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. 2021 Feb 18;127(5):681–695. doi: 10.1093/aob/mcab005

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