| Sample: |
Sample No. 38AM-F1 -- USGS No. Mesozoic loc. 18082
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| Locality: |
Field No. 38AM-F1
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| Description: |
(NW1/4 of SE1/4 of 621) At foot of glacier at the head of the south fork of the Little Tok River. Mesozoic.; [USGS Mesozoic Iocs. 5723, 16921, 16922, 18082, 18086, and 18089. Area between Slana and Nabesna in eastern part of Alaska Range (Moffit and Knopf, 1910, p. 29; Moffit, 1938b, p. 32; Moffit, 1954, p. 131). Buchia concentrica (Sowerby). (description from Imlay and Detterman, 1973, p. 25)]; [USGS Mes. Cat.: 16921. Orig. No. 34-AM-F3. (NW1/4 of SE1/4 of t21) 2 miles south 30°E of the summit (east side) of Suslota Pass 2 2/3 mi. E. of the lake on Suslositna Creek, Alaska. Coll: F.H. Moffit July 4, 1934] |
| Location: |
Alaska Quadrangle: Nabesna C-5 |
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Reference
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| Title: |
Report on Mesozoic fossils collected in Nutzotin Mountains, Yukon Valley, Alaska, by F.H. Moffit in 1938.
,
1939
(06/30)
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[Note by R.B. Blodgett: report found on pp. 2819-2820 of Alaskan Fossil Reports, v. 12 (1935-1947), kept in Tech. Data Archives office in Anchorage, Alaska--Request for Examination of Fossils form on p. 2817, Fossil Localities, 1938 Moffit on p. 2818] |
| Report by: |
John B. Reeside
, Jr.
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| Referred by: |
J. B. Mertie
, Jr.
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| | Age: | Jurassic |
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| Comment: | Buchia (Aucella) sp., with fine radiating ribs. This seems to me to be a Jurassic form. |
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| Title: |
Jurassic Paleobiogeography of Alaska
,
1973
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ABSTRACT: Jurassic marginal seas occupied considerable areas in southern and northern Alaska and in the western part of the Kuskokwim region of southwestern Alaska. They appear to have been absent during late Callovian time, much restricted during Hettangian, Bathonian, early Oxfordian and late Tithonian time, and most extensive during Sinemurian, Bajocian, and late Oxfordian to middle Tithonian time. A large area in central Alaska was probably never covered. A southwestern prolongation of that area from the Talkeetna Mountains westward to the western end of the Alaska Penin- sula was the site of granitic intrusions during late Early Jurassic time and of extensive erosion during Middle and Late Jurassic time. Variations in the rate of uplift of the area of these granitic intrusive rocks may explain why marine transgressions and regressions were at different times in southern than in northern Alaska during the Bajocian and Bathonian. Connection of the northern and southern marginal seas occurred through Yukon Territory and eastern- most Alaska. The Jurassic ammonite succession in Alaska is similar to that in central and northern Europe and northern Asia. In Lower Jurassic beds, it is essentially identical. In Bajocian and in Oxfordian to lower Kimmeridgian beds, the ammonite succession in Alaska differs from that in the other areas mainly by the presence of some genera found only in areas bordering the Pacific Ocean and by the absence of a few genera common in central and northern Europe. In con- trast, the Bathonian rocks of Alaska contain ammonites, such as Arcticoceras, Arctocephalites, and Cranocephalites, that are widespread in the Arctic region but are unknown in central Europe. Comparisons with the Tithonian of Europe are not possible because ammonites of that age, other than Lytoceras and Phylloceras, are not yet known from Alaska. The Alaskan Jurassic ammonites of late Pliensbachian Age and of Bathonian to early Kimmeridgian Age belong mostly to the Boreal realm and have very little in common with Tethyan realm ammonites such as those found in areas bordering the Mediterranean Sea. |
| Report by: |
Ralph W. Imlay
,
Robert L. Detterman
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| | Age: | Oxfordian-Kimmeridgian (late Oxfordian - early Kimmeridgian) |
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| Comment: | Generalized locality shown shown as locality 6 in figure 7 |
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