| Sample: |
Sample No. AG 882 -- USGS No. Mesozoic loc. 29135
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| Locality: |
Field No. AG 882
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| Description: |
Many USGS Mesozoic localities near the Canning River, northeast Alaska. Mesozoic Iocs. 24014, 21028, 25598, and 29882 (Imlay, 1955, p. 79, 80; Keller and others, 1961, p. 193) from lat 69°30'45" N. to 69°33' N.; long 146°18' W. to 146°23' W.; Mesozoic Iocs. 29134-29136 near Shublik Island at lat 69°24' N., long 146° 10' W. Amoeboceras (Prionodoceras) and Buchia concentrica ( Sowerby). (description from Imlay and Detterman, 1973, p. 25); British Petroleum Alaska (Inc.) , 1964. Canning River near Shublik Island and about 1.6 km west of mouth of Cache Creek, lat 69°24' N., long 146°10' W., SE. cor.
T. 1 N., R. 24 T., Mt. Michelson Quadrangle, Kingak Shale. Late Oxfordian to early Kimmeridgian. (description from Imlay, 1981, USGS PP 1190, p. 23); [USGS Mes. Cat.: 29135 (AG 882) Upper Jurassic - Kingak Sh. Same loc. as 29134. Collector: British Petroleum, 1964] |
| Location: |
Alaska Quadrangle: Mt Michelson B-4
Lat.: 69o24' " Long.: 146o10' " |
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Reference
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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) |
| Formation: | Kingak Shale |
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| Comment: | Generalized locality shown shown as locality 4 in figure 7 |
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| Title: |
Late Jurassic Ammonites from Alaska
,
1981
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| Report by: |
Ralph W. Imlay
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| | Age: | Oxfordian-Kimmeridgian (late Oxfordian - early Kimmeridgian) |
| Formation: | Kingak Shale |
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| Comment: | Shown as loc.. 2 on Fig. 1; also shown on Figure 2 and Table 4 "In the Canning River area, the Kingak Shale has furnished the late Oxfordian to Kimmeridgian ammonite Amoeboceras (Prionodoceras) and A.
(Amoebites) in association with the bivalve Buchia concentrica (Sowerby). Such mollusks were collected from about 1,040 feet (315 m) of shale exposed on the west side of the river opposite the mouth of Cache Creek (Imlay, 1976, p. 4). The lowermost occurrence (USGS Mesozoic loc. 29135) is about 600 feet (182 m) above beds containing the late middle Bathonian ammonite Arctocephulites." [from Imlay, 1981, p. 15] |
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