Ruddiman, William F; Farrell, John W (1996): Calcium carbonate content of sediment core V22-195 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.51227
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: 13.417000 * Longitude: -19.450000
Date/Time Start: 1966-05-22T00:00:00 * Date/Time End: 1966-05-22T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 10.76 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:
62 data points
Data
| 1 Depth sed [m] | 2 CaCO3 [%] |
|---|---|
| 0.00 | 39.30 |
| 0.10 | 49.90 |
| 0.20 | 32.10 |
| 0.30 | 32.40 |
| 0.40 | 9.70 |
| 0.50 | 7.40 |
| 0.60 | 5.80 |
| 0.80 | 1.20 |
| 1.00 | 1.40 |
| 1.20 | 3.60 |
| 1.40 | 1.20 |
| 1.60 | 3.80 |
| 1.80 | 14.40 |
| 2.00 | 7.20 |
| 2.20 | 0.60 |
| 2.40 | 0.90 |
| 2.60 | 1.90 |
| 2.80 | 16.00 |
| 3.00 | 8.70 |
| 3.20 | 22.00 |
| 3.40 | 31.30 |
| 3.60 | 17.30 |
| 3.80 | 11.30 |
| 4.00 | 42.10 |
| 4.20 | 46.20 |
| 4.40 | 12.00 |
| 4.60 | 8.60 |
| 4.80 | 6.60 |
| 5.00 | 5.50 |
| 5.20 | 1.90 |
| 5.40 | 4.40 |
| 5.60 | 8.00 |
| 5.80 | 3.50 |
| 6.00 | 4.80 |
| 6.20 | 2.50 |
| 6.40 | 0.90 |
| 6.60 | 13.90 |
| 6.80 | 4.30 |
| 7.00 | 4.40 |
| 7.20 | 2.30 |
| 7.40 | 2.60 |
| 7.60 | 24.20 |
| 7.80 | 5.10 |
| 7.90 | 9.90 |
| 8.00 | 20.40 |
| 8.20 | 36.30 |
| 8.30 | 19.30 |
| 8.40 | 5.00 |
| 8.50 | 5.40 |
| 8.60 | 1.20 |
| 8.70 | 0.30 |
| 8.80 | 0.90 |
| 9.00 | 0.90 |
| 9.20 | 49.20 |
| 9.40 | 16.60 |
| 9.60 | 6.20 |
| 9.80 | 16.10 |
| 10.00 | 17.30 |
| 10.20 | 1.60 |
| 10.40 | 0.60 |
| 10.60 | 8.30 |
| 10.76 | 39.90 |