Pinus matthewsii
Pinus matthewsii Temporal range:
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Scientific classification | |
Kingdom: | Plantae |
Clade: | Tracheophytes |
Clade: | Gymnospermae |
Division: | Pinophyta |
Class: | Pinopsida |
Order: | Pinales |
Family: | Pinaceae |
Genus: | Pinus |
Section: | P. sect. Trifoliae
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Subsection: | P. subsect. Contortae
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Species: | P. matthewsii
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Binomial name | |
Pinus matthewsii |
Pinus matthewsii is an extinct species of conifer in the pine family. The species is solely known from the Pliocene sediments exposed at Ch’ijee's Bluff on the Porcupine River near Old Crow, Yukon, Canada.[1]
Type locality
Pinus matthewsii was described from the three
History and classification
Pinus matthewsii is known from only three fossils, the
The ovulate cones of Pinus matthewsii range from 3.4–4.4 centimetres (1.3–1.7 in) in length and 2.8–3.4 centimetres (1.1–1.3 in). While the overall morphology and structure of P. matthewsii cones compare to cones of the living species Pinus banksiana, notable differences occur. The elongated cones of P. banksiana have an asymmetrically reflexed cone base, while P. matthewsii are symmetrical and oval. Cones of P. matthewsii and P. contorta are also similar in structuring, however the combination of characters that are present in P. matthewsii are not found in any one of the subspecies of P. contorta.[1]
Similar to the modern habits of P. contorta, it is suggested that P. matthewsii may have been a shade intolerant tree which acted as a colonizer. This is supported by the seeds preserved within the cones, the seeds being small with long detachable wings. The combination of characters would support a large wind dispersal range.[1]
References
- ^ S2CID 86234947. Archived from the original(PDF) on 2008-02-21. Retrieved 2011-05-16.