Hendrizan, Marfasran; Kuhnt, Wolfgang; Holbourn, Ann E (2017): CaCO3 content of sediment core GIK18517-2 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.880964, In: Hendrizan, M et al. (2017): High resolution reconstruction of hydrological changes over the last 14 kyr from sediment core GIK18517-2 [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.880971
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Published: 2017-09-25 • DOI registered: 2017-10-23
Related to:
Hendrizan, Marfasran; Kuhnt, Wolfgang; Holbourn, Ann E (2017): Variability of Indonesian Throughflow and Borneo Runoff During the Last 14 kyr. Paleoceanography, 32(10), 1054-1069, https://doi.org/10.1002/2016PA003030
Project(s):
Coverage:
Latitude: -1.536630 * Longitude: 117.562600
Date/Time Start: 2011-07-30T04:27:00 * Date/Time End: 2011-07-30T04:27:00
Minimum DEPTH, sediment/rock: 0.215 m * Maximum DEPTH, sediment/rock: 13.785 m
Event(s):
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Hendrizan, Marfasran | Geocode | |
| 2 | AGE | Age | ka BP | Hendrizan, Marfasran | Geocode | |
| 3 | Calcium carbonate | CaCO3 | % | Hendrizan, Marfasran | Carbonate bomb (Müller & Gastner, 1971) |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
28 data points
Data
| 1 Depth sed [m] | 2 Age [ka BP] | 3 CaCO3 [%] |
|---|---|---|
| 0.215 | 0.28034 | 10 |
| 0.715 | 0.92245 | 10 |
| 1.215 | 1.55080 | 10 |
| 1.715 | 2.16540 | 11 |
| 2.215 | 2.76620 | 11 |
| 2.715 | 3.35320 | 12 |
| 3.215 | 3.92650 | 13 |
| 3.715 | 4.48600 | 14 |
| 4.265 | 5.08560 | 14 |
| 4.765 | 5.61620 | 13 |
| 5.265 | 6.13150 | 15 |
| 5.765 | 6.62870 | 15 |
| 6.265 | 7.27150 | 15 |
| 6.765 | 8.07240 | 14 |
| 7.265 | 8.52340 | 13 |
| 7.765 | 8.90050 | 13 |
| 8.265 | 9.28910 | 13 |
| 8.765 | 9.72120 | 14 |
| 9.285 | 10.23700 | 15 |
| 9.785 | 10.82000 | 14 |
| 10.285 | 11.41500 | 13 |
| 10.785 | 11.79800 | 8 |
| 11.285 | 12.07600 | 7 |
| 11.785 | 12.33300 | 6 |
| 12.285 | 12.64000 | 7 |
| 12.785 | 13.06600 | 11 |
| 13.285 | 13.47600 | 9 |
| 13.785 | 13.86100 | 10 |