Owens, Jeremy D; Lyons, Timothy W; Li, Xiaona N; MacLeod, Kenneth G; Gordon, Gwenyth; Kuypers, Marcel MM; Anbar, Ariel D; Kuhnt, Wolfgang; Severmann, Silke (2012): (Table S6) Geochemistry of Cenomanian-Turonian sediments from section Eastbourne [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.824950, In supplement to: Owens, JD et al. (2012): Iron isotope and trace metal records of iron cycling in the proto-North Atlantic during the Cenomanian-Turonian oceanic anoxic event (OAE-2). Paleoceanography, 27(3), PA3223, https://doi.org/10.1029/2012PA002328
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Coverage:
Latitude: 50.700000 * Longitude: 0.300000
Minimum HEIGHT above ground: 0.20 m * Maximum HEIGHT above ground: 18.90 m
Event(s):
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Sample code/label | Sample label | Owens, Jeremy D | |||
| 2 | HEIGHT above ground | Height | m | Geocode | ||
| 3 | Aluminium | Al | % | Owens, Jeremy D | ||
| 4 | Iron | Fe | % | Owens, Jeremy D | ||
| 5 | Molybdenum | Mo | % | Owens, Jeremy D | ||
| 6 | Iron/Aluminium ratio | Fe/Al | Owens, Jeremy D | |||
| 7 | δ56Fe | δ56Fe | ‰ | Owens, Jeremy D | ||
| 8 | δ56Fe, standard deviation | δ56Fe std dev | ± | Owens, Jeremy D | ||
| 9 | Replicates | Repl | # | Owens, Jeremy D |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
399 data points
Data
| 1 Sample label | 2 Height [m] | 3 Al [%] | 4 Fe [%] | 5 Mo [%] | 6 Fe/Al | 7 δ56Fe [‰] | 8 δ56Fe std dev [±] | 9 Repl [#] |
|---|---|---|---|---|---|---|---|---|
| WC +/-650 | 18.90 | 0.63 | 0.50 | 0.78 | ||||
| WC +/-600 | 18.40 | 0.16 | 0.12 | 0.72 | -0.13 | 0.00 | 2 | |
| WC +/-550 | 17.90 | 1.63 | 0.75 | 0.46 | ||||
| WC +/-500 | 17.40 | 1.55 | 0.71 | 0.46 | ||||
| WC +/-450 | 16.90 | 0.43 | 0.21 | 0.48 | ||||
| WC +/-400 | 16.40 | 0.71 | 0.38 | 0.53 | ||||
| WC +/-350 | 15.90 | 0.93 | 0.35 | 0.38 | 0.18 | 0.01 | 2 | |
| WC +/-300 | 15.40 | 0.76 | 0.30 | 0.40 | ||||
| WC +/-250 | 14.90 | 0.54 | 0.23 | 0.42 | ||||
| WC +/-200 | 14.40 | 0.57 | 0.26 | 0.45 | ||||
| WC +/-160 | 14.00 | 0.58 | 0.27 | 0.11 | 0.47 | |||
| WC +/-140 | 13.80 | 1.41 | 0.56 | 0.14 | 0.40 | |||
| WC +/-120 | 13.60 | 0.82 | 0.43 | 0.07 | 0.53 | 0.07 | 0.02 | 2 |
| PM +/-100 | 13.40 | 0.90 | 0.47 | 0.52 | ||||
| PM +/-80 | 13.20 | 0.80 | 0.47 | 0.14 | 0.58 | |||
| PM +/-60 | 13.00 | 0.72 | 0.45 | 0.62 | ||||
| PM +/-40 | 12.80 | 2.91 | 1.36 | 0.47 | 0.29 | 0.02 | 2 | |
| PM +/-20 | 12.60 | 0.76 | 0.42 | 0.55 | ||||
| PM+640 | 12.40 | 0.65 | 0.43 | 0.67 | ||||
| PM+620 | 12.20 | 2.05 | 1.03 | 0.50 | 0.04 | 0.01 | 2 | |
| PM+600 | 12.00 | 1.68 | 0.88 | 0.53 | ||||
| PM+580 | 11.80 | 1.76 | 0.91 | 0.52 | ||||
| PM+560 | 11.60 | 1.57 | 0.73 | 0.47 | 0.11 | 0.05 | 2 | |
| PM+540 | 11.40 | 1.72 | 0.79 | 0.46 | ||||
| PM+520 | 11.20 | 1.57 | 0.69 | 0.12 | 0.44 | |||
| PM+500 | 11.00 | 1.42 | 0.63 | 0.44 | ||||
| PM+480 | 10.80 | 0.87 | 0.44 | 0.50 | -0.03 | 0.03 | 2 | |
| PM+460 | 10.60 | 0.83 | 0.41 | 0.49 | ||||
| PM+440 | 10.40 | 1.16 | 0.52 | 0.45 | ||||
| PM+420 | 10.20 | 1.02 | 0.48 | 0.47 | ||||
| PM+400 | 10.00 | 1.11 | 0.50 | 0.00 | 0.46 | |||
| PM+380 | 9.80 | 1.12 | 0.50 | 0.45 | ||||
| PM+360 | 9.60 | 1.39 | 0.64 | 0.46 | 0.07 | 0.08 | 2 | |
| PM+340 | 9.40 | 1.44 | 0.65 | 0.45 | ||||
| PM+320 | 9.20 | 2.11 | 1.01 | 0.48 | 0.10 | 0.05 | 2 | |
| PM+300 | 9.00 | 2.16 | 0.92 | 0.43 | ||||
| PM+280 | 8.80 | 2.27 | 0.96 | 0.43 | ||||
| PM+260 | 8.60 | 1.60 | 0.70 | 0.44 | 0.08 | 0.08 | 2 | |
| PM+240 | 8.40 | 1.87 | 0.72 | 0.39 | ||||
| PM+220 | 8.20 | 1.61 | 0.62 | 0.38 | ||||
| PM+200 | 8.00 | 1.69 | 0.62 | 0.37 | ||||
| PM+180 | 7.80 | 1.81 | 0.78 | 0.43 | ||||
| PM+160 | 7.60 | 1.89 | 0.74 | 0.37 | 0.39 | |||
| PM+140 | 7.40 | 1.92 | 0.73 | 0.38 | 0.09 | 0.02 | 2 | |
| PM+120 | 7.20 | 1.79 | 0.71 | 0.40 | ||||
| PM+100 | 7.00 | 2.11 | 0.82 | 0.39 | ||||
| PM+80 | 6.80 | 2.03 | 0.80 | 0.07 | 0.40 | |||
| PM+60 | 6.60 | 1.74 | 0.65 | 0.37 | 0.12 | 0.00 | 2 | |
| PM+40 | 6.40 | 1.52 | 0.59 | 0.39 | ||||
| PM+20 | 6.20 | 2.44 | 0.88 | 0.36 | ||||
| GC-0 | 6.00 | 1.03 | 0.41 | 0.38 | 0.39 | |||
| GC-20 | 5.80 | 0.87 | 0.35 | 0.27 | 0.40 | |||
| GC-40 | 5.60 | 0.72 | 0.32 | 0.45 | -0.02 | 0.04 | 2 | |
| GC-60 | 5.40 | 0.63 | 0.28 | 0.44 | ||||
| GC-80 | 5.20 | 0.71 | 0.31 | 0.85 | 0.43 | |||
| GC-100 | 5.00 | 0.64 | 0.29 | 0.45 | ||||
| GC-120 | 4.80 | 0.45 | 0.22 | 0.16 | 0.48 | |||
| GC-140 | 4.60 | 0.41 | 0.20 | 0.49 | ||||
| GC-160 | 4.40 | 0.50 | 0.23 | 0.49 | 0.46 | 0.05 | 0.07 | 3 |
| GC-180 | 4.20 | 0.44 | 0.22 | 0.49 | ||||
| GC-200 | 4.00 | 0.56 | 0.24 | 0.44 | ||||
| GC-220 | 3.80 | 0.46 | 0.22 | 0.47 | ||||
| GC-240 | 3.60 | 0.67 | 0.29 | 0.43 | 0.13 | 0.03 | 2 | |
| GC-260 | 3.40 | 1.06 | 0.41 | 0.39 | ||||
| GC-280 | 3.20 | 1.11 | 0.43 | 0.20 | 0.39 | |||
| GC-300 | 3.00 | 0.44 | 0.22 | 0.50 | ||||
| GC-320 | 2.80 | 0.45 | 0.23 | 0.51 | ||||
| GC-340 | 2.60 | 0.43 | 0.22 | 0.07 | 0.50 | 0.00 | 0.01 | 2 |
| GC-360 | 2.40 | 0.52 | 0.25 | 0.48 | ||||
| GC-380 | 2.20 | 0.80 | 0.36 | 0.08 | 0.45 | |||
| GC-400 | 2.00 | 0.83 | 0.34 | 0.41 | ||||
| GC-410 | 1.90 | 0.66 | 0.29 | 0.41 | 0.43 | |||
| GC 420 | 1.80 | 0.75 | 0.31 | 0.41 | ||||
| GC-440 | 1.60 | 0.76 | 0.30 | 0.16 | 0.39 | |||
| GC-480 | 1.40 | 0.51 | 0.26 | 0.40 | 0.51 | |||
| GC-500 | 1.20 | 0.77 | 0.34 | 0.26 | 0.44 | 0.11 | 0.04 | 3 |
| GC-520 | 0.90 | 1.23 | 0.50 | 0.40 | ||||
| GC-540 | 0.80 | 1.25 | 0.46 | 0.37 | 0.22 | 0.06 | 2 | |
| GC-560 | 0.60 | 0.85 | 0.35 | 0.41 | ||||
| GC-580 | 0.40 | 0.85 | 0.36 | 0.06 | 0.43 | |||
| GC-600 | 0.20 | 0.52 | 0.26 | 0.49 |