Brückner, Sylvia; Mackensen, Andreas (2008): (Table 3b) Paired δ¹³C differences between various benthic foraminifera of sediment core Alkor_159_225510 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.716158, 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
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Project(s):
Coverage:
Latitude: 58.042220 * Longitude: 9.621440
Date/Time Start: 2000-05-10T00:00:00 * Date/Time End: 2000-05-10T00:00:00
Minimum DEPTH, sediment/rock: 0.10 m * Maximum DEPTH, sediment/rock: 5.29 m
Event(s):
AL159_225510 * Latitude: 58.042220 * Longitude: 9.621440 * Date/Time: 2000-05-10T00:00:00 * Elevation: -285.0 m * Recovery: 5.44 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 | Age model in radiocarbon 14C ages | |
| 3 | Δδ13C | Δδ13C | ‰ PDB | Mackensen, Andreas | Calculated | Globobulimina turgida-Cassidulina laevigata |
| 4 | Δδ13C | Δδ13C | ‰ PDB | Mackensen, Andreas | Calculated | Globobulimina turgida-Hyalinea balthica |
| 5 | Δδ13C | Δδ13C | ‰ PDB | Mackensen, Andreas | Calculated | Globobulimina turgida-Melonis zaandami |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
95 data points
Data
| 1 Depth sed [m] | 2 Age [a AD/CE] (Age model in radiocarbon 14C ...) | 3 Δδ13C [‰ PDB] (Globobulimina turgida-Cassidu...) | 4 Δδ13C [‰ PDB] (Globobulimina turgida-Hyaline...) | 5 Δδ13C [‰ PDB] (Globobulimina turgida-Melonis...) |
|---|---|---|---|---|
| 0.10 | 1998 | 1.01 | ||
| 0.20 | 1996 | 0.76 | -0.33 | |
| 0.30 | 1994 | 0.11 | ||
| 0.50 | 1990 | 0.45 | 1.17 | -0.15 |
| 0.60 | 1988 | 0.62 | 1.16 | 0.17 |
| 0.70 | 1986 | 0.32 | 0.88 | -0.17 |
| 0.80 | 1985 | 0.46 | 1.27 | -0.01 |
| 0.90 | 1983 | 0.78 | 1.13 | 0.14 |
| 1.10 | 1979 | 0.37 | 0.97 | |
| 1.20 | 1977 | 0.64 | 1.42 | |
| 1.30 | 1975 | 0.20 | ||
| 1.40 | 1973 | 0.54 | 0.85 | |
| 1.50 | 1971 | 0.55 | 1.33 | |
| 1.60 | 1969 | 0.15 | ||
| 1.70 | 1967 | 0.69 | ||
| 1.80 | 1965 | 0.27 | ||
| 1.90 | 1963 | 0.19 | ||
| 2.20 | 1927 | -0.04 | 0.64 | -0.20 |
| 2.30 | 1914 | 1.25 | ||
| 2.40 | 1901 | 1.01 | ||
| 2.70 | 1863 | 0.49 | 1.27 | |
| 2.80 | 1851 | 0.26 | ||
| 2.90 | 1838 | 0.49 | ||
| 3.00 | 1825 | 0.13 | ||
| 3.10 | 1813 | 0.09 | -0.09 | |
| 3.20 | 1800 | 0.31 | 0.59 | |
| 3.30 | 1787 | 0.21 | 0.89 | |
| 3.50 | 1762 | 0.17 | ||
| 3.70 | 1737 | 0.10 | ||
| 3.80 | 1724 | 0.07 | ||
| 3.90 | 1711 | 0.20 | ||
| 4.00 | 1699 | 0.22 | ||
| 4.10 | 1686 | 0.12 | ||
| 4.68 | 1612 | 0.35 | ||
| 4.78 | 1600 | 0.22 | ||
| 5.19 | 1548 | 0.26 | ||
| 5.29 | 1535 | -0.09 |