kazuhiko | Termination III (MIS 8/7 transition). Subsidence since Terminations II, III, and IV was calculated from reported subsidence rates of Tahiti (~0.25 mm yr-1; Bard et al., 1996, doi:10.1038/382241a0), multiplied by the mid-point age of the MIS 6/5e transition (ca. 130 ka; e.g., Thompson and Goldstein, 2006, doi:10.1126/science.1104035), the MIS 8/7 transition (ca. 245 ka; Imbrie et al., 1984), and the MIS 10/9 transition (ca. 340 ka; Imbrie et al., 1984). | |
| 11 | Sea level, corrected | Sea lev corr | m | Fujita, Kazuhiko | Termination III (MIS 8/7 transition). The positions of past sea levels were calculated by correcting the positions of relative sea levels for subsidence since the time of deposition. | |
| 12 | Sea level, corrected, standard deviation | Sea lev corr std dev | ± | Fujita, Kazuhiko | Termination III (MIS 8/7 transition). The positions of past sea levels were calculated by correcting the positions of relative sea levels for subsidence since the time of deposition. | |
| 13 | Subsidence | Subs | m | Fujita, Kazuhiko | Termination IV (MIS 10/9 transition). Subsidence since Terminations II, III, and IV was calculated from reported subsidence rates of Tahiti (~0.25 mm yr-1; Bard et al., 1996, doi:10.1038/382241a0), multiplied by the mid-point age of the MIS 6/5e transition (ca. 130 ka; e.g., Thompson and Goldstein, 2006, doi:10.1126/science.1104035), the MIS 8/7 transition (ca. 245 ka; Imbrie et al., 1984), and the MIS 10/9 transition (ca. 340 ka; Imbrie et al., 1984). | |
| 14 | Sea level, corrected | Sea lev corr | m | Fujita, Kazuhiko | Termination IV (MIS 10/9 transition). The positions of past sea levels were calculated by correcting the positions of relative sea levels for subsidence since the time of deposition. | |
| 15 | Sea level, corrected, standard deviation | Sea lev corr std dev | ± | Fujita, Kazuhiko | Termination IV (MIS 10/9 transition). The positions of past sea levels were calculated by correcting the positions of relative sea levels for subsidence since the time of deposition. |
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98 data points