File:GSG GLA FIG 22 02.jpg: Difference between revisions

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|description={{en|1=Figure 22.2 Some of the fossil chelicerates from the Jamoytius horizon. a, ?aquatic scorpion Allopalaeophonus caledonicus x 2112 (after Petrunkevitch); b-d, eurypterids (water-scorpions, after Størmer); b, Slimonia acuminata x116; c, Hughmilleria lanceolata x112; d, Erettopterus [Pterygotus] bilobus, x1/6; e, early king crab Cyamocephalus loganensis x 2/3 (after Stormer). The eurypterids are rare at this horizon, but occur more abundantly at Shank Castle, Dunside.
|description={{en|1=Figure 22.2 Some of the fossil chelicerates from the Jamoytius horizon. a, ?aquatic scorpion ''Allopalaeophonus caledonicus'' x 2112 (after Petrunkevitch); b-d, eurypterids (water-scorpions, after Størmer); b, ''Slimonia acuminata'' x116; c, ''Hughmilleria lanceolata'' x112; d, ''Erettopterus'' [''Pterygotus''] ''bilobus'', x1/6; e, early king crab ''Cyamocephalus loganensis'' x 2/3 (after Stormer). The eurypterids are rare at this horizon, but occur more abundantly at Shank Castle, Dunside.
{{GSGGlasgow}}}}
{{GSGGlasgow}}}}
|date=2019-02-11 09:04:44
|date=2019-02-11 09:04:44

Revision as of 10:36, 11 February 2019

Summary

description
English: Figure 22.2 Some of the fossil chelicerates from the Jamoytius horizon. a, ?aquatic scorpion Allopalaeophonus caledonicus x 2112 (after Petrunkevitch); b-d, eurypterids (water-scorpions, after Størmer); b, Slimonia acuminata x116; c, Hughmilleria lanceolata x112; d, Erettopterus [Pterygotus] bilobus, x1/6; e, early king crab Cyamocephalus loganensis x 2/3 (after Stormer). The eurypterids are rare at this horizon, but occur more abundantly at Shank Castle, Dunside.
From: Lawson, J.D. and Weedon, D.S. (editors). 1992. Geological excursions around Glasgow & Girvan. Glasgow : Geological Society of Glasgow.
source Geological Society of Glasgow
author Geological Society of Glasgow

Licensing

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© 1992. Geological Society of Glasgow. All rights reserved. Published by the Geological Society of Glasgow. For all uses of the images please contact the Geological Society Glasgow. [1]

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