Fagel, Nathalie; Mattielli, Nadine (2011): (Table S2) Mineral composition of composite sediment core HU91-045-080 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.829685, In supplement to: Fagel, N; Mattielli, N (2011): Holocene evolution of deep circulation in the northern North Atlantic traced by Sm, Nd and Pb isotopes and bulk sediment mineralogy. Paleoceanography, 26(4), PA4220, https://doi.org/10.1029/2011PA002168
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Coverage:
Latitude: 53.056670 * Longitude: -33.529670
Minimum DEPTH, sediment/rock: 0.010 m * Maximum DEPTH, sediment/rock: 2.480 m
Event(s):
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Event label | Event | ||||
2 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
3 | Age, dated | Age dated | ka | Fagel, Nathalie | Age, 14C AMS | |
4 | Age, dated standard deviation | Age dated std dev | ± | Fagel, Nathalie | Age, 14C AMS | |
5 | AGE | Age | ka BP | Geocode | ||
6 | Clay minerals | Clay min | % | Fagel, Nathalie | X-ray diffraction (XRD) | |
7 | Quartz | Qz | % | Fagel, Nathalie | X-ray diffraction (XRD) | |
8 | Kalifeldspar | Kfs | % | Fagel, Nathalie | X-ray diffraction (XRD) | |
9 | Plagioclase | Pl | % | Fagel, Nathalie | X-ray diffraction (XRD) | |
10 | Calcite | Cal | % | Fagel, Nathalie | X-ray diffraction (XRD) | |
11 | Amphibole | Amp | % | Fagel, Nathalie | X-ray diffraction (XRD) | |
12 | Pyroxene | Pyrox | % | Fagel, Nathalie | X-ray diffraction (XRD) |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
259 data points
Data
1 Event | 2 Depth sed [m] | 3 Age dated [ka] | 4 Age dated std dev [±] | 5 Age [ka BP] | 6 Clay min [%] | 7 Qz [%] | 8 Kfs [%] | 9 Pl [%] | 10 Cal [%] | 11 Amp [%] | 12 Pyrox [%] |
---|---|---|---|---|---|---|---|---|---|---|---|
HU91-045-080TWC | 0.115 | 1.245 | 0.05 | 0.8 | 14 | 1 | 4 | 3 | 72 | 1 | 4 |
HU91-045-080TWC | 0.200 | 1.4 | 15 | 1 | 5 | 3 | 71 | 1 | 4 | ||
HU91-045-080TWC | 0.290 | 2.0 | 12 | 1 | 4 | 3 | 74 | 0 | 5 | ||
HU91-045-080TWC | 0.385 | 2.6 | 11 | 2 | 4 | 3 | 76 | 0 | 5 | ||
HU91-045-080TWC | 0.480 | 3.3 | 10 | 1 | 5 | 3 | 77 | 0 | 3 | ||
HU91-045-080TWC | 0.570 | 3.9 | 13 | 1 | 4 | 3 | 72 | 0 | 6 | ||
HU91-045-080TWC | 0.660 | 4.5 | 13 | 1 | 5 | 3 | 71 | 0 | 7 | ||
HU91-045-080TWC | 0.755 | 5.1 | 9 | 2 | 3 | 3 | 78 | 0 | 5 | ||
HU91-045-080TWC | 0.850 | 5.8 | 7 | 2 | 4 | 4 | 78 | 0 | 6 | ||
HU91-45-080P | 0.010 | 4.990 | 0.07 | 5.3 | 14 | 2 | 4 | 3 | 73 | 0 | 5 |
HU91-45-080P | 0.095 | 5.7 | 15 | 3 | 5 | 5 | 67 | 0 | 5 | ||
HU91-45-080P | 0.180 | 6.2 | 21 | 4 | 5 | 5 | 59 | 0 | 7 | ||
HU91-45-080P | 0.275 | 6.7 | 21 | 4 | 4 | 4 | 61 | 0 | 5 | ||
HU91-45-080P | 0.365 | 7.1 | 22 | 4 | 4 | 5 | 58 | 0 | 7 | ||
HU91-45-080P | 0.460 | 7.6 | 21 | 4 | 6 | 4 | 59 | 0 | 6 | ||
HU91-45-080P | 0.530 | 8.0 | 18 | 4 | 5 | 5 | 61 | 0 | 6 | ||
HU91-45-080P | 0.640 | 8.5 | 19 | 5 | 4 | 6 | 59 | 0 | 8 | ||
HU91-45-080P | 0.760 | 9.1 | 20 | 5 | 4 | 5 | 61 | 0 | 6 | ||
HU91-45-080P | 0.855 | 8.985 | 0.05 | 9.6 | 22 | 6 | 4 | 6 | 56 | 0 | 7 |
HU91-45-080P | 0.940 | 9.8 | 21 | 5 | 6 | 6 | 54 | 0 | 8 | ||
HU91-45-080P | 1.035 | 10.0 | 25 | 5 | 5 | 5 | 55 | 0 | 6 | ||
HU91-45-080P | 1.130 | 10.2 | 25 | 7 | 5 | 5 | 53 | 0 | 6 | ||
HU91-45-080P | 1.155 | 9.570 | 0.10 | ||||||||
HU91-45-080P | 1.220 | 10.5 | 24 | 7 | 6 | 6 | 52 | 0 | 6 | ||
HU91-45-080P | 1.310 | 10.7 | 28 | 6 | 6 | 6 | 48 | 0 | 6 | ||
HU91-45-080P | 1.400 | 11.0 | 28 | 7 | 6 | 5 | 46 | 0 | 7 | ||
HU91-45-080P | 1.490 | 11.2 | 26 | 8 | 6 | 6 | 47 | 0 | 7 | ||
HU91-45-080P | 1.590 | 11.5 | 26 | 8 | 6 | 7 | 47 | 0 | 6 | ||
HU91-45-080P | 1.680 | 11.8 | 37 | 12 | 10 | 8 | 32 | 2 | 0 | ||
HU91-45-080P | 1.780 | 10.750 | 0.10 | 12.1 | 36 | 11 | 7 | 8 | 28 | 1 | 9 |
HU91-45-080P | 1.880 | 12.5 | 36 | 11 | 9 | 8 | 27 | 0 | 8 | ||
HU91-45-080P | 1.980 | 12.9 | 54 | 7 | 17 | 7 | 8 | 0 | 7 | ||
HU91-45-080P | 2.180 | 12.210 | 0.09 | 13.7 | 27 | 19 | 8 | 10 | 25 | 5 | 5 |
HU91-45-080P | 2.240 | 14.4 | 30 | 11 | 5 | 8 | 38 | 1 | 7 | ||
HU91-45-080P | 2.380 | 16.0 | 36 | 13 | 11 | 8 | 24 | 2 | 6 | ||
HU91-45-080P | 2.480 | 14.880 | 0.13 | 17.2 | 29 | 20 | 9 | 11 | 23 | 1 | 6 |