Pérez-Asensio, José N; Frigola, Jaime; Pena, Leopoldo D; Sierro, Francisco Javier; Reguera, Maria Isabel; Rodríguez-Tovar, Francisco Javier; Dorador, Javier; Asioli, Alessandra; Kuhlmann, Jannis; Huhn, Katrin; Cacho, Isabel (2020): Sedimentation rate of sediment core MD95-2043 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.910804, In supplement to: Pérez-Asensio, JN et al. (2020): Changes in western Mediterranean thermohaline circulation in association with a deglacial Organic Rich Layer formation in the Alboran Sea. Quaternary Science Reviews, 228, 106075, https://doi.org/10.1016/j.quascirev.2019.106075
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Published: 2020-01-14 • DOI registered: 2020-07-10
Coverage:
Latitude: 36.143333 * Longitude: -2.621167
Date/Time Start: 1995-07-09T00:00:00 * Date/Time End: 1995-07-09T00:00:00
Minimum Elevation: -1841.0 m * Maximum Elevation: -1841.0 m
Event(s):
MD95-2043 (MD952043) * Latitude: 36.143333 * Longitude: -2.621167 * Date/Time: 1995-07-09T00:00:00 * Elevation: -1841.0 m * Recovery: 37 m * Location: Alboran Sea * Campaign: MD101 (IMAGES I) * Basis: Marion Dufresne (1995) * Method/Device: Calypso Corer (CALYPSO) * Comment: XXV Sections, OK; liner exploded in section VIII
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | AGE | Age | ka BP | Pérez-Asensio, José N | Geocode | |
| 2 | Sedimentation rate | SR | cm/ka | Pérez-Asensio, José N | Calculated |
License:
Creative Commons Attribution 4.0 International (CC-BY-4.0)
Size:
32 data points
Data
| 1 Age [ka BP] | 2 SR [cm/ka] |
|---|---|
| 1.5400 | 27.13 |
| 3.0100 | 27.13 |
| 3.0100 | 30.65 |
| 4.3800 | 30.65 |
| 4.3800 | 49.34 |
| 6.0400 | 49.34 |
| 6.0400 | 45.13 |
| 7.3700 | 45.13 |
| 7.3700 | 34.85 |
| 9.1000 | 34.85 |
| 9.1000 | 72.62 |
| 9.7800 | 72.62 |
| 9.7800 | 64.49 |
| 10.8700 | 64.49 |
| 10.8700 | 89.96 |
| 11.6400 | 89.96 |
| 11.6400 | 67.93 |
| 12.0000 | 67.93 |
| 12.0000 | 70.96 |
| 13.0800 | 70.96 |
| 13.0800 | 17.83 |
| 13.4700 | 17.83 |
| 13.4700 | 74.49 |
| 14.6400 | 74.49 |
| 14.6400 | 97.56 |
| 14.9000 | 97.56 |
| 14.9000 | 29.10 |
| 16.6200 | 29.10 |
| 16.6200 | 35.20 |
| 17.8700 | 35.20 |
| 17.8700 | 17.26 |
| 21.1200 | 17.26 |