Loubere, Paul; Mekik, Figen; Francois, Roger; Pichat, Sylvain (2014): (Table 3) Th230 excess content and calcite accumulation rates in the eastern equatorial Pacific [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.839227, In supplement to: Loubere, P et al. (2004): Export fluxes of calcite in the eastern equatorial Pacific from the Last Glacial Maximum to present. Paleoceanography, 19(2), PA2018, https://doi.org/10.1029/2003PA000986
Always quote citation above when using data! You can download the citation in several formats below.
Project(s):
Ocean Drilling Program (ODP)
Coverage:
Median Latitude: -0.998980 * Median Longitude: -95.391167 * South-bound Latitude: -3.094930 * West-bound Longitude: -110.519710 * North-bound Latitude: 0.183050 * East-bound Longitude: -86.483330
Date/Time Start: 1970-04-26T00:00:00 * Date/Time End: 1991-06-10T12:04:00
Minimum DEPTH, sediment/rock: 0.000 m * Maximum DEPTH, sediment/rock: 2.600 m
Event(s):
138-846B * Latitude: -3.094930 * Longitude: -90.817960 * Date/Time Start: 1991-05-21T17:00:00 * Date/Time End: 1991-05-24T06:08:00 * Elevation: -3295.8 m * Penetration: 422.4 m * Recovery: 373.44 m * Location: South Pacific Ocean * Campaign: Leg138 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 45 cores; 422.4 m cored; 0 m drilled; 88.4 % recovery
138-849B * Latitude: 0.183050 * Longitude: -110.519710 * Date/Time Start: 1991-06-07T23:25:00 * Date/Time End: 1991-06-10T12:04:00 * Elevation: -3839.1 m * Penetration: 350.5 m * Recovery: 343.78 m * Location: North Pacific Ocean * Campaign: Leg138 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 37 cores; 350.5 m cored; 0 m drilled; 98.1 % recovery
Comment:
Age dating of sediment intervals is based on oxygen isotope stratigraphy and identification of 4 intervals, or boundaries: postdeglacial, MIS 1/2, MIS 2.2, and MIS 2/3. Data are averaged for intervals defined by these boundaries for presentation in Figures 3 and 12.
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Event label | Event | ||||
| 2 | Latitude of event | Latitude | ||||
| 3 | Longitude of event | Longitude | ||||
| 4 | Elevation of event | Elevation | m | |||
| 5 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 6 | AGE | Age | ka BP | Geocode | ||
| 7 | Thorium-230 excess | 230Th xs | dpm/g | Loubere, Paul | ||
| 8 | Calcite | Cal | % | Loubere, Paul | # = interpolated | |
| 9 | Accumulation rate, calcite | Acc rate cal | g/cm2/ka | Loubere, Paul | ||
| 10 | Calcite, fractionated | Cal frac | % | Loubere, Paul | preserved | |
| 11 | Method comment | Method comm | Loubere, Paul | Globorotalia menardii done, yes/no | ||
| 12 | Calcite, flux | Cal flux | µmol/cm2/a | Loubere, Paul | here µmol/cm**2/a = 10 * g/cm**2/ka |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
407 data points
Data
| 1 Event | 2 Latitude | 3 Longitude | 4 Elevation [m] | 5 Depth sed [m] | 6 Age [ka BP] | 7 230Th xs [dpm/g] | 8 Cal [%] | 9 Acc rate cal [g/cm2/ka] | 10 Cal frac [%] | 11 Method comm | 12 Cal flux [µmol/cm2/a] |
|---|---|---|---|---|---|---|---|---|---|---|---|
| VNTR01-13GC | -3.0920 | -90.8230 | -3304 | 0.000 | 2.0 | 12.06 | 60.6 | 0.43 | 15.90 | yes | 26.9 |
| VNTR01-13GC | -3.0920 | -90.8230 | -3304 | 0.050 | 3.6 | 11.69 | 62.9 | 0.45 | 16.80 | yes | 26.7 |
| 138-846B | -3.0949 | -90.8180 | -3296 | 0.060 | 5.5 | 11.33 | 57.4 | 0.42 | 24.40 | yes | 17.2 |
| 138-846B | -3.0949 | -90.8180 | -3296 | 0.130 | 59.1 | 31.07 | yes | ||||
| 138-846B | -3.0949 | -90.8180 | -3296 | 0.195 | 8.2 | 8.80 | 58.4 | 0.55 | 32.10 | no | 17.1 |
| 138-846B | -3.0949 | -90.8180 | -3296 | 0.270 | 10.3 | 7.23 | #60.0 | 0.65 | 33.70 | yes | 19.2 |
| 138-846B | -3.0949 | -90.8180 | -3296 | 0.330 | 12.0 | 6.80 | #60.5 | 0.69 | 33.50 | yes | 20.4 |
| 138-846B | -3.0949 | -90.8180 | -3296 | 0.390 | 12.9 | 7.08 | 60.9 | 0.66 | 32.50 | yes | 20.0 |
| 138-846B | -3.0949 | -90.8180 | -3296 | 0.430 | 38.30 | yes | |||||
| 138-846B | -3.0949 | -90.8180 | -3296 | 0.450 | 14.0 | 6.16 | #60.0 | 0.74 | 38.30 | no | 19.3 |
| 138-846B | -3.0949 | -90.8180 | -3296 | 0.500 | 59.8 | 39.40 | yes | ||||
| 138-846B | -3.0949 | -90.8180 | -3296 | 0.540 | 16.0 | 5.79 | #60.0 | 0.78 | 44.00 | yes | 17.7 |
| 138-846B | -3.0949 | -90.8180 | -3296 | 0.590 | 17.1 | 6.26 | 60.2 | 0.71 | 39.80 | yes | 17.8 |
| 138-846B | -3.0949 | -90.8180 | -3296 | 0.630 | 18.0 | 6.13 | #57.8 | 0.69 | 57.70 | yes | 11.9 |
| 138-846B | -3.0949 | -90.8180 | -3296 | 0.690 | 19.8 | 6.10 | 54.3 | 0.64 | 53.30 | no | 12.0 |
| 138-846B | -3.0949 | -90.8180 | -3296 | 0.730 | 21.0 | 5.89 | #56.1 | 0.68 | 50.40 | no | 13.5 |
| 138-846B | -3.0949 | -90.8180 | -3296 | 0.790 | 21.6 | 6.45 | 58.0 | 0.64 | 45.90 | yes | 13.9 |
| 138-846B | -3.0949 | -90.8180 | -3296 | 0.830 | 22.0 | 6.20 | 54.9 | 0.63 | 41.40 | yes | 15.2 |
| 138-846B | -3.0949 | -90.8180 | -3296 | 0.880 | 22.6 | 6.41 | 54.5 | 0.60 | 62.90 | yes | 9.5 |
| 138-846B | -3.0949 | -90.8180 | -3296 | 0.950 | 23.7 | 7.11 | 55.6 | 0.55 | 43.80 | yes | 12.6 |
| 138-846B | -3.0949 | -90.8180 | -3296 | 1.010 | 24.7 | 7.40 | 58.5 | 0.55 | 56.00 | yes | 9.8 |
| 138-846B | -3.0949 | -90.8180 | -3296 | 1.070 | 57.3 | no | |||||
| 138-846B | -3.0949 | -90.8180 | -3296 | 1.130 | 25.9 | 5.99 | 56.0 | 0.64 | 51.50 | no | 12.4 |
| 138-846B | -3.0949 | -90.8180 | -3296 | 1.190 | 58.4 | no | |||||
| 138-846B | -3.0949 | -90.8180 | -3296 | 1.240 | 27.3 | 6.38 | 52.0 | 0.55 | 47.00 | yes | 11.7 |
| 138-846B | -3.0949 | -90.8180 | -3296 | 1.290 | 51.0 | 42.90 | no | ||||
| 138-846B | -3.0949 | -90.8180 | -3296 | 1.330 | 28.2 | 6.24 | 51.2 | 0.55 | 37.30 | yes | 14.7 |
| Y69-71P | 0.1000 | -86.4833 | -2740 | 0.100 | 3.5 | 7.80 | 60.6 | 0.54 | 23.60 | yes | 22.9 |
| Y69-71P | 0.1000 | -86.4833 | -2740 | 0.180 | 25.90 | yes | |||||
| Y69-71P | 0.1000 | -86.4833 | -2740 | 0.200 | 5.2 | 7.22 | 63.7 | 0.61 | 24.80 | no | 24.6 |
| Y69-71P | 0.1000 | -86.4833 | -2740 | 0.300 | 6.3 | 6.71 | 65.1 | 0.66 | 21.30 | yes | 30.9 |
| Y69-71P | 0.1000 | -86.4833 | -2740 | 0.400 | 7.0 | 6.17 | 66.4 | 0.73 | 19.80 | yes | 36.7 |
| Y69-71P | 0.1000 | -86.4833 | -2740 | 0.500 | 26.40 | yes | |||||
| Y69-71P | 0.1000 | -86.4833 | -2740 | 0.600 | 10.6 | 5.47 | 58.2 | 0.70 | 36.30 | yes | 19.3 |
| Y69-71P | 0.1000 | -86.4833 | -2740 | 0.710 | 29.30 | yes | |||||
| Y69-71P | 0.1000 | -86.4833 | -2740 | 0.800 | 13.6 | 5.04 | 65.7 | 0.83 | 32.50 | no | 25.5 |
| Y69-71P | 0.1000 | -86.4833 | -2740 | 0.900 | 36.80 | yes | |||||
| Y69-71P | 0.1000 | -86.4833 | -2740 | 1.000 | 15.5 | 4.14 | 67.6 | 1.02 | 39.20 | yes | 26.0 |
| Y69-71P | 0.1000 | -86.4833 | -2740 | 1.120 | 43.10 | yes | |||||
| Y69-71P | 0.1000 | -86.4833 | -2740 | 1.200 | 17.5 | 4.52 | 68.5 | 0.93 | 42.40 | yes | 21.9 |
| Y69-71P | 0.1000 | -86.4833 | -2740 | 1.300 | 32.30 | yes | |||||
| Y69-71P | 0.1000 | -86.4833 | -2740 | 1.390 | 19.0 | 4.79 | 63.8 | 0.81 | 43.10 | no | 18.8 |
| Y69-71P | 0.1000 | -86.4833 | -2740 | 1.460 | 49.50 | yes | |||||
| Y69-71P | 0.1000 | -86.4833 | -2740 | 1.600 | 20.5 | 4.58 | 64.2 | 0.84 | 44.30 | no | 18.9 |
| Y69-71P | 0.1000 | -86.4833 | -2740 | 1.700 | 40.60 | yes | |||||
| Y69-71P | 0.1000 | -86.4833 | -2740 | 1.800 | 22.0 | 5.51 | 64.6 | 0.69 | 35.20 | no | 19.6 |
| Y69-71P | 0.1000 | -86.4833 | -2740 | 2.000 | 23.5 | 5.59 | 66.7 | 0.69 | 37.80 | yes | 18.2 |
| Y69-71P | 0.1000 | -86.4833 | -2740 | 2.200 | 24.8 | 5.65 | 66.5 | 0.67 | 36.00 | yes | 18.6 |
| Y69-71P | 0.1000 | -86.4833 | -2740 | 2.400 | 26.1 | 4.87 | 64.1 | 0.75 | 48.30 | yes | 15.5 |
| Y69-71P | 0.1000 | -86.4833 | -2740 | 2.600 | 27.8 | 5.58 | 61.1 | 0.61 | 34.90 | yes | 17.5 |
| GS7202-16 | 0.0070 | -98.0530 | -3183 | 0.000 | 1.5 | 10.60 | 70.8 | 0.55 | 26.50 | yes | 20.7 |
| RC13-110 | -0.0970 | -95.6500 | -3231 | 0.050 | 2.5 | 9.80 | 62.7 | 0.53 | 27.40 | no | 19.3 |
| RC13-110 | -0.0970 | -95.6500 | -3231 | 0.100 | 3.6 | 11.02 | 68.3 | 0.51 | 28.30 | yes | 17.9 |
| RC13-110 | -0.0970 | -95.6500 | -3231 | 0.140 | 29.90 | yes | |||||
| RC13-110 | -0.0970 | -95.6500 | -3231 | 0.200 | 6.7 | 8.42 | 69.8 | 0.66 | 35.00 | yes | 18.9 |
| RC13-110 | -0.0970 | -95.6500 | -3231 | 0.230 | 7.7 | 8.31 | 71.2 | 0.68 | 40.50 | yes | 16.8 |
| RC13-110 | -0.0970 | -95.6500 | -3231 | 0.300 | 9.9 | 6.75 | 71.8 | 0.83 | 52.80 | yes | 15.6 |
| RC13-110 | -0.0970 | -95.6500 | -3231 | 0.330 | 11.8 | 7.05 | 71.6 | 0.77 | 52.40 | yes | 14.7 |
| RC13-110 | -0.0970 | -95.6500 | -3231 | 0.400 | 14.0 | 8.72 | 69.7 | 0.60 | 44.80 | yes | 13.4 |
| RC13-110 | -0.0970 | -95.6500 | -3231 | 0.430 | 15.5 | 8.31 | 70.2 | 0.62 | 48.00 | yes | 12.9 |
| RC13-110 | -0.0970 | -95.6500 | -3231 | 0.500 | 17.3 | 9.02 | 72.3 | 0.58 | 37.70 | yes | 15.4 |
| RC13-110 | -0.0970 | -95.6500 | -3231 | 0.530 | 19.1 | 9.26 | 70.6 | 0.54 | 37.30 | yes | 14.5 |
| RC13-110 | -0.0970 | -95.6500 | -3231 | 0.600 | 22.0 | 9.02 | 66.7 | 0.51 | 37.80 | yes | 13.5 |
| RC13-110 | -0.0970 | -95.6500 | -3231 | 0.630 | 22.9 | 8.83 | 67.9 | 0.53 | 39.90 | yes | 13.3 |
| RC13-110 | -0.0970 | -95.6500 | -3231 | 0.700 | 42.60 | yes | |||||
| RC13-110 | -0.0970 | -95.6500 | -3231 | 0.730 | 27.8 | 7.80 | 69.7 | 0.61 | 36.40 | yes | 16.7 |
| 138-849B | 0.1830 | -110.5197 | -3839 | 0.110 | 3.4 | 10.67 | 69.0 | 0.63 | 26.80 | yes | 23.6 |
| 138-849B | 0.1830 | -110.5197 | -3839 | 0.300 | 9.1 | 8.30 | 76.0 | 0.85 | 35.00 | no | 24.2 |
| 138-849B | 0.1830 | -110.5197 | -3839 | 0.340 | 77.6 | 37.40 | yes | ||||
| 138-849B | 0.1830 | -110.5197 | -3839 | 0.400 | 12.0 | 8.40 | #76.5 | 0.80 | 37.20 | no | 22.0 |
| 138-849B | 0.1830 | -110.5197 | -3839 | 0.450 | 75.8 | 37.10 | yes | ||||
| 138-849B | 0.1830 | -110.5197 | -3839 | 0.510 | 14.6 | 8.87 | 76.3 | 0.75 | 40.60 | yes | 18.5 |
| 138-849B | 0.1830 | -110.5197 | -3839 | 0.610 | 16.4 | 9.21 | #82.0 | 0.78 | 39.00 | no | 20.0 |
| 138-849B | 0.1830 | -110.5197 | -3839 | 0.630 | 83.4 | 38.30 | yes | ||||
| 138-849B | 0.1830 | -110.5197 | -3839 | 0.750 | 20.2 | 8.48 | 81.8 | 0.78 | 46.50 | yes | 16.8 |
| 138-849B | 0.1830 | -110.5197 | -3839 | 0.830 | 22.3 | 9.31 | 81.0 | 0.69 | 46.40 | yes | 14.9 |
| 138-849B | 0.1830 | -110.5197 | -3839 | 1.000 | 25.9 | 7.24 | 78.7 | 0.82 | 48.50 | yes | 16.9 |
| 138-849B | 0.1830 | -110.5197 | -3839 | 1.100 | 29.1 | 6.69 | 78.9 | 0.87 | 58.00 | yes | 15.0 |
| 138-849B | 0.1830 | -110.5197 | -3839 | 1.200 | 31.7 | 6.08 | #79.0 | 0.94 | 61.00 | no | 15.4 |
| 138-849B | 0.1830 | -110.5197 | -3839 | 1.230 | 79.0 | 63.70 | yes |