Pteronepelys

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Pteronepelys
Temporal range: 49.5–44  Ma
Pteronepelys wehrii samara SRIC 01.jpg
Fossil Pteronepelys wehrii fruit
Scientific classification OOjs UI icon edit-ltr.svg
Kingdom: Plantae
Clade: Tracheophytes
Clade: Angiosperms
Order: incertae sedis
Genus:† Pteronepelys
Manchester, 1994
Species:
†P. wehrii
Binomial name
†Pteronepelys wehrii

Pteronepelys, sometimes known as the winged stranger, is an extinct genus of flowering plant of uncertain affinities, which contains the one species, Pteronepelys wehrii. It is known from isolated fossil seeds found in middle Eocene sediments exposed in north central Oregon and Ypresian-age fossils found in Washington, US.

Contents

Distribution and paleoecology

Pteronepelys wehrii has been identified from two locations in the Clarno Formation, the leaf layer in the Clarno nut beds, type locality for the species plus the White Cliffs. The nut beds are approximately 3 kilometres (1.9 mi) east of the unincorporated community of Clarno, Oregon, while the White Cliffs locality is south of Clarno, and both considered to be middle Eocene in age. The dating is based on averaging zircon fission track radiometric dating which yielded an age of 43.7  ± 0.1 million years ago and Argon–argon dating radiometric dating which yielded a 36.38  ± 1.31 million years ago to 46.8  ± 3.36 million years ago date. [1] The average of the dates resulted in an age range of 2  million years ago. The beds are composed of silica and calcium carbonate cemented tuffaceous sandstones, siltstones, and conglomerates which preserve either a lake delta environment, or alternatively periodic floods and volcanic mudflows preserved with hot spring activity. [1]

Five additional specimens were studied from a location in the Eocene Okanagan Highlands, an outcrop of the Ypresian [2] Klondike Mountain Formation in Republic. [3] The formation preserves an upland lake system surrounded by a mixed conifer–broadleaf forest with nearby volcanism. [4] The pollen flora has notable elements of birch and golden larch, and distinct trace amounts of fir, spruce, cypress, and palm. [2] Wolfe and Tanai (1987) interpreted the forest climate to have been microthermal, [5] [6] having distinct seasonal temperature swings which dipped below freezing in the winters. However, further study has shown the lake system was surrounded by a warm temperate ecosystem that likely had a mesic upper microthermal to lower mesothermal climate, in which winter temperatures rarely dropped low enough for snow, and which were seasonably equitable. [2] [7]

It was likely wind-dispersed seed, and possibly part of the canopy flora of the forests, [1] however the affinities of Pteronepelys with other flowering plants were unknown at the time of description. [1]

History and classification

The Pteronepelys wehrii specimens were studied by paleobotanist Steven R. Manchester of the University of Florida. He published his 1994 type description for P. wehrii in the Journal Palaeontographica Americana . The genus and species were described from a series of type specimens, the holotype specimen OMSI PM018, which was preserved in the paleobotanical collections of the Oregon Museum of Science and Industry in Portland, Oregon, and seven paratype specimens. Of the paratypes, one is housed in the University of Florida collections, a second is in the OMSI collections, with the remaining five in the Burke Museum paleontology collections. [1]

The genus name Pteronepelys is a combination of the Greek word elements Pteron meaning "wing" and epelys roughly translating to "stranger", while Manchester coined the specific epithet wehrii in honor of paleobotanist and artist Wesley Wehr, in recognition of contribution of the Klondike Mountain Formation specimens. [1] The genus has been occasionally given the vernacular name "winged stranger" as a result of the genus name. [8] [9]

Description

Pteronepelys wehrii samaras are elongated and flattened sideways, with an elliptical wing that joins to an ovoid endocarp. The nutlets are 3.5 mm–4.5 mm × 2.6 mm–3.0 mm (0.14 in–0.18 in × 0.10 in–0.12 in) with an estimated thickness between 2–2.5 mm (0.079–0.098 in). The tip of the nutlet sports four to five short sepals which are 1.5 mm × 1.5 mm (0.059 in × 0.059 in) with round tips. In the middle of the nutlet tip are two central styles. The 10.0–13.9 mm (0.39–0.55 in) wing has a convex lower margin and a convex to straight upper margin which meet at the basal end of the samara at a point where it would have connected to the parent plant. Three veins run the length of the wing, arising from the basal wingtip and merging onto the nutlet. Thick veins follow along the upper margin and cross the midline of the wing, while a third, thin vein curves parallel to the lower margin between the midvein and margin. [1]

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References

  1. 1 2 3 4 5 6 7 Manchester, S.R. (1994). "Fruits and Seeds of the Middle Eocene Nut Beds Flora, Clarno Formation, Oregon". Palaeontographica Americana. 58: 21, 106–107.
  2. 1 2 3 Moss, P. T.; Greenwood, D. R.; Archibald, S. B. (2005). "Regional and local vegetation community dynamics of the Eocene Okanagan Highlands (British Columbia – Washington State) from palynology". Canadian Journal of Earth Sciences. 42 (2): 187–204. Bibcode:2005CaJES..42..187M. doi:10.1139/E04-095.
  3. ↑ Pigg, K. B.; Manchester, S. R.; Wehr, W. C. (2003). "Corylus, Carpinus, and Palaeocarpinus (Betulaceae) from the Middle Eocene Klondike Mountain and Allenby Formations of Northwestern North America". International Journal of Plant Sciences. 164 (5): 807–822. doi:10.1086/376816. S2CID   19802370.
  4. ↑ Archibald, S.; Greenwood, D.; Smith, R.; Mathewes, R.; Basinger, J. (2011). "Great Canadian Lagerstätten 1. Early Eocene Lagerstätten of the Okanagan Highlands (British Columbia and Washington State)". Geoscience Canada. 38 (4): 155–164.
  5. ↑ Wolfe, J.A.; Tanai, T. (1987). "Systematics, Phylogeny, and Distribution of Acer (maples) in the Cenozoic of Western North America". Journal of the Faculty of Science, Hokkaido University. Series 4, Geology and Mineralogy. 22 (1): 1–246.
  6. ↑ Wolfe, J. A.; Wehr, W. C. (1987). Middle Eocene dicotyledonous plants from Republic, northeastern Washington (PDF) (Report). Bulletin. Vol. 1597. United States Geological Survey. pp. 1–25. doi: 10.3133/b1597 .
  7. ↑ Greenwood, D. R.; Archibald, S. B.; Mathewes, R. W; Moss, P. T. (2005). "Fossil biotas from the Okanagan Highlands, southern British Columbia and northeastern Washington State: climates and ecosystems across an Eocene landscape". Canadian Journal of Earth Sciences. 42 (2): 167–185. Bibcode:2005CaJES..42..167G. doi:10.1139/e04-100.
  8. ↑ Archibald, S. B.; et al. (2005). "Wes Wehr dedication". Canadian Journal of Earth Sciences. 42 (2): 115–117. Bibcode:2005CaJES..42..115A. doi:10.1139/E05-013.
  9. ↑ Julie Vanderwal (2019-02-27). "Jack Nisbet presents Highland Wonders program about Wes Wehr". The Wenatchee World. Wenatchee, Washington. Retrieved 2021-11-07.
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