Ruddiman, William F; Farrell, John W (1996): Calcium carbonate content of sediment core V28-35 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.51331
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: 67.117000 * Longitude: -9.567000
Date/Time Start: 1970-08-10T00:00:00 * Date/Time End: 1970-08-10T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 6.60 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:
69 data points
Data
1 Depth sed [m] | 2 CaCO3 [%] |
---|---|
0.00 | 30.20 |
0.10 | 33.70 |
0.20 | 5.60 |
0.30 | 5.00 |
0.40 | 14.60 |
0.50 | 14.20 |
0.60 | 11.40 |
0.70 | 8.50 |
0.80 | 9.00 |
0.90 | 8.80 |
1.00 | 5.50 |
1.10 | 15.70 |
1.20 | 10.40 |
1.30 | 13.90 |
1.40 | 10.60 |
1.50 | 23.40 |
1.60 | 3.50 |
1.65 | 1.70 |
1.70 | 25.80 |
1.78 | 9.60 |
1.84 | 9.00 |
1.90 | 13.20 |
2.00 | 11.80 |
2.10 | 8.10 |
2.20 | 2.40 |
2.30 | 12.00 |
2.40 | 8.10 |
2.50 | 15.10 |
2.60 | 9.90 |
2.70 | 6.60 |
2.80 | 8.60 |
2.90 | 5.90 |
3.00 | 6.00 |
3.10 | 6.20 |
3.20 | 6.10 |
3.30 | 10.30 |
3.40 | 6.50 |
3.50 | 19.60 |
3.60 | 13.50 |
3.70 | 6.00 |
3.80 | 5.50 |
3.90 | 2.00 |
4.00 | 1.20 |
4.10 | 1.40 |
4.20 | 2.70 |
4.30 | 3.00 |
4.40 | 1.50 |
4.50 | 0.80 |
4.60 | 7.00 |
4.70 | 7.30 |
4.80 | 7.10 |
4.90 | 10.10 |
5.00 | 35.20 |
5.10 | 28.80 |
5.20 | 22.20 |
5.30 | 6.50 |
5.40 | 1.20 |
5.50 | 0.50 |
5.60 | 1.60 |
5.70 | 1.20 |
5.80 | 1.10 |
5.90 | 1.80 |
6.00 | 2.20 |
6.10 | 1.90 |
6.20 | 0.60 |
6.30 | 2.60 |
6.40 | 9.50 |
6.50 | 5.10 |
6.60 | 2.90 |