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-5) [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.884935, 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:
144 data points
Data
| 1 Years [a] | 2 G. planicostalis growth [mm] | 3 phi ´ |
|---|---|---|
| 10 | 0.374 | -1.145 |
| 11 | 0.325 | -0.989 |
| 12 | 0.262 | -1.039 |
| 13 | 0.258 | -0.250 |
| 14 | 0.132 | -1.789 |
| 15 | 0.123 | -1.337 |
| 16 | 0.113 | -0.898 |
| 17 | 0.095 | -0.916 |
| 18 | 0.105 | 0.035 |
| 19 | 0.085 | -0.554 |
| 20 | 0.146 | 2.509 |
| 21 | 0.138 | 2.110 |
| 22 | 0.108 | 0.572 |
| 23 | 0.102 | 0.162 |
| 24 | 0.122 | 0.912 |
| 25 | 0.118 | 0.626 |
| 26 | 0.113 | 0.297 |
| 27 | 0.086 | -0.943 |
| 28 | 0.104 | -0.258 |
| 29 | 0.145 | 1.340 |
| 30 | 0.143 | 1.214 |
| 31 | 0.099 | -0.606 |
| 32 | 0.084 | -1.215 |
| 33 | 0.099 | -0.682 |
| 34 | 0.128 | 0.379 |
| 35 | 0.109 | -0.437 |
| 36 | 0.117 | -0.266 |
| 37 | 0.131 | 0.130 |
| 38 | 0.121 | -0.310 |
| 39 | 0.141 | 0.295 |
| 40 | 0.168 | 1.174 |
| 41 | 0.144 | 0.322 |
| 42 | 0.125 | -0.288 |
| 43 | 0.144 | 0.379 |
| 44 | 0.098 | -1.151 |
| 45 | 0.125 | -0.163 |
| 46 | 0.119 | -0.305 |
| 47 | 0.124 | -0.095 |
| 48 | 0.139 | 0.528 |
| 49 | 0.160 | 1.420 |
| 50 | 0.132 | 0.505 |
| 51 | 0.085 | -1.191 |
| 52 | 0.089 | -0.927 |
| 53 | 0.085 | -1.050 |
| 54 | 0.120 | 0.505 |
| 55 | 0.109 | 0.106 |
| 56 | 0.130 | 1.025 |
| 57 | 0.094 | -0.467 |