Ruddiman, William F; Farrell, John W (1996): Calcium carbonate content of sediment core V27-239 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.51277
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: -7.833000 * Longitude: -1.517000
Date/Time Start: 1970-03-23T00:00:00 * Date/Time End: 1970-03-23T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 6.00 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:
61 data points
Data
1 Depth sed [m] | 2 CaCO3 [%] |
---|---|
0.00 | 91.82 |
0.10 | 82.28 |
0.20 | 83.44 |
0.30 | 82.75 |
0.40 | 84.87 |
0.50 | 88.54 |
0.60 | 85.42 |
0.70 | 88.02 |
0.80 | 89.09 |
0.90 | 84.99 |
1.00 | 82.23 |
1.10 | 78.09 |
1.20 | 84.38 |
1.30 | 86.15 |
1.40 | 81.64 |
1.50 | 81.11 |
1.60 | 93.45 |
1.70 | 85.95 |
1.80 | 80.39 |
1.90 | 86.21 |
2.00 | 88.64 |
2.10 | 85.88 |
2.20 | 77.11 |
2.30 | 77.79 |
2.40 | 82.11 |
2.50 | 89.52 |
2.60 | 72.44 |
2.70 | 73.52 |
2.80 | 72.13 |
2.90 | 74.88 |
3.00 | 84.60 |
3.10 | 86.44 |
3.20 | 68.95 |
3.30 | 76.78 |
3.40 | 89.60 |
3.50 | 94.37 |
3.60 | 90.45 |
3.70 | 87.80 |
3.80 | 90.68 |
3.90 | 92.41 |
4.00 | 92.35 |
4.10 | 85.39 |
4.20 | 87.00 |
4.30 | 85.97 |
4.40 | 81.83 |
4.50 | 84.91 |
4.60 | 83.53 |
4.70 | 84.69 |
4.80 | 80.60 |
4.90 | 83.88 |
5.00 | 85.72 |
5.10 | 80.16 |
5.20 | 90.31 |
5.30 | 86.53 |
5.40 | 86.73 |
5.50 | 84.57 |
5.60 | 84.47 |
5.70 | 82.54 |
5.80 | 74.96 |
5.90 | 81.73 |
6.00 | 89.16 |