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-4) [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.884929, 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:
141 data points
Data
| 1 Years [a] | 2 G. planicostalis growth [mm] | 3 phi ´ |
|---|---|---|
| 10 | 0.124 | 0.126 |
| 11 | 0.105 | -1.454 |
| 12 | 0.151 | 1.628 |
| 13 | 0.151 | 1.842 |
| 14 | 0.104 | -1.114 |
| 15 | 0.109 | -0.142 |
| 16 | 0.107 | 0.249 |
| 17 | 0.072 | -2.479 |
| 18 | 0.100 | -0.103 |
| 19 | 0.106 | 0.216 |
| 20 | 0.120 | 1.188 |
| 21 | 0.103 | -0.189 |
| 22 | 0.100 | -0.338 |
| 23 | 0.100 | -0.229 |
| 24 | 0.105 | 0.523 |
| 25 | 0.103 | 0.745 |
| 26 | 0.101 | 1.237 |
| 27 | 0.069 | -1.427 |
| 28 | 0.064 | -1.653 |
| 29 | 0.083 | 0.446 |
| 30 | 0.089 | 0.965 |
| 31 | 0.091 | 1.067 |
| 32 | 0.074 | -0.890 |
| 33 | 0.091 | 0.880 |
| 34 | 0.083 | -0.178 |
| 35 | 0.083 | -0.491 |
| 36 | 0.086 | -0.650 |
| 37 | 0.113 | 1.265 |
| 38 | 0.104 | -0.079 |
| 39 | 0.096 | -1.098 |
| 40 | 0.131 | 1.272 |
| 41 | 0.118 | -0.029 |
| 42 | 0.110 | -0.788 |
| 43 | 0.117 | -0.577 |
| 44 | 0.111 | -1.329 |
| 45 | 0.147 | 0.704 |
| 46 | 0.155 | 1.073 |
| 47 | 0.132 | -0.313 |
| 48 | 0.108 | -1.621 |
| 49 | 0.137 | 0.760 |
| 50 | 0.123 | 0.373 |
| 51 | 0.101 | -0.550 |
| 52 | 0.102 | 0.408 |
| 53 | 0.092 | 0.428 |
| 54 | 0.072 | -0.566 |
| 55 | 0.062 | -0.862 |
| 56 | 0.074 | 1.753 |