Reference Detail of

Report on Referred Fossils
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Stratigraphic range: Silurian? and Devonian
Kinds of fossils: Corals
Quadrangle or area: Upper Yukon River, Alaska
Shipment No.: A-60-28
Referred by: Brabb, Earl E.
Report prepared by: Oliver, William A., Jr.
Date: 01/05/1961

Collections 184A, 206, 203, and 204 (page 3 of request form) contain archaeocyathids and are of Cambrian age. The archaeocyathids are somewhat similar to corals in external form but can be easily differentiated in section. These will be reported on by another specialist.

Collections 71, 82, 211, and 631 contain no recognizable corals. These will be reported on by specialists in the fossil groups that are present.

Collections 48B contains abundant bryozoans, and coll. 83 and 632 contain a few. These will be reported on by a National Museum specialist if they are identifiable or if they contribute additional age data.

The following collections contain the corals indicated. Ages are based on the presence of certain structures in the scarce rugose corals and on the ranges of tabulate genera unless otherwise indicated.

Discussion: The tabulate genera Alveolites and Cladopora are limited to the Silurian and Devonian. In addition a moderate to large assemblage of Favosites and branching tabulate corals is indicative of the same age. So Silurian-Devonian is relatively easy to recognize on any decent sized collection of tabulate corals. However, these same corals cannot be used to differentiate between Silurian and Devonian or to recognized subdivisions of either, except in a very few places where species have been described and their ranges are well known.

Chain corals (Halysites, etc.) are often present in Silurian collections, but are not known in Devonian ones. Since they are absent from your collections I would suspect that most of them are Devonian, rather than Silurian.

Rugose corals (solitary or colonial horn corals) are of much more use in recognizing Silurian-Devonian subdivisions than are the tabulates. In the above collections, all of my finer age “guesses” are based on rugose coral genera which are limited to one system or series.

On the basis of this collection I would suggest the following for future consideration:
1. Collect tabulates as here, but recognize that these are of broad age value only.
2. Hunt for chain corals (Halysites, etc.) as these are all pre-Devonian.
3. Collect a variety of rugose corals where common, all possible ones where rare. If they are decently preserved they can be very good indices.

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60ABa 83 (6441-SD) , Eagle , Grayish-black, coarse-grained, cherty, fetid, massive limestone. The collecting area was mapped as alluvium by Mertie (1933, USGS Bull 836, pl. 7), but he reports (Ibid., p. 413, sample 28Mt 161, F and S no. 2063) a Middle Devonian fauna from a locality that plots very close to, if not at 60ABa 83. The fossils at 80ABa 83 include abundant rhynchonellid-like brachiopods, abundant Pelmatozoa columnals, and Favositid-like corals or bryozoa. They were collected along the north bank of the Tatonduk River, approx. 15.5 miles NNE of Eagle, Alaska. coords. (22.2, 18.0).
cyathophylloid horn coral
branching favositoid corals
Favosites sp.
echinoderm debris
60ABa 84B (6442-SD) , Eagle , North bank of Tatonduk River, 4,000 feet (river distance) upstream from mouth of Funnel Creek, 600 feet downstream from 60ABa 83, and more or less at the same stratigraphic horizon as 60ABa 83. Fauna and lithology similar to those of 60ABa 83 except that 60ABa 84B also has stromatoporoids.
cyathophylloid horn corals
Alveolites? sp.
Favosites sp.
branching favositoid corals
echinodermal debris
60ABa 192 (6443-SD) , Charley River , Lithology and fauna similar to those at 60ABa 83 and 60ABa 84B. Localities 60ABa 192, 60ABa 83 and 60ABa 84B are along strike and probably at approx. the same stratigraphic horizon. The beds at 60ABa 192 were mapped by Mertie (USGS Bull 836, pl. 7) as "Middle Devonian Limestone, shale, and chert". Mertie considered this unit slightly younger than the Salmontrout limestone. Charley River A-1 Quad. Along Funnel Creek about 1,200 feet (airline distance) upstream from mouth.
Macgeea? sp.
cyathophylloid horn coral
Alveolites sp.
Cladopora sp.
Favosites sp.
Pachypora sp.
Thamnopora sp.
stromatoporoid (massive)
echinodermal debris
60ABa 204 (6444-SD) , Charley River , Grayish-black limestone, largely recrystallized. Contains poorly preserved Pelmatozoa columnals and a coral or bryozoa. Charley River A-1 Quad.; along Funnel Creek, 2.4 miles (airline distance) upstream from mouth. [Description from A.R. Palmer E&R report of 2/16/65: NE1/4 sec. 5, T. 2 N., R. 23 E. - 2.4 mi. (airline) upstream from mouth of Funnel Creek.
Hexagonaria sp.
60ABa 632 (6445-SD) , Charley River , Grayish-black, fine- to coarse-grained limestone. Contains abundant and well-preserved fossils, including crinoid stems as large as 3/4" dia. atrypid brachiopods, bryozoa, favositid-like corals, and a gastropod. Charley River B-2 Quad.; west bank of Nation River, approx. 1.8 miles (airline) downstream from mouth of Hard Luck Creek.
Spongophyllum sp.
Favosites sp.
Thamnopora sp.
60ABa 1063 (6446-SD) , Charley River , Grayish-black, fine- to coarse-grained, fetid limestone. Contains abundant fossils including brachiopods, bryozoa or corals, and Pelmatozoa columnals. Mapped as Woodchopper volcanics (Middle Devonian) by Mertie (see USGS Bull 616, p. 78-60). Charley River B-5 quad.; north bank Yukon River opposite Woodchopper Roadhouse.(from original E&R report); [Dover & Miyaoka, 1988 has no locality description given, shown as locality 35 on map, lat./long based on digitization of map location: 65º21'54" N, 143º18'47". Collection from collections of Earl Brabb. Kept in the U.S. National Museum (Smithsonian Institution), Washington, D.C.
Favosites sp.
60ABa 1064 (6447-SD) , Charley River , Dark-gray, fine-grained limestone with brachiopods, Pelmatozoa columnals, bryozoa, and favositid-like corals. Mapped as Woodchopper volcanics (M. Dev.) by Mertie. Charley River B-5 quad.; south bank Yukon River, approx. 3.7 miles downstream from Woodchopper Roadhouse. [Shown as locality 36 on Sheet 2 of Dover & Miyaoka, 1988, but no locality description given. Collection kept in U.S. National Museum (Natural History), Smithsonian Institution, Washington, D.C. Collections of E.E. Brabb.]
amplexoid horn coral
cyathophylloid horn corals
ptenophylloid horn coral
indeterminate horn corals
Favosites sp.