Brückner, Sylvia; Mackensen, Andreas (2008): (Table 3a) Paired δ¹³C differences between Globobulimina turgida and Melonis barleeanus of sediment core Alkor_159_225514 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.716157, In supplement to: Brückner, S; Mackensen, A (2008): Organic matter rain rates, oxygen availability, and vital effects from benthic foraminiferal d13C in the historic Skagerrak, North Sea. Marine Micropaleontology, 66(3-4), 192-207, https://doi.org/10.1016/j.marmicro.2007.09.002
Always quote citation above when using data! You can download the citation in several formats below.
Project(s):
Coverage:
Latitude: 57.840550 * Longitude: 8.709080
Date/Time Start: 2000-05-10T00:00:00 * Date/Time End: 2000-05-10T00:00:00
Minimum DEPTH, sediment/rock: 0.01 m * Maximum DEPTH, sediment/rock: 0.85 m
Event(s):
AL159_225514 * Latitude: 57.840550 * Longitude: 8.709080 * Date/Time: 2000-05-10T00:00:00 * Elevation: -420.0 m * Recovery: 4.05 m * Location: Skagerrak * Campaign: AL159 * Basis: Alkor (1990) * Method/Device: Gravity corer (GC)
Comment:
Project: Integrated Baltic Sea Environmental Study (IBSEN); funded by German Ministry of Education and Research (BMBF)
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Age | Age | a AD/CE | Mackensen, Andreas | based on core correlation with Core III KAL (Hass, 1996) | |
| 3 | Δδ13C | Δδ13C | ‰ PDB | Mackensen, Andreas | Calculated | Globobulimina turgida-Melonis barleeanus |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
50 data points
Data
| 1 Depth sed [m] | 2 Age [a AD/CE] | 3 Δδ13C [‰ PDB] |
|---|---|---|
| 0.01 | 1993 | 0.73 |
| 0.02 | 1986 | 0.43 |
| 0.03 | 1979 | 0.44 |
| 0.07 | 1951 | 0.25 |
| 0.08 | 1944 | 0.26 |
| 0.12 | 1917 | 0.01 |
| 0.13 | 1910 | 0.32 |
| 0.15 | 1896 | 0.49 |
| 0.18 | 1878 | 0.11 |
| 0.20 | 1869 | 0.36 |
| 0.23 | 1856 | -0.02 |
| 0.25 | 1848 | -0.03 |
| 0.28 | 1835 | 0.22 |
| 0.30 | 1827 | 0.18 |
| 0.33 | 1814 | 0.74 |
| 0.35 | 1805 | 0.02 |
| 0.40 | 1784 | 0.33 |
| 0.48 | 1750 | 0.39 |
| 0.50 | 1741 | 0.17 |
| 0.53 | 1728 | 0.40 |
| 0.55 | 1720 | 0.28 |
| 0.58 | 1707 | 0.25 |
| 0.75 | 1634 | 0.48 |
| 0.78 | 1622 | 0.18 |
| 0.85 | 1592 | -0.23 |