Filipsson, Helena L; Nordberg, Kjell (2010): δ¹³C of Cassidulina laevigata in sediment core Skagerrak01_GA113-2Aa from the Gullmar Fjord on the west coast of Sweden [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.773806, In supplement to: Filipsson, HL; Nordberg, K (2010): Variations in organic carbon flux and stagnation periods during the last 2400 years in a Skagerrak fjord basin, inferred from benthic foraminiferal d13C. In: Howe, JA; Austin, WEN; Forwick, M; Paetzel, M (eds.) Fjord Systems and Archives. Geological Society, London, Special Publications, 344, 261-270, https://doi.org/10.1144/SP344.18
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Coverage:
Latitude: 58.292800 * Longitude: 11.384300
Date/Time Start: 2001-01-01T00:00:00 * Date/Time End: 2001-01-01T00:00:00
Minimum DEPTH, sediment/rock: 0.050 m * Maximum DEPTH, sediment/rock: 0.595 m
Event(s):
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode – mbsf | ||
2 | Cassidulina laevigata, δ13C | C. laevigata δ13C | ‰ PDB | Filipsson, Helena L | Isotope ratio mass spectrometry | # = outlier |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
48 data points
Data
1 Depth sed [m] | 2 C. laevigata δ13C [‰ PDB] |
---|---|
0.050 | -1.08 |
0.070 | -1.04 |
0.090 | -1.19 |
0.105 | -1.12 |
0.115 | -1.32 |
0.123 | -1.22 |
0.135 | #-1.55 |
0.145 | -1.26 |
0.155 | -0.95 |
0.165 | -0.90 |
0.175 | -0.93 |
0.185 | -0.97 |
0.195 | -0.75 |
0.205 | #-1.89 |
0.220 | -0.64 |
0.235 | -0.69 |
0.245 | -0.62 |
0.260 | -0.57 |
0.275 | -0.52 |
0.285 | -0.59 |
0.295 | -0.58 |
0.305 | -0.43 |
0.315 | -0.40 |
0.325 | -0.54 |
0.335 | -0.57 |
0.345 | -0.44 |
0.355 | -0.58 |
0.365 | -0.71 |
0.375 | -0.56 |
0.385 | -0.69 |
0.395 | -0.68 |
0.405 | -0.42 |
0.420 | -0.65 |
0.435 | -0.66 |
0.445 | -0.65 |
0.455 | -0.73 |
0.465 | -0.60 |
0.475 | -0.62 |
0.485 | -0.59 |
0.495 | -0.60 |
0.505 | -0.51 |
0.520 | -0.57 |
0.535 | -0.50 |
0.550 | -0.35 |
0.565 | -0.57 |
0.575 | -0.50 |
0.585 | -0.43 |
0.595 | -0.51 |