Farrell, John W; Prell, Warren L (1991): Calcium carbonate content of sediment core V24-59 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.133069, 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: 2.567000 * Longitude: -145.533000
Date/Time Start: 1967-03-13T00:00:00 * Date/Time End: 1967-03-13T00:00:00
Minimum DEPTH, sediment/rock: 0.10 m * Maximum DEPTH, sediment/rock: 10.10 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:
105 data points
Data
1 Depth sed [m] | 2 Age [ka BP] | 3 CaCO3 [%] |
---|---|---|
0.10 | 16 | 87 |
0.20 | 32 | 88 |
0.30 | 45 | 92 |
0.40 | 56 | 88 |
0.50 | 67 | 67 |
0.55 | 85 | 57 |
0.60 | 106 | 52 |
0.70 | 156 | 70 |
0.80 | 185 | 60 |
0.90 | 215 | 62 |
1.00 | 245 | 56 |
1.10 | 275 | 60 |
1.20 | 305 | 34 |
1.30 | 344 | 48 |
1.40 | 383 | 47 |
1.50 | 422 | 74 |
1.60 | 452 | 71 |
1.70 | 475 | 48 |
1.80 | 498 | 68 |
1.90 | 522 | 82 |
2.00 | 555 | 68 |
2.10 | 588 | 60 |
2.20 | 603 | 66 |
2.30 | 618 | 90 |
2.40 | 633 | 90 |
2.50 | 645 | 91 |
2.60 | 654 | 93 |
2.70 | 663 | 86 |
2.75 | 668 | 81 |
2.80 | 672 | 73 |
2.90 | 681 | 65 |
3.00 | 690 | 86 |
3.10 | 699 | 86 |
3.20 | 707 | 92 |
3.30 | 713 | 88 |
3.40 | 719 | 71 |
3.50 | 725 | 61 |
3.60 | 748 | 68 |
3.70 | 775 | 47 |
3.80 | 797 | 65 |
3.90 | 818 | 75 |
4.00 | 841 | 78 |
4.10 | 865 | 57 |
4.20 | 893 | 42 |
4.30 | 927 | 66 |
4.40 | 961 | 59 |
4.50 | 1014 | 70 |
4.60 | 1082 | 58 |
4.70 | 1150 | 51 |
4.80 | 1218 | 77 |
4.85 | 1252 | 80 |
4.90 | 1286 | 58 |
5.00 | 1354 | 59 |
5.10 | 1422 | 65 |
5.20 | 1490 | 48 |
5.30 | 1558 | 53 |
5.40 | 1626 | 53 |
5.50 | 1697 | 44 |
5.60 | 1770 | 41 |
5.70 | 1843 | 52 |
5.80 | 1905 | 56 |
5.90 | 1955 | 53 |
6.00 | 2006 | 61 |
6.10 | 2056 | 60 |
6.20 | 2100 | 60 |
6.30 | 2145 | 56 |
6.40 | 2190 | 59 |
6.50 | 2234 | 52 |
6.60 | 2264 | 58 |
6.70 | 2294 | 76 |
6.80 | 2324 | 64 |
6.90 | 2354 | 62 |
7.00 | 2383 | 60 |
7.10 | 2412 | 63 |
7.20 | 2441 | 36 |
7.30 | 2460 | 59 |
7.40 | 2489 | 63 |
7.50 | 2526 | 69 |
7.60 | 2564 | 71 |
7.70 | 2601 | 61 |
7.80 | 2639 | 50 |
7.90 | 2676 | 35 |
8.00 | 2714 | 60 |
8.10 | 2751 | 56 |
8.20 | 2789 | 57 |
8.30 | 2826 | 49 |
8.40 | 2864 | 54 |
8.50 | 2901 | 39 |
8.60 | 2960 | 30 |
8.70 | 3040 | 24 |
8.80 | 3139 | 35 |
8.90 | 3217 | 49 |
9.00 | 3290 | 39 |
9.10 | 3363 | 45 |
9.20 | 3436 | 29 |
9.30 | 3509 | 33 |
9.40 | 3581 | 29 |
9.50 | 3642 | 26 |
9.60 | 3677 | 34 |
9.70 | 3711 | 33 |
9.80 | 3746 | 34 |
9.85 | 3763 | 38 |
9.90 | 3780 | 36 |
10.00 | 3815 | 50 |
10.10 | 3849 | 53 |