| Sample: |
Sample No. 68APs54F -- USGS No. Mesozoic loc. 29773
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| Locality: |
Field No. 68APs54F
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| Description: |
George Plafker, 1968, Float from sec. 34, T. 23 S., R. 35 E., Yakutat (D-4) quadrangle, southeastern Alaska. Yakutat Group. Probably early Pliensbachian rather than late Sinemurian. (from Imlay, 1981, p. 24) [E&R report has handwritten note stating location is in Yakutat D-4 quad. 59o 52.63'N, 139o 23.8'W.]; [USGS Mesozoic loc. 29773. Float, sec. 37, T. 23 S., R. 35 E., Yakutat D-4 quadrangle, southeast Alaska. Crucilobiceras. (description from Imlay and Detterman, 1973, p. 22)]; [USGS Mes. Cat.: Jurassic, Lower, Yakutat Group. Orig. No. 68APs54F. Float sec. 34, T. 23, R. 35., Yakutat District, S.E. Alaska. Collector: Perkins, 1968 for George Plafker] |
| Location: |
Alaska Quadrangle: Yakutat D-4 Township&Range: T23S R35E Section: Sec.34
Lat.: 59o52.63 ' Long.: 139o23.8 ' |
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Reference
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| Title: |
Report on Referred Fossils
,
1968
(11/05)
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| Report by: |
Ralph W. Imlay
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| Referred by: |
George Plafker
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| | Age: | Sinemurian (late Sinemurian) |
| Formation: | Yakutat Group |
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| Comment: | The ammonite fragment from a float block in the Yakutat group at 68APs54F (sec. 34, T. 23, R. 35) is identical in appearance with the outer whorl of the Early Jurassic (late Sinemurian) genus Crucilobiceras. This genus has been found in beds of that age in California, eastern Oregon, and in many parts of Aalsak, such as the Wrangell Mountains, the Talkeetna Mountains, the eastern part of the Alaska Range, and northern Alaska. |
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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: | Sinemurian |
| Formation: | Yakutat Group (Yakutat Group (acc. to USGS Mes. Catalogue entry)) |
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| Comment: | Age: Sinemurian Yakutat Group Shown as locality 9 in figure 2 |
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