Ruddiman, William F; Farrell, John W (1996): Calcium carbonate content of sediment core V22-218 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.51232
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: 27.833000 * Longitude: -43.420000
Date/Time Start: 1966-06-03T00:00:00 * Date/Time End: 1966-06-03T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 5.80 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:
64 data points
Data
1 Depth sed [m] | 2 CaCO3 [%] |
---|---|
0.00 | 85.44 |
0.10 | 83.38 |
0.20 | 87.15 |
0.30 | 90.02 |
0.40 | 88.85 |
0.50 | 89.33 |
0.60 | 84.97 |
0.70 | 81.76 |
0.80 | 79.98 |
0.90 | 87.25 |
1.00 | 87.24 |
1.10 | 85.93 |
1.20 | 88.33 |
1.30 | 86.73 |
1.40 | 84.24 |
1.50 | 88.15 |
1.60 | 84.87 |
1.70 | 85.61 |
1.80 | 91.23 |
1.80 | 93.30 |
1.90 | 85.35 |
1.90 | 89.09 |
2.00 | 92.68 |
2.00 | 91.55 |
2.10 | 88.96 |
2.20 | 91.71 |
2.30 | 92.89 |
2.40 | 93.86 |
2.50 | 94.66 |
2.60 | 94.71 |
2.70 | 94.68 |
2.80 | 90.74 |
2.90 | 91.52 |
3.00 | 90.66 |
3.10 | 92.46 |
3.20 | 92.80 |
3.30 | 88.99 |
3.30 | 89.71 |
3.40 | 92.53 |
3.50 | 92.89 |
3.60 | 89.96 |
3.70 | 92.99 |
3.80 | 88.74 |
3.90 | 91.87 |
4.00 | 91.55 |
4.10 | 90.64 |
4.20 | 87.58 |
4.30 | 90.13 |
4.40 | 89.22 |
4.50 | 92.40 |
4.60 | 89.62 |
4.70 | 88.84 |
4.80 | 92.76 |
4.90 | 89.59 |
4.90 | 90.82 |
5.00 | 94.25 |
5.10 | 92.16 |
5.20 | 90.91 |
5.30 | 92.79 |
5.40 | 90.41 |
5.50 | 88.94 |
5.60 | 92.55 |
5.70 | 92.02 |
5.80 | 91.34 |