Farrell, John W; Prell, Warren L (1991): Calcium carbonate content of sediment core RC11-209. PANGAEA, https://doi.org/10.1594/PANGAEA.133060, 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: 3.650000 * Longitude: -140.100000
Date/Time Start: 1967-09-07T00:00:00 * Date/Time End: 1967-09-07T00:00:00
Minimum DEPTH, sediment/rock: 0.10 m * Maximum DEPTH, sediment/rock: 14.60 m
Event(s):
RC11-209 * Latitude: 3.650000 * Longitude: -140.100000 * Date/Time: 1967-09-07T00:00:00 * Elevation: -4400.0 m * Recovery: 14.63 m * Campaign: RC11 (RC1112) * Basis: Robert Conrad * Method/Device: Piston corer (PC)
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:
153 data points
Data
1 Depth sed [m] | 2 Age [ka BP] | 3 CaCO3 [%] |
---|---|---|
0.10 | 10 | 87 |
0.20 | 20 | 87 |
0.25 | 25 | 87 |
0.30 | 30 | 89 |
0.37 | 37 | 88 |
0.40 | 39 | 90 |
0.50 | 45 | 92 |
0.60 | 51 | 90 |
0.63 | 53 | 87 |
0.70 | 57 | 90 |
0.80 | 63 | 84 |
0.90 | 72 | 73 |
1.00 | 86 | 71 |
1.03 | 90 | 68 |
1.10 | 102 | 72 |
1.20 | 121 | 72 |
1.26 | 130 | 85 |
1.30 | 135 | 73 |
1.40 | 145 | 89 |
1.50 | 156 | 86 |
1.60 | 167 | 86 |
1.66 | 175 | 80 |
1.70 | 179 | 76 |
1.80 | 194 | 52 |
1.87 | 209 | 54 |
1.90 | 217 | 62 |
2.00 | 229 | 74 |
2.10 | 241 | 88 |
2.20 | 255 | 84 |
2.27 | 267 | 67 |
2.30 | 272 | 73 |
2.40 | 305 | 55 |
2.50 | 318 | 66 |
2.60 | 332 | 71 |
2.70 | 338 | 82 |
2.80 | 344 | 88 |
2.90 | 349 | 84 |
3.00 | 354 | 72 |
3.10 | 372 | 66 |
3.20 | 393 | 60 |
3.30 | 420 | 74 |
3.40 | 428 | 89 |
3.50 | 437 | 88 |
3.60 | 445 | 87 |
3.70 | 452 | 85 |
3.80 | 459 | 78 |
3.90 | 469 | 61 |
4.00 | 481 | 61 |
4.10 | 496 | 85 |
4.20 | 513 | 89 |
4.30 | 529 | 89 |
4.40 | 542 | 86 |
4.50 | 556 | 83 |
4.60 | 571 | 76 |
4.70 | 583 | 81 |
4.80 | 596 | 83 |
4.90 | 612 | 82 |
5.00 | 625 | 91 |
5.10 | 630 | 92 |
5.20 | 634 | 91 |
5.30 | 639 | 94 |
5.40 | 644 | 95 |
5.50 | 652 | 92 |
5.60 | 659 | 89 |
5.70 | 666 | 89 |
5.80 | 673 | 84 |
5.90 | 679 | 83 |
6.00 | 686 | 93 |
6.10 | 692 | 93 |
6.20 | 698 | 88 |
6.30 | 704 | 95 |
6.40 | 708 | 94 |
6.50 | 713 | 93 |
6.60 | 717 | 92 |
6.70 | 722 | 79 |
6.80 | 726 | 76 |
6.90 | 732 | 91 |
7.00 | 743 | 87 |
7.10 | 755 | 87 |
7.20 | 765 | 77 |
7.30 | 772 | 72 |
7.40 | 782 | 56 |
7.50 | 795 | 86 |
7.60 | 809 | 87 |
7.70 | 822 | 85 |
7.80 | 834 | 87 |
7.90 | 845 | 87 |
8.00 | 856 | 85 |
8.10 | 866 | 71 |
8.20 | 877 | 52 |
8.30 | 888 | 61 |
8.40 | 899 | 71 |
8.50 | 910 | 79 |
8.60 | 920 | 87 |
8.70 | 930 | 82 |
8.80 | 940 | 88 |
9.00 | 961 | 74 |
9.10 | 970 | 85 |
9.20 | 979 | 88 |
9.30 | 1002 | 78 |
9.40 | 1026 | 73 |
9.50 | 1050 | 64 |
9.60 | 1056 | 78 |
9.70 | 1063 | 88 |
9.80 | 1077 | 84 |
9.90 | 1091 | 72 |
10.00 | 1107 | 76 |
10.10 | 1123 | 81 |
10.20 | 1148 | 78 |
10.30 | 1160 | 83 |
10.40 | 1172 | 90 |
10.50 | 1191 | 86 |
10.60 | 1209 | 79 |
10.70 | 1232 | 85 |
10.80 | 1252 | 86 |
10.90 | 1268 | 77 |
11.00 | 1285 | 71 |
11.10 | 1301 | 80 |
11.20 | 1322 | 71 |
11.30 | 1343 | 84 |
11.40 | 1360 | 85 |
11.50 | 1373 | 70 |
11.60 | 1387 | 66 |
11.70 | 1400 | 56 |
11.80 | 1412 | 59 |
11.90 | 1423 | 78 |
12.00 | 1439 | 83 |
12.10 | 1458 | 64 |
12.20 | 1471 | 71 |
12.30 | 1485 | 74 |
12.40 | 1496 | 70 |
12.50 | 1506 | 55 |
12.60 | 1521 | 78 |
12.70 | 1535 | 89 |
12.80 | 1549 | 83 |
12.90 | 1568 | 89 |
13.00 | 1586 | 81 |
13.10 | 1605 | 77 |
13.20 | 1623 | 76 |
13.30 | 1641 | 77 |
13.40 | 1658 | 88 |
13.50 | 1691 | 73 |
13.60 | 1725 | 65 |
13.70 | 1752 | 67 |
13.80 | 1779 | 80 |
13.90 | 1807 | 80 |
14.00 | 1838 | 68 |
14.10 | 1868 | 61 |
14.20 | 1891 | 65 |
14.30 | 1904 | 66 |
14.40 | 1916 | 75 |
14.50 | 1928 | 81 |
14.60 | 1957 | 82 |