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Contributed by Yale Peabody Museum of Natural History.
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Transcription
"next fall so that I may use them.
In general he sees the origin of most of our
Late Cambrian or Ordovician faunas from the
Pacific. At times and irregularly there are faunas
that come to us from the European Atlantic.
There Orgueilian and Chazy oscillations
which there's maybe as much so percent of other
unulations and they be reduced to so far east
land.
Orgueilian time may lag. Inserts 3000' of
deposits. All new to geological student. Thinks
this time or lag as all Ordovician time, I shall
not think more than Sedgwickians Chazy to Hues-
Rivers.
Chaz probably at Inyo Buts California.