Latitude: 69.528329 °N
Longitude: -153.887128 °W
Arctic Slope of Alaska locality USGS 11606, north of Maybe Creek. This locality is a bluff approximately 10 m high on the east side of an unnamed tributary of the Price River. The predominant lithologies are bentonitic clays overlying a silty sandstone capped by coal beds up to 2 m thick, which are in turn overlain by a white-gray medium-grained sandstone. Irregularly dispersed throughout the clay are nodules and sheets of ferruginous limestone (sideritic) which, although light gray when fresh, weather to a rusty brown. With the exception of some poorly preserved plant matter in the upper sandstones, and impressions of platanoid leaves in the power sandstones, the plant material is confined to these fine-grained iron-rich nodules and is preserved as impressions totally lacking cuticle. There is little evidence of post-mortem decay but many leaves are penetrated by vertical fossil rootlets. Platanoid leaves are most common in siltier/sandier facies. The uppermost coal surface supports several in situ tree bases each of which is approximately 20 cm in diameter.
Pinnules: subopposite to alternate, with a short stalk, apex rounded, margin lobate to crenulate becoming dentate near apex, pinnules distally becoming united by wing of rachis; venation indistinct; sori single, globular, marginal on pinnules.
These fern fragments probably all represent the same species which, while they are perhaps most properly referred to the form genus Cladophlebis Brogniart, nevertheless should be compared with the modern genus Dennstaedtia Berhardi of the Cyatheaceae and in particuar D. bipinnata (Cavanilles) Maxon. Specimens USGS 11606.29a and b are part and counterpart of the tip of a fertile frond eith the sori positioned marginally of the pinnules. Similar forms have been described from the Nanaimo Group by Bell (1957, p. 25, Plate, Figs. 2, 4-6; Plate 6, Figs. 1-3, 5, 6; Plate 7, Fig. 3) under the names Cladophlebis (Dennstaedtia?) columbiana. None of Bell's specimens were fertile.