Table 2.
Identification of the number of A. unedo accessions (N) and edaphoclimatic characterization of the respective provenance in Portugal.
| Local/Provenance | N | Lithology 1 | pH 2 | T annual (°C) 3 | P annual (mm) 3 | Humidity Index | Xeroth. Index | Climatic Classification 4 | Climatic Classif. 5 |
|---|---|---|---|---|---|---|---|---|---|
| TM-Fisgas Ermelo/FE | 6 | Shales, Quarzites | 2 | 13.4 | 1390.5 | 111.51 | 42.40 | Sub-Mediterranean | B4 B′2 s a′ |
| TM-Mosteiró | 19 | Shales | 3 | 13.4 | 1128.1 | 84.69 | 60.96 | Attenuated Mesomed 4.1 | B3 B′2 s2 a′ |
| São Mamede | 26 | Shales, Sandst. 1.1 | 2 | 15.2 | 852.4 | 45.41 | 71.38 | Attenuated Mesomed 4.1 | B1 B′2 s2 a′ |
| Penamacor | 24 | Shales, Quarzites | 2 | 14.4 | 838.2 | 47.80 | 98.64 | Accentuated Mesomed 4.1 | B1 B′2 s2 a′ |
| Penha Garcia * | 2 | Shales | 3 | 14.4 | 838.2 | 47.80 | 98.64 | Accentuated Mesomed 4.1 | B1 B′2 s2 a′ |
| Cadaval * | 4 | Gonglomerates 1.2 Sand 1.1 | 3 | 15.0 | 777.6 | 40.20 | 86.64 | Accentuated Mesomed 4.1 | C2 B′2 s a′ |
| Monchique * | 25 | Syenite & Shale | 2 | 15.1 | 949.0 | 60.22 | 87.36 | Accentuated Mesomed 4.1 | B1 B′2 s2 a′ |
| ODM-Pomba * | 16 | Shale, graywacke | 3 | 15.8 | 715.7 | 34.27 | 87.52 | Accentuated Mesomed 4.1 | C2 B′2 s2 a′ |
| ODM-Cerca Pomares * | 3 | Shale, graywacke | 3 | 15.0 | 760.5 | 35.69 | 88.96 | Accentuated Mesomed 4.1 | C2 B′2 s a′ |
| ODM-Trancão * | 9 | Shale, graywacke | 3 | 15.0 | 571.9 | 15.73 | 85.04 | Accentuated Mesomed 4.1 | C1 B′2 s a′ |
| ODM-Nave Redondo * | 10 | Shale, graywacke | 3 | 15.1 | 748.9 | 40.03 | 90.56 | Accentuated Mesomed 4.1 | C2 B′2 s2 a′ |
| ODM-Cortes Pereira * | 15 | Shale, graywacke | 3 | 15.8 | 623.1 | 22.08 | 83.52 | Accentuated Mesomed 4.1 | C1 B′2 s2 a′ |
| Caldeirão | 25 | Shale, graywacke | 3 | 15.9 | 866.7 | 51.40 | 95.90 | Accentuated Mesomed 4.1 | B1 B′2 s2 a′ |
| Barrocal | 20 | Limestone | 4 | 15.9 | 697.0 | 33.96 | 118.18 | Attenuated Thermomed 4.2 | C2 B′2 s2 a′ |
* Cultivated and wild plants identified with the Producers’ support. 1 Lithology according to lithological map [44] associated, in general (according to Soil Classification WRB [45]), to Leptosols and Cambisols [46]. 1.1 Shales and sandstones; 1.2 conglomerates and sandstones. 2 pH soil classification mean per provenance: 1-very low (<4); 2-low (4–5.4); 3-medium (5.5–7.4); 4-high (7.5–9); 5-very high (>9). 3 Annual averages of temperature (°C) and precipitation (mm), corresponding to 1951–1980 period [47]. 4 Climatic classification according to xerothermic index [48]. 4.1 Mesomediterranean; 4.2 Thermomediterranean. 5 Climatic classification according to Thornthwaite [49] present in the table: 1st letter (Hydric index–IH): (i) humid and rainy climates B4, B3 e C2—respectively very humid, humid and subhumid vs. (ii) dry climates C1–Dry subhumid. 2nd letter (Thermal efficiency (∑ PET): B′2—mesothermic. 3rd letter for mediterranean climate: (i) Humid and subhumid climate group (1st Letter A, B or C2):–s (moderate water deficiency in summer); s2 (severe scarcity of water in the summer); (ii) Dry climate group (1st letter C1 or D): s (moderate excess water in winter); s2 (high water excesses in the winter season). 4th letter (concentration of thermal efficiency in the hot season): a′–small concentration of thermal efficiency during summer.