Ruddiman, William F; Farrell, John W (1996): Calcium carbonate content of sediment core V27-83 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.51295
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: 74.200000 * Longitude: -5.717000
Date/Time Start: 1969-09-02T00:00:00 * Date/Time End: 1969-09-02T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 5.70 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:
58 data points
Data
| 1 Depth sed [m] | 2 CaCO3 [%] |
|---|---|
| 0.00 | 20.90 |
| 0.10 | 22.80 |
| 0.20 | 8.50 |
| 0.30 | 5.70 |
| 0.40 | 6.70 |
| 0.50 | 7.40 |
| 0.60 | 7.30 |
| 0.70 | 11.90 |
| 0.80 | 9.60 |
| 0.90 | 12.80 |
| 1.00 | 1.30 |
| 1.10 | 5.40 |
| 1.20 | 3.90 |
| 1.30 | 5.40 |
| 1.40 | 10.40 |
| 1.50 | 5.90 |
| 1.60 | 5.30 |
| 1.70 | 5.40 |
| 1.80 | 2.60 |
| 1.90 | 1.80 |
| 2.00 | 5.20 |
| 2.10 | 8.20 |
| 2.20 | 2.60 |
| 2.30 | 3.60 |
| 2.40 | 5.80 |
| 2.50 | 7.30 |
| 2.60 | 6.50 |
| 2.70 | 6.20 |
| 2.80 | 5.00 |
| 2.90 | 7.70 |
| 3.00 | 5.20 |
| 3.10 | 7.30 |
| 3.20 | 7.80 |
| 3.30 | 6.30 |
| 3.40 | 12.50 |
| 3.50 | 6.40 |
| 3.60 | 1.70 |
| 3.70 | 1.00 |
| 3.80 | 2.60 |
| 3.90 | 0.40 |
| 4.00 | 0.80 |
| 4.10 | 2.80 |
| 4.20 | 14.20 |
| 4.30 | 2.20 |
| 4.40 | 11.90 |
| 4.50 | 10.80 |
| 4.60 | 3.80 |
| 4.70 | 12.40 |
| 4.80 | 1.70 |
| 4.90 | 7.80 |
| 5.00 | 7.20 |
| 5.10 | 9.00 |
| 5.20 | 2.20 |
| 5.30 | 3.80 |
| 5.40 | 3.20 |
| 5.50 | 2.80 |
| 5.60 | 6.30 |
| 5.70 | 3.20 |