Boyle, Edward A (1999): Cadmium/Calcium ratio of sediment core TR163-31 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.55544
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Boyle, Edward A; Keigwin, Lloyd D (1985): Comparison of Atlantic and Pacific paleochemical records for the last 215.000 years: changes in deep ocean circulation and chemical inventories. Earth and Planetary Science Letters, 76(1-2), 135-150, https://doi.org/10.1016/0012-821X(85)90154-2
Coverage:
Latitude: -3.616700 * Longitude: -83.966700
Minimum DEPTH, sediment/rock: 0.015 m * Maximum DEPTH, sediment/rock: 1.595 m
Event(s):
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Cadmium/Calcium ratio | Cd/Ca | mmol/mol | Boyle, Edward A | Graphite furnace atomic absorption spectrometer (GF-AAS) | Uvigerina spp. |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
53 data points
Data
1 Depth sed [m] | 2 Cd/Ca [mmol/mol] |
---|---|
0.015 | 0.000244 |
0.035 | 0.000229 |
0.065 | 0.000199 |
0.095 | 0.000223 |
0.135 | 0.000225 |
0.165 | 0.000216 |
0.195 | 0.000212 |
0.235 | 0.000221 |
0.255 | 0.000251 |
0.265 | 0.000238 |
0.295 | 0.000219 |
0.335 | 0.000202 |
0.365 | 0.000220 |
0.375 | 0.000225 |
0.395 | 0.000224 |
0.435 | 0.000214 |
0.465 | 0.000205 |
0.495 | 0.000191 |
0.535 | 0.000188 |
0.565 | 0.000197 |
0.595 | 0.000198 |
0.615 | 0.000197 |
0.635 | 0.000191 |
0.665 | 0.000173 |
0.695 | 0.000187 |
0.735 | 0.000181 |
0.765 | 0.000176 |
0.795 | 0.000201 |
0.835 | 0.000187 |
0.855 | 0.000191 |
0.865 | 0.000196 |
0.895 | 0.000206 |
0.935 | 0.000180 |
0.965 | 0.000209 |
0.995 | 0.000193 |
1.035 | 0.000181 |
1.065 | 0.000167 |
1.095 | 0.000177 |
1.135 | 0.000175 |
1.165 | 0.000160 |
1.195 | 0.000190 |
1.235 | 0.000197 |
1.265 | 0.000183 |
1.295 | 0.000204 |
1.335 | 0.000201 |
1.365 | 0.000188 |
1.395 | 0.000175 |
1.435 | 0.000188 |
1.455 | 0.000171 |
1.495 | 0.000182 |
1.535 | 0.000193 |
1.565 | 0.000171 |
1.595 | 0.000225 |