Ruddiman, William F; Farrell, John W (1996): Calcium carbonate content of sediment core V29-26 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.51353
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: 5.083000 * Longitude: 73.800000
Date/Time Start: 1971-12-20T00:00:00 * Date/Time End: 1971-12-20T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 6.00 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:
63 data points
Data
1 Depth sed [m] | 2 CaCO3 [%] |
---|---|
0.00 | 80.16 |
0.10 | 79.70 |
0.20 | 80.79 |
0.30 | 81.46 |
0.40 | 79.88 |
0.50 | 79.52 |
0.60 | 72.29 |
0.70 | 73.26 |
0.80 | 70.44 |
0.90 | 66.42 |
1.00 | 65.61 |
1.10 | 65.40 |
1.20 | 64.79 |
1.30 | 66.48 |
1.40 | 63.17 |
1.50 | 67.05 |
1.60 | 68.62 |
1.70 | 66.85 |
1.80 | 69.11 |
1.90 | 70.61 |
2.00 | 67.94 |
2.10 | 72.05 |
2.20 | 70.45 |
2.30 | 62.79 |
2.40 | 60.55 |
2.50 | 57.94 |
2.60 | 54.77 |
2.70 | 69.00 |
2.80 | 70.09 |
2.90 | 78.29 |
3.00 | 72.05 |
3.10 | 65.83 |
3.10 | 65.19 |
3.20 | 78.00 |
3.20 | 81.35 |
3.30 | 73.67 |
3.40 | 76.39 |
3.50 | 75.72 |
3.60 | 75.09 |
3.70 | 72.12 |
3.80 | 75.79 |
3.90 | 75.90 |
4.00 | 77.28 |
4.10 | 78.49 |
4.20 | 73.58 |
4.30 | 71.07 |
4.40 | 67.47 |
4.50 | 67.79 |
4.60 | 67.55 |
4.70 | 68.19 |
4.80 | 66.15 |
4.90 | 61.49 |
5.00 | 66.22 |
5.10 | 66.33 |
5.20 | 65.20 |
5.30 | 68.83 |
5.40 | 70.59 |
5.50 | 68.68 |
5.60 | 65.13 |
5.70 | 63.53 |
5.80 | 66.20 |
5.90 | 75.43 |
6.00 | 75.72 |