Sample: |
Sample No. 48AI81 -- USGS No. Mesozoic loc. 21282
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Locality: |
Field No. 48AI81
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Description: |
[Shown as locality 133 on Pl. 3 of Detterman and Hartsock, 1966 - Note by R.B. Blodgett: digitization of this point gives approx. lat. 60o 06'26" N., 152o 42'40" W.][Imlay, 1982, p. 13 provides following description: "R.W. Imlay and D.J. Miller, 1948. Tuxedni Bay area, on tributary entering Bear Creek from the southeast, 4.75 miles (7.6 km) S. 22o W. of Fossil Point. Twist Creek Siltstone, 300 ft. (91 m) above base."];[21282 R. W. Imlay and D. J. Miller, 1948. Tuxedni Bay area, on tributary entering Bear Creek from the southeast 4.75 miles S 22° W of Fossil Point. Bowser member of the Tuxedni formation, about 300 feet above base. (description from Imlay, 1961, p. 469)] |
Location: |
Alaska Quadrangle: Kenai A-8 Lat.: 60o06'26 " Long.: 152o42'40 " |
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Reference
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Title: |
Late Bajocian ammonites from southern Alaska
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1982
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ABSTRACT Early late Bajocian ammonites have been found in southern Alaska in the Talkeetna Mountains, on the west side of Cook Inlet between Tuxedni Bay and Iniskin Bay, and in the lower Kuskokwim-Bristol Bay area north of Togiak Bay. This dating is based mostly only the association of Normannites, Stephanoceras, and Stemmatoceras, which are unknown or rare above beds of that age, with Cadomites and Leptosphinctes, which occur rarely just below beds of that age but range much higher. The dating is also based on the presence of a fragmentary ammonite that in lateral view resembles Spiroceras, a genus not known in beds older than early late Bajocian. Such an association of ammonites occurs west of Cook Inlet in the Twist Creek Siltstone, which rests conformably on the Cynthia Falls Sandstone of late middle Bajocian age and is overlain with marked unconformity by the Bowser Formation of early to late Bathonian Age. Such as association of ammonites is also found in the Talkeetna Mountains in unnamed beds that are nearly identical lithologically with the Twist Creek Siltstone, that rest conformably on beds of late middle Bajocian Age, and that are overlain with probably unconformity by beds of early Bathonian Age. The presence of such an unconformity is suggested by the fact that beds of early late Bajocian age have been found only in two areas in the Talkeetna Mountains, that still younger Bajocian beds have not been found anywhere in southern Alaska, and that still younger lower Bathonian beds are fairly widespread inthe Talkeetna Mountains as well as west of Cook Inlet. Most of the ammonite genera and subgenera present in the Twist Creek Silstone and in equivalent beds in southern Alaska are characteristic of the Tethyan Realm. The exceptions include |
Report by: |
Ralph W. Imlay
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| Age: | Bajocian (early late Bajocian) |
Formation: | Twist Creek Siltstone |
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Comment: | Shown as locality 3 on Fig. 4 |
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Title: |
New genera and subgenera of Jurassic (Bajocian) ammonites from Alaska
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1961
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ABSTRACT-New genera and species of Bajocian ammonites from Alaska include
Megasphaeroceras rotundum Imlay, Dettermanites vigorosus Imlay, and Parabigotites
crassicostatus Imlay. A new subgenus and species is Oppelia (Liroxyites) kellumi
Imlay. Of these Megasphaeroceras, Dettermanites and Oppelia (Liroxyites) are associated
with Spiroceras? Leptosphinctes, and Sphaeroceras of late Bajocian age. Parabigotites is associated with Stephanoceras, Otoites, Sonninia, Witchellia and
Lissoceras of middle Bajocian age. |
Report by: |
Ralph W. Imlay
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| Age: | Bajocian (late Bajocian) |
Formation: | Bowser Formation (Bowser Member of Tuxedni Formation) |
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