Ruddiman, William F; Farrell, John W (1996): Calcium carbonate content of sediment core V27-84 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.51296
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: 68.633000 * Longitude: -1.600000
Date/Time Start: 1969-09-04T00:00:00 * Date/Time End: 1969-09-04T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 7.09 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 | 53.10 |
0.10 | 56.30 |
0.20 | 43.00 |
0.30 | 11.10 |
0.40 | 7.50 |
0.50 | 10.10 |
0.60 | 9.50 |
0.70 | 10.10 |
0.80 | 10.70 |
0.90 | 11.90 |
1.00 | 11.30 |
1.10 | 10.70 |
1.20 | 8.90 |
1.30 | 2.80 |
1.40 | 10.60 |
1.50 | 8.00 |
1.60 | 7.30 |
1.70 | 3.30 |
1.80 | 5.60 |
1.90 | 8.50 |
2.00 | 12.80 |
2.10 | 6.40 |
2.20 | 13.40 |
2.30 | 6.00 |
2.40 | 1.30 |
2.50 | 1.10 |
2.60 | 0.70 |
2.70 | 1.30 |
2.80 | 2.90 |
2.90 | 2.50 |
3.00 | 4.50 |
3.10 | 10.20 |
3.20 | 5.80 |
3.30 | 2.60 |
3.40 | 3.00 |
3.50 | 1.20 |
3.60 | 1.00 |
3.70 | 11.60 |
3.80 | 9.70 |
3.90 | 1.20 |
4.00 | 1.70 |
4.10 | 0.50 |
4.20 | 0.90 |
4.30 | 1.70 |
4.40 | 7.30 |
4.50 | 13.90 |
4.70 | 0.80 |
4.80 | 11.90 |
4.90 | 8.60 |
5.00 | 0.90 |
5.10 | 6.40 |
5.20 | 1.80 |
5.30 | 0.70 |
5.40 | 2.10 |
5.50 | 5.40 |
5.60 | 1.00 |
5.70 | 1.20 |
5.80 | 6.70 |
5.90 | 1.80 |
6.00 | 1.10 |
6.10 | 1.20 |
6.20 | 0.60 |
6.30 | 1.50 |
6.40 | 1.10 |
6.50 | 1.40 |
6.60 | 1.60 |
6.70 | 1.10 |
6.80 | 0.90 |
6.90 | 1.00 |
7.00 | 2.00 |
7.09 | 0.80 |