Walliser, Eric Otto; Lohmann, Gerrit; Niezgodzki, Igor; Schöne, Bernd R (2018): Growth increment width measurement and SGIshell data, Stadecken Formation, Mainz Basin, late Rupelian (MB-Sph-8) [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.884942, In supplement to: Walliser, EO et al. (2017): Inter-annual climate variability in Europe during the Oligocene icehouse. Palaeogeography, Palaeoclimatology, Palaeoecology, 475, 140-153, https://doi.org/10.1016/j.palaeo.2017.03.020
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Coverage:
Latitude: 49.812880 * Longitude: 8.142220
Event(s):
Comment:
SGI=standardized growth indices.
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Number of years | Years | a | Walliser, Eric Otto | Ontogenetic year | |
| 2 | Glycymeris planicostalis, growth increment width | G. planicostalis growth | mm | Walliser, Eric Otto | ||
| 3 | Growth index | phi ´ | Walliser, Eric Otto | SGI |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
138 data points
Data
| 1 Years [a] | 2 G. planicostalis growth [mm] | 3 phi ´ |
|---|---|---|
| 10 | 0.486 | -0.601 |
| 11 | 0.354 | -1.189 |
| 12 | 0.328 | -0.232 |
| 13 | 0.321 | 1.302 |
| 14 | 0.218 | -0.011 |
| 15 | 0.153 | -1.000 |
| 16 | 0.170 | 1.058 |
| 17 | 0.107 | -1.279 |
| 18 | 0.131 | 0.506 |
| 19 | 0.097 | -1.421 |
| 20 | 0.166 | 2.502 |
| 21 | 0.117 | -0.502 |
| 22 | 0.124 | -0.062 |
| 23 | 0.119 | -0.294 |
| 24 | 0.145 | 1.438 |
| 25 | 0.124 | 0.590 |
| 26 | 0.093 | -1.071 |
| 27 | 0.094 | -0.873 |
| 28 | 0.083 | -1.741 |
| 29 | 0.120 | 0.214 |
| 30 | 0.160 | 2.169 |
| 31 | 0.128 | 0.208 |
| 32 | 0.132 | 0.694 |
| 33 | 0.091 | -1.564 |
| 34 | 0.109 | -0.149 |
| 35 | 0.114 | 0.305 |
| 36 | 0.108 | -0.085 |
| 37 | 0.117 | 0.472 |
| 38 | 0.106 | -0.434 |
| 39 | 0.117 | 0.002 |
| 40 | 0.106 | -1.012 |
| 41 | 0.152 | 1.149 |
| 42 | 0.141 | 0.178 |
| 43 | 0.134 | -0.494 |
| 44 | 0.153 | 0.183 |
| 45 | 0.157 | 0.159 |
| 46 | 0.136 | -0.927 |
| 47 | 0.187 | 1.384 |
| 48 | 0.147 | -0.350 |
| 49 | 0.158 | 0.382 |
| 50 | 0.127 | -0.810 |
| 51 | 0.144 | 0.390 |
| 52 | 0.153 | 1.297 |
| 53 | 0.091 | -1.953 |
| 54 | 0.113 | -0.502 |
| 55 | 0.140 | 1.015 |