Walliser, Eric Otto; Lohmann, Gerrit; Niezgodzki, Igor; Schöne, Bernd R (2018): Growth increment width measurement and SGIshell data, Alzey Formation, Mainz Basin, middle Rupelian (MB-Wht-8) [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.884923, 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: 49.740056 * Longitude: 8.072333
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 | 0.874 | -0.828 |
| 11 | 0.959 | 0.945 |
| 12 | 0.531 | -0.712 |
| 13 | 0.368 | -1.180 |
| 14 | 0.338 | -0.718 |
| 15 | 0.545 | 3.089 |
| 16 | 0.301 | 0.176 |
| 17 | 0.168 | -1.675 |
| 18 | 0.253 | 0.727 |
| 19 | 0.228 | 0.698 |
| 20 | 0.181 | -0.069 |
| 21 | 0.163 | -0.324 |
| 22 | 0.138 | -1.007 |
| 23 | 0.192 | 0.412 |
| 24 | 0.226 | 1.151 |
| 25 | 0.173 | -0.412 |
| 26 | 0.180 | -0.284 |
| 27 | 0.203 | 0.269 |
| 28 | 0.194 | 0.077 |
| 29 | 0.206 | 0.548 |
| 30 | 0.179 | 0.070 |
| 31 | 0.128 | -1.098 |
| 32 | 0.174 | 0.754 |
| 33 | 0.155 | 0.598 |
| 34 | 0.109 | -0.639 |
| 35 | 0.109 | -0.206 |
| 36 | 0.107 | -0.019 |
| 37 | 0.099 | -0.334 |
| 38 | 0.068 | -1.963 |
| 39 | 0.121 | 0.070 |
| 40 | 0.182 | 2.308 |
| 41 | 0.153 | 1.272 |
| 42 | 0.097 | -0.658 |
| 43 | 0.083 | -0.896 |
| 44 | 0.057 | -1.980 |
| 45 | 0.109 | 0.932 |
| 46 | 0.099 | 0.381 |
| 47 | 0.097 | 0.304 |
| 48 | 0.086 | -0.284 |
| 49 | 0.066 | -1.377 |
| 50 | 0.115 | 1.387 |
| 51 | 0.090 | 0.053 |
| 52 | 0.076 | -0.705 |
| 53 | 0.104 | 1.042 |
| 54 | 0.083 | -0.135 |
| 55 | 0.068 | -1.058 |
| 56 | 0.103 | 0.895 |