Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
7/29/02
Summary
Winthrop fm is arkosic at T0 and becomes siliclastic
in basal 300',
Fossil plants are found
in sandy and clayey units
throughout or at least 10
levels in the unit T0 within
30m of the base.
The basal several sands have
larger amounts of Widdington-
itites than those above
It may be that it is deriving
a larger sample from
the conifer woodlands
surrounding the faw/marnder
zone where the majority of
the fossil plantary record
appears to be derived.
Summary of Smithsonian Winthrop
collection
~ 125 specimens
Coll. Hardley x Russell in
1898 for uses