Concavistylon

''Concavistylon'' is an extinct genus of flowering plant in the family Trochodendraceae comprising a single species ''Concavistylon kvacekii''. The genus is known from fossils found in Middle Miocene deposits of central Oregon. A second species '' "Concavistylon" wehrii'' was originally placed in ''Concavistylon'', but subsequently moved to a new genus ''Paraconcavistylon'' in 2020.

Distribution and paleoenvironment

''Concavistylon kvacekii'' fossils were found in the Moose Mountain Flora, formerly called the Cascadia flora or Menagerie Wilderness flora, of Linn County, Oregon. The flora is included in the Little Butte Volcanic series outcropping near the town of Cascadia in the central Oregon Cascades. Work on the flora by paleobotanist Jack Wolfe in 1964 gave an estimated age of Early Miocene, this was later revised by Wolfe and Tanai in 1987 to a Late Oligocene estimation. In the descriptive paper naming ''Concavistylon'' Manchester ''et al.'' reported that radioisotope dating of plagioclase crystals collected by Robert Rosé from the fossiliferous horizon of the Moose Mountain flora had been performed. Using crystals obtained from tuffaceous sandstones, Argon–argon dating provided an age of 14.91 ± 0.23 Ma placing the flora as Middle Miocene Langhian stage. ''C. kvacekii'' is found associated with species such as '' Acer cascadense'', '' Acer smileyi'', '' Ozakia emryi'', '' Trochodendron postnastae'', and '' Trochodendron rosayi''.

Taxonomy and phylogeny

The type species holotype was originally collected during the 1950s by Eleanor Gordon Thompson and donated to the University of California Museum of Paleontology in Berkeley, California as specimen UCMP 151875. Study of the fossil by paleobotanists Steven Manchester, Kathleen Pigg, and Melanie DeVore, resulted in the description of ''Concavistylon kvacekii'' published 60 years later in 2018. The etymology of the genus name was explained, while the specific name "''kvacekii''" was coined as a patronym honoring Czech paleobotanist Zlatko Kvaček.

In a paper published nearly concurrently, a second species was described and placed into the genus as ''Concavistylon wehrii''. The new species was from the older Ypresian age Klondike Mountain Formation of northeastern Washington and McAbee Fossil Beds in central British Columbia. The description of Paleocene trochodendraceous fossils from Wyoming and a phylogenetic analysis of two living and four extinct genera indicated that ''Concavistylon'' was not monophyletic. Based on the pendulous nature of ''"C." wehrii'' inflorescences, which are distinct from the erect inflorescences of ''C. kvacekii'', the new genus ''Paraconcavistylon'' was erected with ''"C." wehrii'' as the type species.

Description

The fruiting bodies of ''Concavistylon kvacekii'' are simple long racemes with a stout central stem. The fruits are either subsessile or born on very short pedicels. Each fruit is composed of between four and six carpels and range between wide by tall. There are between four and five persistent styles that curve upwards towards the fruit apex, a feature not seen in either ''Tetracentron'' or ''Trochodendron'' where the styles curve out and down from the fruit. The fruits open in a four to six ray dehiscence split.

References

{{Taxonbar, from=Q101992533

Trochodendrales
Prehistoric angiosperms
Plants described in 2018
Fossil taxa described in 2018
Miocene plants
Extinct flora of North America
Fossils of the United States