Ruddiman, William F; Farrell, John W (1996): Calcium carbonate content of sediment core V30-192 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.51359
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: 35.350000 * Longitude: -17.120000
Date/Time Start: 1973-11-04T00:00:00 * Date/Time End: 1973-11-04T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 5.40 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:
63 data points
Data
1 Depth sed [m] | 2 CaCO3 [%] |
---|---|
0.00 | 60.22 |
0.00 | 61.37 |
0.10 | 80.66 |
0.20 | 86.09 |
0.30 | 83.31 |
0.40 | 84.27 |
0.50 | 78.34 |
0.60 | 74.74 |
0.70 | 67.56 |
0.80 | 61.89 |
0.90 | 74.58 |
1.00 | 74.73 |
1.10 | 84.88 |
1.20 | 71.15 |
1.20 | 71.27 |
1.30 | 85.43 |
1.40 | 79.41 |
1.50 | 80.58 |
1.60 | 54.52 |
1.60 | 53.29 |
1.70 | 82.55 |
1.80 | 92.13 |
1.90 | 84.33 |
2.00 | 86.38 |
2.10 | 87.72 |
2.20 | 83.85 |
2.20 | 84.01 |
2.30 | 90.01 |
2.30 | 90.47 |
2.40 | 78.59 |
2.40 | 77.14 |
2.50 | 85.28 |
2.50 | 83.83 |
2.60 | 64.13 |
2.60 | 63.39 |
2.70 | 82.81 |
2.80 | 86.16 |
2.90 | 88.13 |
3.00 | 91.25 |
3.10 | 90.56 |
3.20 | 88.89 |
3.30 | 88.19 |
3.40 | 88.34 |
3.50 | 86.34 |
3.60 | 83.92 |
3.70 | 86.81 |
3.80 | 85.16 |
3.90 | 85.37 |
4.00 | 87.32 |
4.10 | 85.56 |
4.20 | 85.54 |
4.30 | 85.97 |
4.40 | 84.81 |
4.50 | 85.79 |
4.60 | 86.49 |
4.70 | 86.38 |
4.80 | 86.00 |
4.90 | 85.12 |
5.00 | 88.15 |
5.10 | 86.55 |
5.20 | 86.28 |
5.30 | 87.28 |
5.40 | 87.37 |