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| Morphology | Ecology and taphonomy | External Literature Search | Age range and collections |
Smithtonia jonesii
Taxonomy
Smithtonia jonesii was named by Hill and Pole (1992) [Type locality. Little Rapid River, north-western Tasmania. Specimens examined. LRR2-1306, 1310, 1311.]. It is considered to be a form taxon. Its type specimen is Holotype. LRR2-1311, housed in the Department of Plant Science, University of Tasmania., a leaf (Cuticle), and it is a compression fossil. Its type locality is Little Rapid River 2, which is in an Oligocene lacustrine mudstone/sandstone in Australia.
Synonymy list
| Year | Name and author |
|---|---|
| 1992 | Smithtonia jonesii Hill and Pole p. 355 figs. 31-35 |
| 1992 | Smithtonia jonesii Pole p. 443 |
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If no rank is listed, the taxon is considered an unranked clade in modern classifications. Ranks may be repeated or presented in the wrong order because authors working on different parts of the classification may disagree about how to rank taxa.
†Smithtonia jonesii Hill and Pole 1992
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
No ecological data are available
Age range: base of the Middle Eocene to the top of the Late/Upper Oligocene or 47.80000 to 23.03000 Ma
Collections (2 total)
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Middle Eocene - Late/Upper Eocene | Australia (Tasmania) | Smithtonia jonesii (166978) | |
| Late/Upper Oligocene | Australia (Tasmania) | Smithtonia jonesii (type locality: 167317) |