of
Sample: Sample No. 67AR260 -- USGS No. Paleobot. loc. 11123
Locality: Field No. 67AR260
Description: From unnamed conglomerate, sandstone, and siltstone sequences north of Farewell Fault. Alaska. SW1/4 sec. 33, T. 27 N., R. 27 W., McGrath B-3 quad. Lat. 62o 23'05" N., long. 154o 17'55" W. Coll: Bruce Reed, 1967.
Location: Alaska Quadrangle: Mc Grath B-3
Township&Range: T27N R27W Section: SW1/4 sec. 33
Lat.: 62o23'05 " Long.: 154o17'55 "
Reference
Title: Report on Referred Fossils ,  1968 (05/03)
If the material, which is not sufficiently well preserved for specific determination, represents the compared species, an early Tertiary, probably Paleocene, age is indicated.
Report by: Jack A. Wolfe
Referred by: Bruce Reed
Age: Oligocene
Formation: Unnamed
Rock Type:Primary: Clastics
Comment:The above collections [67AR260, 67AR222, 67AR259] are of probable middle or late Oligocene age. Both Alnus evidens and "Carya" magnifica (this is actually referable to Juglans) are indicative of this age. The presence of Metasequoia morphologically identical on foliage to the extant species definitely prohibits a Paleocene or early Eocene age. The new species of Alnus is very similar to, but probably not conspecific with the Seldovian A. barnesi Wolfe. The Populus in 11125 is poorly preserved but appears conspecific with a Populus found in several other mid-late Oligocene floras in Alaska.
Occurrence(s)
No. Group Name Qty Notes
1 Plants Glyptostrobus sp.
2 Plants Metasequoia cf. M. glyptostroboides Hu & Cheng
3 Plants Alnus evidens (Holl.) Wolfe
4 Plants Alnus n. sp.