Farrell, John W; Prell, Warren L (1991): Calcium carbonate content of sediment core V24-55 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.133067, In supplement to: Farrell, JW; Prell, WL (1991): Pacific CaCO3 preservation and d18O since 4 Ma: paleoceanic and paleoclimatic implications. Paleoceanography, 6(4), 485-498, https://doi.org/10.1029/91PA00877
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Project(s):
Coverage:
Latitude: 2.050000 * Longitude: -134.600000
Date/Time Start: 1967-03-10T00:00:00 * Date/Time End: 1967-03-10T00:00:00
Minimum DEPTH, sediment/rock: 0.10 m * Maximum DEPTH, sediment/rock: 8.30 m
Event(s):
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | AGE | Age | ka BP | Geocode | ||
3 | Calcium carbonate | CaCO3 | % | Farrell, John W | Data source: NGDC 1992, compiled by Farrell &Prell, 1991 |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
81 data points
Data
1 Depth sed [m] | 2 Age [ka BP] | 3 CaCO3 [%] |
---|---|---|
0.10 | 13 | 89 |
0.19 | 25 | 89 |
0.30 | 39 | 92 |
0.60 | 61 | 89 |
0.70 | 69 | 77 |
0.80 | 87 | 82 |
0.90 | 102 | 83 |
1.00 | 113 | 79 |
1.10 | 134 | 82 |
1.20 | 156 | 81 |
1.30 | 178 | 82 |
1.40 | 200 | 79 |
1.50 | 247 | 85 |
1.60 | 285 | 81 |
1.70 | 313 | 82 |
1.80 | 328 | 87 |
1.90 | 344 | 90 |
2.00 | 356 | 89 |
2.10 | 368 | 83 |
2.20 | 380 | 76 |
2.30 | 411 | 87 |
2.40 | 441 | 87 |
2.50 | 452 | 89 |
2.60 | 464 | 85 |
2.70 | 475 | 82 |
2.80 | 506 | 87 |
2.89 | 539 | 85 |
3.00 | 588 | 84 |
3.10 | 602 | 88 |
3.19 | 614 | 90 |
3.30 | 629 | 90 |
3.39 | 641 | 91 |
3.50 | 650 | 91 |
3.60 | 659 | 86 |
3.70 | 668 | 86 |
3.80 | 676 | 87 |
3.90 | 683 | 89 |
4.01 | 691 | 88 |
4.10 | 697 | 91 |
4.20 | 704 | 90 |
4.30 | 709 | 90 |
4.41 | 715 | 87 |
4.50 | 720 | 85 |
4.61 | 726 | 87 |
4.70 | 731 | 88 |
4.79 | 745 | 85 |
4.90 | 760 | 85 |
5.00 | 775 | 80 |
5.10 | 797 | 85 |
5.20 | 818 | 87 |
5.29 | 838 | 86 |
5.41 | 863 | 85 |
5.50 | 882 | 76 |
5.62 | 919 | 82 |
5.72 | 941 | 89 |
5.81 | 961 | 86 |
5.90 | 980 | 89 |
6.02 | 1001 | 90 |
6.10 | 1015 | 91 |
6.20 | 1032 | 85 |
6.30 | 1050 | 81 |
6.40 | 1071 | 84 |
6.50 | 1091 | 87 |
6.59 | 1110 | 86 |
6.70 | 1133 | 87 |
6.79 | 1151 | 84 |
6.88 | 1170 | 83 |
6.99 | 1193 | 83 |
7.10 | 1216 | 81 |
7.19 | 1234 | 80 |
7.30 | 1257 | 85 |
7.41 | 1280 | 83 |
7.50 | 1299 | 86 |
7.60 | 1319 | 80 |
7.70 | 1340 | 80 |
7.80 | 1361 | 80 |
7.90 | 1381 | 83 |
7.99 | 1400 | 78 |
8.10 | 1423 | 87 |
8.19 | 1441 | 86 |
8.30 | 1464 | 84 |