By J. L. Wray (auth.), Dr. Donald F. Toomey, Dr. Matthew H. Nitecki (eds.)
Prior to the third overseas Symposium on Fossil Algae, held in Golden, Colorado in August of 1983, a 3-day fieldtrip targeting contemporary algal distribution in southern Florida was once led by means of Robert N. Ginsburg and his affiliates from Miami. A post-symosium fieldtrip to the West Texas-southern New Mexico sector used to be led through Don Toomey and Jack Babcock. This fieldtrip tested Precambrian and Paleozoic algal carbonates in a zone characterised via amazing outcrop exposures, and incorporated the well-known Permian Reef advanced. The Toomey-Babcock fieldtrip ended in a special fieldguide released through the Colorado tuition of Mines (1983), and issued to all contributors of the symposium. The symposium itself used to be held from August 15 via Augsut 17 at the campus of the Colorado institution of Mines the place Professor J. Harlan Johnson, to whose reminiscence this quantity is devoted, spent lots of his profession learning fossil algae. The symposium classes have been held for three days, and through that point forty papers have been offered and mentioned. A I-day fieldtrip, led through John L. Wray, to envision overdue Paleozoic phylloid algal carbonates uncovered within the close by Rocky Mountains, concluded the formal meetings.
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Extra resources for Paleoalgology: Contemporary Research and Applications
32 33 34 35 36 37 38 42 43 44 45 46 47 48 49 50 51 52 HJH 83 Fig. 3. J. Hofmann Fig. 4A,B. 1 Ga sequences. Little Dal Group, Mackenzie Mountains, Northwest Territories, Canada (Locality 1; = section 76AC-2 in Hofmann and Aitken 1979, Figs. 5W). A Note wide range of shape and size of Tawuia specimens associated with small and large Chuaria specimens. Geol. Surv. Canada, hypotype 66185 (large curved specimen at lower left). B Juxtaposed individuals of Tawuia dalensis and Chuaria circularis. ). Geol.
2B) <1 Fig. 8. ) with a preferred orientation (compare with Monty 1976, Fig. 15). Scale bar = 2 mm Fig. 9. Thin section photomicrograph of lamination in a stromatolite dome showing the alternation of the two types of laminae. The wider, lighter bands contain threads with a reticulate pattern that often show a preferred orientation (arrowed). The thin dark bands have prostrate threads. Several sediment rich laminae occur (S). Field of view is 17 mm wide V A Stromatolite Built by a Phormidium-Like Alga 47 Fig.
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