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Thomas, Alexander L; Henderson, Gideon M; Deschamps, Pierre; Yokoyama, Yusuke; Mason, Andrew J; Bard, Edouard; Hamelin, Bruno; Durand, Nicolas; Camoin, Gilbert (2009): (Table S1) Uranium and Thorium isotopes and U/Th ages of IODP Exp310 cores from offshore Tahiti [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.756921, Supplement to: Thomas, AL et al. (2009): Penultimate deglacial sea-level timing from Uranium/Thorium dating of Tahitian corals. Science, 324(5931), 1186-1189, https://doi.org/10.1126/science.1168754

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Abstract:
The timing of sea-level change provides important constraints on the mechanisms driving Earth's climate between glacial and interglacial states. Fossil corals constrain the timing of past sea level by their suitability for dating and their growth position close to sea level. The coral-derived age for the last deglaciation is consistent with climate change forced by Northern Hemisphere summer insolation (NHI), but the timing of the penultimate deglaciation is more controversial. We found, by means of uranium/thorium dating of fossil corals, that sea level during the penultimate deglaciation had risen to ~85 meters below the present sea level by 137,000 years ago, and that it fluctuated on a millennial time scale during deglaciation. This indicates that the penultimate deglaciation occurred earlier with respect to NHI than the last deglacial, beginning when NHI was at a minimum.
Coverage:
Median Latitude: -17.541353 * Median Longitude: -149.480283 * South-bound Latitude: -17.766520 * West-bound Longitude: -149.598790 * North-bound Latitude: -17.488540 * East-bound Longitude: -149.403350
Date/Time Start: 2005-10-10T22:55:00 * Date/Time End: 2005-11-09T05:27:00
Minimum Elevation: -103.2 m * Maximum Elevation: -58.8 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
310-M0009B (TAH-02A-5A) * Latitude: -17.488580 * Longitude: -149.403400 * Date/Time Start: 2005-10-18T21:50:00 * Date/Time End: 2005-10-19T11:40:00 * Elevation: -100.3 m * Penetration: 27.12 m * Recovery: 17.42 m * Location: Tahiti, offshore Tiarei * Campaign: Exp310 (Tahiti Sea Level) * Basis: DP Hunter * Method/Device: Drilling/drill rig (DRILL) * Comment: Coordinate system: WGS84, Time zone: UTC -10
310-M0009C (TAH-02A-5B) * Latitude: -17.488540 * Longitude: -149.403470 * Date/Time Start: 2005-10-20T02:49:00 * Date/Time End: 2005-10-20T19:25:00 * Elevation: -99.8 m * Penetration: 25.66 m * Recovery: 12.66 m * Location: Tahiti, offshore Tiarei * Campaign: Exp310 (Tahiti Sea Level) * Basis: DP Hunter * Method/Device: Drilling/drill rig (DRILL) * Comment: Coordinate system: WGS84, Time zone: UTC -10
Comment:
Features indicating the coral is in growth position are: co, the orientation of the coral; cap, the positioning of an algal crust on the upper surface of the coral; gp, the orientation of partially filled geopetals within the coral; and cf, whether the coral forms part of a continuous framework.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Event labelEvent
2Area/localityAreaThomas, Alexander L
3Sample code/labelSample labelThomas, Alexander LDSDP/ODP/IODP sample designation
4CoralCoralThomas, Alexander L
5DescriptionDescriptionThomas, Alexander LGrowth position indicators
6Depth, reconstructedReconstr depthmThomas, Alexander LCalculated, see reference(s)Subsidence corrected depth [mbsl]
7Uranium-238238Umg/kgThomas, Alexander LMulti-collector inductively coupled plasma mass spectrometer (MC-ICP-MS)
8Uranium-238, standard deviation238U std dev±Thomas, Alexander LMulti-collector inductively coupled plasma mass spectrometer (MC-ICP-MS)
9Hafniasphaera spp.Hafniasphaera spp.Thomas, Alexander LMulti-collector inductively coupled plasma mass spectrometer (MC-ICP-MS)
10Thorium-232, standard deviation232Th std dev±Thomas, Alexander LMulti-collector inductively coupled plasma mass spectrometer (MC-ICP-MS)
11Thorium-230/Uranium-238 activity ratio(230Th/238U)Thomas, Alexander LMulti-collector inductively coupled plasma mass spectrometer (MC-ICP-MS)
12Thorium-230/Uranium-238 activity ratio, standard deviation(230Th/238U) std dev±Thomas, Alexander LMulti-collector inductively coupled plasma mass spectrometer (MC-ICP-MS)
13Uranium-234/Uranium-238 activity ratio(234U/238U)Thomas, Alexander LMulti-collector inductively coupled plasma mass spectrometer (MC-ICP-MS)Calculated as the ratio at the time when the coral grew, using the U/Th age
14Uranium-234/Uranium-238 activity ratio, standard deviation(234U/238U) std dev±Thomas, Alexander LMulti-collector inductively coupled plasma mass spectrometer (MC-ICP-MS)Calculated as the ratio at the time when the coral grew, using the U/Th age
15Thorium-232/Uranium-238 activity ratio(232Th/238U)Thomas, Alexander LMulti-collector inductively coupled plasma mass spectrometer (MC-ICP-MS)
16Thorium-232/Uranium-238 activity ratio, standard deviation(232Th/238U) std dev±Thomas, Alexander LMulti-collector inductively coupled plasma mass spectrometer (MC-ICP-MS)
17AGEAgeka BPGeocode
18Age, standard deviationAge std dev±Thomas, Alexander LMulti-collector inductively coupled plasma mass spectrometer (MC-ICP-MS)
19Uranium-234/Uranium-238 activity ratio(234U/238U)Thomas, Alexander LMulti-collector inductively coupled plasma mass spectrometer (MC-ICP-MS)
20Uranium-234/Uranium-238 activity ratio, standard deviation(234U/238U) std dev±Thomas, Alexander LMulti-collector inductively coupled plasma mass spectrometer (MC-ICP-MS)
21CalciteCal%Thomas, Alexander L
22Calcite, standard deviationCal std dev±Thomas, Alexander L
Size:
678 data points

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