Farrell, John W; Prell, Warren L (1991): Calcium carbonate content of sediment core V24-62 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.133070, 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: 3.067000 * Longitude: -153.583000
Date/Time Start: 1967-03-15T00:00:00 * Date/Time End: 1967-03-15T00:00:00
Minimum DEPTH, sediment/rock: 0.10 m * Maximum DEPTH, sediment/rock: 12.90 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:
125 data points
Data
1 Depth sed [m] | 2 Age [ka BP] | 3 CaCO3 [%] |
---|---|---|
0.10 | 20 | 81 |
0.20 | 39 | 84 |
0.30 | 68 | 75 |
0.40 | 96 | 34 |
0.50 | 126 | 44 |
0.60 | 156 | 63 |
0.70 | 196 | 32 |
0.80 | 237 | 17 |
0.90 | 278 | 21 |
1.00 | 318 | 18 |
1.10 | 359 | 32 |
1.15 | 379 | 21 |
1.20 | 400 | 22 |
1.30 | 440 | 29 |
1.40 | 481 | 23 |
1.50 | 522 | 64 |
1.60 | 588 | 38 |
1.65 | 601 | 43 |
1.70 | 615 | 83 |
1.80 | 641 | 88 |
1.90 | 655 | 87 |
2.00 | 669 | 64 |
2.10 | 686 | 61 |
2.20 | 704 | 86 |
2.30 | 713 | 71 |
2.40 | 721 | 42 |
2.50 | 730 | 45 |
2.60 | 775 | 22 |
2.70 | 811 | 42 |
2.80 | 847 | 48 |
2.90 | 882 | 16 |
3.00 | 901 | 26 |
3.10 | 928 | 41 |
3.20 | 963 | 35 |
3.30 | 994 | 34 |
3.40 | 1022 | 31 |
3.50 | 1050 | 17 |
3.60 | 1108 | 26 |
3.70 | 1167 | 20 |
3.80 | 1225 | 12 |
3.90 | 1283 | 5 |
4.00 | 1342 | 3 |
4.10 | 1400 | 3 |
4.20 | 1427 | 4 |
4.30 | 1453 | 5 |
4.40 | 1480 | 19 |
4.50 | 1506 | 13 |
4.60 | 1550 | 15 |
4.70 | 1594 | 10 |
4.80 | 1638 | 22 |
4.90 | 1682 | 25 |
5.00 | 1726 | 10 |
5.10 | 1770 | 17 |
5.20 | 1814 | 6 |
5.40 | 1888 | 14 |
5.50 | 1905 | 10 |
5.60 | 1922 | 31 |
5.70 | 1939 | 36 |
5.90 | 1972 | 14 |
6.00 | 1989 | 16 |
6.10 | 2006 | 19 |
6.30 | 2039 | 30 |
6.40 | 2056 | 32 |
6.50 | 2086 | 38 |
6.60 | 2115 | 29 |
6.80 | 2175 | 31 |
6.90 | 2204 | 27 |
7.00 | 2234 | 24 |
7.10 | 2261 | 26 |
7.20 | 2287 | 31 |
7.30 | 2314 | 40 |
7.40 | 2340 | 26 |
7.50 | 2366 | 37 |
7.60 | 2391 | 35 |
7.70 | 2416 | 15 |
7.80 | 2441 | 6 |
7.90 | 2453 | 13 |
8.00 | 2464 | 25 |
8.10 | 2484 | 21 |
8.20 | 2511 | 20 |
8.30 | 2538 | 30 |
8.40 | 2566 | 34 |
8.50 | 2593 | 35 |
8.60 | 2620 | 31 |
8.70 | 2647 | 24 |
8.80 | 2675 | 26 |
8.90 | 2702 | 17 |
9.00 | 2729 | 11 |
9.10 | 2756 | 10 |
9.20 | 2784 | 7 |
9.30 | 2811 | 10 |
9.40 | 2838 | 7 |
9.50 | 2866 | 5 |
9.60 | 2893 | 3 |
9.80 | 2956 | 3 |
9.90 | 2991 | 4 |
10.00 | 3027 | 2 |
10.10 | 3062 | 2 |
10.20 | 3088 | 2 |
10.30 | 3105 | 3 |
10.40 | 3122 | 2 |
10.60 | 3155 | 2 |
10.70 | 3172 | 4 |
10.80 | 3198 | 2 |
10.90 | 3235 | 3 |
11.00 | 3272 | 2 |
11.10 | 3308 | 3 |
11.20 | 3345 | 2 |
11.30 | 3382 | 2 |
11.40 | 3416 | 3 |
11.50 | 3448 | 4 |
11.60 | 3479 | 2 |
11.70 | 3511 | 3 |
11.80 | 3543 | 3 |
11.90 | 3575 | 2 |
12.00 | 3606 | 2 |
12.10 | 3638 | 3 |
12.20 | 3670 | 2 |
12.30 | 3702 | 2 |
12.40 | 3734 | 2 |
12.50 | 3765 | 2 |
12.60 | 3797 | 3 |
12.70 | 3829 | 2 |
12.80 | 3861 | 2 |
12.90 | 3892 | 5 |