of
Sample: Sample No. No Data -- USGS No. Mesozoic loc. M1911
Locality: Field No. No Data
Description: From a 0.3 m (1 ft) thick silicified shell bed situtated 52.7-53.0 m (173-174 ft) above the contact with underlying Keku Volcanics. Bed within a beautifully exposed shoreline section of the Cornwallis Limestone situated on the south side of small cove. Geographic coordinates for the locality (approximately 3 m (10 ft) west of a prominent cliff of limestone) is 56o 51.66' N and 134o 00.62' W.; SW1/4, NE1/4, NW 1/4, of the NW1/4 of sec. 12, T. 58 S., R. 72 E, Port Alexander D-1 quad. (description from Blodgett and Fryda, 2001, p. 236)
Location: Alaska Quadrangle: Port Alexander D-1
Township&Range: T58S R72E Section: SW1/4,NE1/4,NW1/4NW1/4 sec. 12
Lat.: 56o51.66 ' Long.: 134o00.62 '
Reference
Title: On the occurrence of Spinidelphinulopsis whaleni (Gastropoda) in the Late Triassic (early Norian) Cornwallis Limestone, Kuiu Island, southeastern Alaska (Alexander terrane) and its paleobiogeographic significance ,  2001
Abstract. The gastropod Spinidelphinulopsis whaleni Blodgett, Fryda and Stanley, 2001, was originally described from late Carnian or early Norian strata on the Oregon side of Hells Canyon in the Wallowa terrane of the Pacific Northwest (Oregon, Idaho, and Washington). It is probably also present in early Norian strata at Green Butte, Wrangell Mountains (Wrangellia terrane) of southern Alaska. The common presence of this species and many other shared gastropod species has previously been cited as being evidence for close biogeographic linkage between the Wrangellia and Wallowa terranes. Quite dissimilar, coeval gastropod faunas are found in the in-board Alexander terrane of southeastern Alaska. New collectionss from early Norian strata on Kuiu Island, southeastern Alaska (Alexander terrane) show that S. whaleni is also present in this terrane as well, in association with an essentially totally different gastropod fauna dominated by pleurotomaroids, trochoideans, and purpurinids. Explanation for the now known widespread distribution of this neritimorph species in a number of different terranes in eastern Panthalassa during Late Triassic times seems to be best attribtued to it having a relatively long-lived planktonic larval stage, allowing it to be relatively easily dispersed.
Report by: Robert B. Blodgett , Jiri Fryda
Age: Norian (early Norian)
Formation: Cornwallis Limestone
Occurrence(s)
No. Group Name Qty Notes
1 Snails Spinidelphinulopsis whaleni Blodgett, Fryda, and Stanley, 2001 specimens from this locality shown in Fig. 3A-E