Ruddiman, William F; Farrell, John W (1996): Calcium carbonate content of sediment core V22-216 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.51230
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: 26.767000 * Longitude: -40.900000
Date/Time Start: 1966-06-02T00:00:00 * Date/Time End: 1966-06-02T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 5.60 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 | 86.77 |
| 0.10 | 88.24 |
| 0.20 | 84.76 |
| 0.30 | 81.41 |
| 0.40 | 81.97 |
| 0.50 | 83.70 |
| 0.60 | 76.66 |
| 0.70 | 80.17 |
| 0.80 | 82.60 |
| 0.90 | 82.21 |
| 1.00 | 84.91 |
| 1.10 | 87.08 |
| 1.20 | 88.17 |
| 1.30 | 85.29 |
| 1.40 | 85.00 |
| 1.50 | 83.09 |
| 1.60 | 87.28 |
| 1.70 | 80.09 |
| 1.70 | 78.04 |
| 1.80 | 86.92 |
| 1.90 | 93.78 |
| 1.90 | 92.13 |
| 2.00 | 88.89 |
| 2.10 | 85.74 |
| 2.20 | 85.20 |
| 2.30 | 81.10 |
| 2.40 | 84.42 |
| 2.50 | 85.96 |
| 2.60 | 83.45 |
| 2.70 | 81.71 |
| 2.80 | 85.19 |
| 2.80 | 82.62 |
| 2.90 | 81.91 |
| 3.00 | 82.97 |
| 3.10 | 84.72 |
| 3.20 | 83.56 |
| 3.30 | 87.52 |
| 3.40 | 86.92 |
| 3.50 | 88.28 |
| 3.60 | 89.71 |
| 3.70 | 88.28 |
| 3.80 | 85.68 |
| 3.90 | 91.26 |
| 4.00 | 93.30 |
| 4.10 | 88.34 |
| 4.20 | 86.84 |
| 4.30 | 91.93 |
| 4.40 | 87.03 |
| 4.50 | 93.53 |
| 4.60 | 87.57 |
| 4.70 | 91.53 |
| 4.80 | 89.20 |
| 4.90 | 87.85 |
| 5.00 | 89.11 |
| 5.10 | 90.51 |
| 5.20 | 87.39 |
| 5.30 | 90.74 |
| 5.40 | 86.32 |
| 5.50 | 85.17 |
| 5.60 | 84.13 |