Ruddiman, William F; Farrell, John W (1996): Calcium carbonate content of sediment core V21-34 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.51218
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: -5.367000 * Longitude: -93.370000
Date/Time Start: 1965-03-20T00:00:00 * Date/Time End: 1965-03-20T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 7.00 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:
71 data points
Data
1 Depth sed [m] | 2 CaCO3 [%] |
---|---|
0.00 | 85.48 |
0.10 | 87.64 |
0.20 | 91.83 |
0.30 | 92.10 |
0.40 | 94.95 |
0.50 | 87.94 |
0.60 | 90.74 |
0.70 | 93.81 |
0.80 | 92.54 |
0.90 | 93.19 |
1.00 | 93.10 |
1.10 | 95.06 |
1.20 | 93.47 |
1.30 | 91.43 |
1.40 | 93.23 |
1.50 | 90.43 |
1.60 | 93.08 |
1.70 | 88.93 |
1.80 | 91.79 |
1.90 | 93.87 |
2.00 | 92.40 |
2.10 | 95.80 |
2.20 | 91.45 |
2.30 | 89.92 |
2.40 | 93.66 |
2.50 | 93.19 |
2.60 | 91.67 |
2.70 | 90.91 |
2.80 | 92.25 |
2.90 | 91.48 |
3.00 | 91.78 |
3.10 | 91.42 |
3.20 | 94.41 |
3.30 | 94.37 |
3.40 | 94.60 |
3.50 | 93.04 |
3.60 | 94.48 |
3.70 | 90.91 |
3.80 | 92.66 |
3.90 | 93.79 |
4.00 | 91.24 |
4.10 | 92.50 |
4.20 | 92.74 |
4.30 | 91.50 |
4.40 | 92.05 |
4.50 | 94.71 |
4.60 | 91.42 |
4.70 | 91.72 |
4.80 | 95.17 |
4.90 | 95.67 |
5.00 | 96.33 |
5.10 | 95.54 |
5.20 | 95.95 |
5.30 | 97.08 |
5.40 | 96.10 |
5.50 | 97.86 |
5.60 | 95.13 |
5.70 | 96.67 |
5.80 | 97.83 |
5.90 | 96.37 |
6.00 | 99.22 |
6.10 | 97.41 |
6.20 | 97.70 |
6.30 | 97.61 |
6.40 | 95.78 |
6.50 | 98.32 |
6.60 | 97.48 |
6.70 | 97.86 |
6.80 | 98.81 |
6.90 | 96.35 |
7.00 | 99.41 |