Ruddiman, William F; Farrell, John W (1996): Calcium carbonate content of sediment core V28-14 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.51309
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: 64.783000 * Longitude: -29.570000
Date/Time Start: 1970-07-19T00:00:00 * Date/Time End: 1970-07-19T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 6.11 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:
60 data points
Data
| 1 Depth sed [m] | 2 CaCO3 [%] |
|---|---|
| 0.00 | 64.00 |
| 0.10 | 65.00 |
| 0.20 | 63.20 |
| 0.30 | 54.60 |
| 0.40 | 60.50 |
| 0.50 | 55.80 |
| 0.60 | 56.60 |
| 0.70 | 52.30 |
| 0.80 | 46.20 |
| 0.90 | 32.70 |
| 1.00 | 20.00 |
| 1.10 | 21.90 |
| 1.20 | 20.50 |
| 1.30 | 6.90 |
| 1.40 | 5.10 |
| 1.50 | 9.80 |
| 1.60 | 8.20 |
| 1.70 | 8.50 |
| 1.80 | 9.10 |
| 1.90 | 10.60 |
| 2.00 | 9.00 |
| 2.10 | 10.20 |
| 2.20 | 8.70 |
| 2.30 | 8.50 |
| 2.40 | 6.00 |
| 2.50 | 6.80 |
| 2.60 | 9.40 |
| 2.70 | 9.90 |
| 2.80 | 7.30 |
| 2.90 | 9.10 |
| 3.00 | 13.00 |
| 3.10 | 9.90 |
| 3.20 | 8.50 |
| 3.30 | 13.10 |
| 3.40 | 9.50 |
| 3.50 | 10.20 |
| 3.60 | 15.50 |
| 3.70 | 2.80 |
| 3.80 | 1.40 |
| 3.90 | 16.80 |
| 4.00 | 6.20 |
| 4.10 | 7.00 |
| 4.20 | 8.40 |
| 4.30 | 24.90 |
| 4.40 | 37.60 |
| 4.50 | 4.30 |
| 4.60 | 19.50 |
| 4.70 | 23.20 |
| 4.80 | 39.90 |
| 4.90 | 30.00 |
| 5.00 | 25.60 |
| 5.20 | 20.20 |
| 5.30 | 4.60 |
| 5.40 | 13.20 |
| 5.60 | 9.20 |
| 5.70 | 9.80 |
| 5.80 | 11.70 |
| 5.90 | 9.00 |
| 6.00 | 7.00 |
| 6.11 | 12.90 |