Bralower, Timothy J; Kump, Lee R; Self-Trail, Jean; Robinson, Marci M; Lyons, Shelby; Babila, Tali L; Ballaron, Edward; Freeman, Katherine H; Hajek, Elizabeth; Rush, William; Zachos, James C (2018): Abundance of pyrite and siderite and nannofossil Whole Shield Index during the PETM at Wilson Lake [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.896838, In supplement to: Bralower, TJ et al. (2018): Evidence for shelf acidification during the onset of the Paleocene-Eocene Thermal Maximum. Paleoceanography and Paleoclimatology, https://doi.org/10.1029/2018PA003382
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Coverage:
Latitude: 39.655800 * Longitude: -75.042000
Minimum DEPTH, sediment/rock: 104.85 m * Maximum DEPTH, sediment/rock: 112.47 m
Event(s):
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Bralower, Timothy J | Geocode | |
2 | Coccoliths, whole shield index | WSI | % | Bralower, Timothy J | ||
3 | Coccoliths, partial dissolution | Cocco partial | % | Bralower, Timothy J | ||
4 | Pyrite, framboids | Py framb | # | Bralower, Timothy J | framboids in five slide traverses | |
5 | Minerals, altered | Min altered | % | Bralower, Timothy J | framboids that are oxidized | |
6 | Siderite | Sd | # | Bralower, Timothy J | grains in five slide traverses |
License:
Creative Commons Attribution 4.0 International (CC-BY-4.0)
Size:
156 data points
Data
1 Depth sed [m] | 2 WSI [%] | 3 Cocco partial [%] | 4 Py framb [#] | 5 Min altered [%] | 6 Sd [#] |
---|---|---|---|---|---|
104.85 | 71 | 29 | 152 | 15 | 19 |
105.16 | 80 | 20 | |||
105.46 | 76 | 24 | 47 | 1 | |
105.77 | 77 | 23 | 151 | ||
106.07 | 82 | 18 | 31 | 12 | |
106.38 | 83 | 17 | |||
106.68 | 76 | 24 | 141 | 19 | 30 |
106.98 | 83 | 17 | 17 | 33 | |
107.29 | 145 | ||||
107.38 | 44 | 18 | |||
107.44 | 75 | 25 | |||
107.59 | 12 | 212 | |||
107.69 | 40 | 122 | |||
107.75 | 71 | 29 | |||
107.78 | 24 | 17 | |||
107.90 | 34 | 28 | 12 | ||
107.98 | 72 | 28 | |||
108.20 | 38 | 20 | |||
108.51 | 78 | 22 | 27 | 54 | 22 |
108.81 | 85 | 15 | |||
108.91 | 71 | 29 | 14 | 3 | |
109.00 | 71 | 29 | |||
109.12 | 85 | 15 | 4 | 0 | |
109.21 | 75 | 25 | |||
109.23 | 93 | 7 | 94 | ||
109.30 | 5 | 2 | |||
109.33 | 54 | 46 | |||
109.42 | 35 | 65 | 960 | 18 | 9 |
109.49 | 85 | 15 | 645 | ||
109.51 | 0 | 0 | 140 | 95 | 2 |
109.58 | 53 | 47 | |||
109.61 | 0 | 0 | 153 | 44 | 2 |
109.67 | 5 | 2 | |||
109.73 | 0 | 0 | 227 | 4 | 5 |
109.76 | 5 | 0 | |||
109.82 | 5 | 1 | 113 | 35 | 4 |
109.84 | 68 | 32 | |||
109.91 | 48 | 2 | |||
109.95 | 60 | 40 | |||
110.03 | 10 | 11 | 638 | 51 | 3 |
110.06 | 43 | 57 | |||
110.12 | 38 | 62 | 89 | ||
110.22 | 54 | 46 | |||
110.34 | 33 | 67 | 10 | 1 | |
110.43 | 68 | 32 | |||
110.52 | 52 | 48 | |||
110.64 | 40 | 60 | |||
110.73 | 39 | 61 | 23 | 0 | |
110.95 | 9 | 91 | 330 | ||
111.25 | 10 | 90 | |||
111.56 | 3 | 97 | |||
111.86 | 17 | 83 | 196 | ||
112.17 | 31 | 69 | |||
112.47 | 31 | 69 | 28 |