Reference
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Title: |
Report on Referred Fossils
,
1969
(11/17)
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This report concerns the shelly faunas collected by Berg and Jones in 1969 and by Berg in 1968 from Bostwick Inlet, Gravina Island. |
Report by: |
Norman J. Silberling
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Referred by: |
Henry C. Berg
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| Age: | Norian (late Norian) |
Formation: | Chapin Peak Formation (Revised; Robert B. Blodgett, 02/09/2008 ) |
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Comment: | These collections, which I presume are from a fairly retricted stratigraphic thickness, each contain at least one faunal element diagnostic of the upper Norian. They relate most closely to faunas known from Tyaughton Creek in western British Columbia, from Vancouver Island, and from the Gabbs Formation in western Nevada. Some of the species represented, such as the species of Cycloceltites, suggest a latest late Norian age, not Rhaetian but younger than faunas typical of the Suessi Zone and the commonly occurring kinds of Monotis such as M. subcircularis. |
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Title: |
Letter
,
1969
(06/03)
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Letter from D.L. Jones to H.C. Berg. |
Report by: |
David L. Jones
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Referred by: |
Henry C. Berg
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| Age: | Norian (late Norian) |
Formation: | Chapin Peak Formation (Revised; Robert B. Blodgett, 02/09/2008 ) |
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Comment: | Fossils from locality 69ABg130 are definitely Triassic (upper Norian). With the help of Norm Silberling, the following forms have been identified (see faunal list). Other unidentified forms are also present, but the above suffice for the late Norian age determination. Fossils from the "clast" appear to be the same types of things. |
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