Ruddiman, William F; Farrell, John W (1996): Calcium carbonate content of sediment core V22-188 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.51223
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: 4.667000 * Longitude: -20.920000
Date/Time Start: 1966-05-19T00:00:00 * Date/Time End: 1966-05-19T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 9.80 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:
65 data points
Data
1 Depth sed [m] | 2 CaCO3 [%] |
---|---|
0.00 | 79.10 |
0.10 | 81.00 |
0.20 | 59.60 |
0.30 | 58.80 |
0.40 | 68.50 |
0.50 | 67.00 |
0.60 | 73.60 |
0.70 | 48.50 |
0.80 | 66.80 |
0.90 | 72.40 |
1.00 | 68.60 |
1.20 | 65.70 |
1.40 | 76.90 |
1.60 | 57.70 |
1.70 | 62.50 |
1.80 | 67.40 |
1.90 | 55.80 |
2.00 | 54.60 |
2.10 | 84.70 |
2.20 | 67.00 |
2.40 | 58.40 |
2.60 | 64.00 |
2.80 | 84.10 |
2.90 | 77.60 |
3.00 | 47.90 |
3.10 | 59.40 |
3.20 | 85.00 |
3.30 | 73.10 |
3.40 | 65.80 |
3.50 | 76.90 |
3.60 | 79.00 |
3.70 | 63.40 |
3.80 | 46.20 |
3.90 | 69.00 |
4.00 | 78.90 |
4.20 | 69.40 |
4.40 | 74.00 |
4.60 | 59.00 |
4.80 | 69.80 |
5.00 | 74.60 |
5.20 | 88.60 |
5.40 | 74.80 |
5.60 | 71.80 |
5.80 | 85.00 |
6.00 | 64.70 |
6.20 | 88.30 |
6.40 | 68.90 |
6.60 | 62.60 |
6.80 | 45.30 |
7.00 | 77.40 |
7.20 | 79.70 |
7.40 | 73.60 |
7.60 | 77.20 |
7.80 | 71.80 |
8.00 | 67.90 |
8.20 | 54.60 |
8.40 | 55.90 |
8.50 | 35.20 |
8.60 | 80.70 |
8.80 | 77.30 |
9.00 | 83.70 |
9.20 | 72.80 |
9.40 | 69.20 |
9.60 | 75.40 |
9.80 | 68.20 |