Table 2.
Fossils used for nine calibration nodes of the molecular clock. The four with dashes in the last three columns were not used because they are redundant with (and sometimes younger than) the ones used
| Calibration node* | Fossil assigned to | Fossil (reference) | Location | Period | Age | OFFSET | LOGMEAN | LOGSTDV |
|---|---|---|---|---|---|---|---|---|
| 21 | All taxa | Calamostachys binneyana (Good, 1971) | USA, Kentucky, Lewis Creek and Shack Branch | Lower Pennsylvanean | 323–359 | 323 | 3 | 1 |
| 22 | All Equisetum | Equisetum thermale (Channing et al., 2011) | Argentina, Patagonia | Middle to Upper Jurassic | 152–164 | – | – | – |
| 22 | All Equisetum | Equisetites lyelii (Watson, 1983) | UK, Sussex | Lower Cretaceous | 125–150 | – | – | – |
| 22 | Subgenus Paramochaete | Equisetites minimus (Falaschi et al., 2009) | Argentina, Sta Cruz Prov. | Middle Jurassic | 174–164 | 164 | 2 | 1 |
| 22 | Subgenus Paramochaete | Equisetum laterale (Gould, 1968) | Australia, Queensland | Middle Jurassic | 145–174 | – | – | – |
| 25 | E. palustre, E. pratense | Equisetum ‘pratense’ (Zhang et al., 2007) | China, Yunnan | Late Tertiary, Miocene | 5.3–23 | 5.3 | 0.5 | 1 |
| 27 | E. telmateia, E. braunii | Equisetum maximum (Reed, 1971) | Upper Silesia (Poland) | Miocene | 5–23 | 5 | 0.5 | 1 |
| 28 | E. sylvaticum, E. diffusum, E. arvense, E. fluviatile | Equisetum fluviatoides (McIver and Basinger, 1989) | Canada, Saskatchewan | Palaeocene | 56–66 | 56 | 1 | 1 |
| 31 | Subgenus Hippochaete | Equisetum perlaevigatum (Reed 1971) | USA, Colorado | Late Cretaceous | 66–72 | 66 | 1 | 1 |
| 32 | E. variegatum, E. ramosissimum, E. praealtum, E. hyemale, E. giganteum, E. xylochaetum, E. laevigatum, E. myriochaetum | Equisetum clarnoi (Brown, 1975) | USA, Oregon | Middle Eocene | 37.8–47.8 | 37.8 | 1 | 1 |
| 34 | E. giganteum, E. xylochaetum, E. laevigatum, E. myriochaetum | Equisetum sp. (Thomasson, 1980) | USA, Nebraska | Late Tertiary | 0–5.3 | – | – | – |
| 34 | E. giganteum, E. xylochaetum, E. laevigatum, E. myriochaetum | Equisetites sp. (Contreras and Lutz, 2014) | Argentina, Formosa, Bermejo River | Lower Holocene | 2.6–11.6 | 2.6 | 0.5 | 1 |
| 38 | E. praealtum, E. hyemale | Equisetum hyemale (Reed, 1971) | Hungary | Upper Miocene | 11.6–13.8 | 11.6 | 0.5 | 1 |
*Numbers correspond to nodes shown in Fig. 2