Ruddiman, William F; Farrell, John W (1996): Calcium carbonate content of sediment core V17-154 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.51185
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Ruddiman, William F; Farrell, John W (1992): Calcium carbonate database. IGBP/PAGES World Data Center Paleoclimatology, Boulder, Colorado, NOAA Paleoclimatology Program, http://www.ngdc.noaa.gov/paleo/, 91-004, ftp://ftp.ngdc.noaa.gov/paleo/paleocean/carbonate/data
Coverage:
Latitude: 0.383000 * Longitude: -17.970000
Date/Time Start: 1961-07-13T00:00:00 * Date/Time End: 1961-07-13T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 9.80 m
Event(s):
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Calcium carbonate | CaCO3 | % | Ruddiman, William F | Mercury rig; Hulsemann, 1966, J.Sed.Pet. |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
59 data points
Data
| 1 Depth sed [m] | 2 CaCO3 [%] |
|---|---|
| 0.00 | 84.61 |
| 0.10 | 87.35 |
| 0.20 | 86.36 |
| 0.30 | 87.74 |
| 0.40 | 86.54 |
| 0.50 | 86.63 |
| 0.60 | 75.27 |
| 0.70 | 87.30 |
| 0.80 | 83.98 |
| 0.90 | 87.92 |
| 1.00 | 86.98 |
| 1.20 | 89.07 |
| 1.40 | 85.75 |
| 1.60 | 85.74 |
| 1.80 | 87.03 |
| 2.00 | 87.99 |
| 2.20 | 82.22 |
| 2.40 | 87.72 |
| 2.60 | 79.06 |
| 2.80 | 45.91 |
| 2.80 | 46.89 |
| 3.00 | 81.41 |
| 3.20 | 78.80 |
| 3.30 | 84.05 |
| 3.40 | 85.91 |
| 3.60 | 84.82 |
| 3.70 | 82.54 |
| 3.80 | 85.44 |
| 4.00 | 81.61 |
| 4.10 | 81.39 |
| 4.20 | 91.33 |
| 4.40 | 89.05 |
| 4.60 | 76.60 |
| 4.80 | 78.55 |
| 5.00 | 88.73 |
| 5.20 | 86.61 |
| 5.40 | 70.23 |
| 5.60 | 76.96 |
| 5.80 | 83.92 |
| 6.00 | 81.17 |
| 6.20 | 79.71 |
| 6.40 | 66.16 |
| 6.60 | 81.27 |
| 6.80 | 84.73 |
| 7.00 | 87.17 |
| 7.20 | 90.48 |
| 7.40 | 89.48 |
| 7.60 | 89.37 |
| 7.80 | 86.60 |
| 8.00 | 81.48 |
| 8.20 | 89.63 |
| 8.40 | 89.98 |
| 8.60 | 84.98 |
| 8.80 | 80.79 |
| 9.00 | 83.00 |
| 9.20 | 84.70 |
| 9.40 | 79.49 |
| 9.60 | 80.24 |
| 9.80 | 80.65 |