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Palaeoecology and sedimentology of the Achanarras fish bed of the Middle Old Red Sandstone, Scotland

Published online by Cambridge University Press:  03 November 2011

Nigel H. Trewin
Nigel H. Trewin
Affiliation:
Department of Geology and Mineralogy, Marischal College,University of Aberdeen, Aberdeen AB9 1AS, Scotland.
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Abstract

The Achanarras fish bed of Middle Devonian age in the Orcadian Basin was deposited in a large freshwater lake of variable productivity in which thermal stratification was normally developed. The fish bed consists of lacustrine laminites of organic, carbonate (dolomite and calcite) and clastic types. Carbonate laminae were precipitated as a result of photosynthetic activity and organic laminae were deposited following algal decay, clastic material was introduced by processes including overflow and interflow currents and wind transport.

The fish bed represents a major lacustrine transgression during a wetter climatic period which provided connections to other lakes and by overflow to the sea. Calcitic laminites represent the deepest water (>60 m) phase with greatest faunal variety due to availability of migration routes and stability of environments caused by lake overflow.

Initial lake transgression was characterised by Dipteras-dominated faunas which reappear as the last surviving fish during lake regression. Further regression resulted in the introduction of turbidites to the laminites.

Many fish were preserved following mass mortalities induced by algal blooms, mixing of waters by storms and lake overturn. Most of the fish inhabited shallow areas of the lake and drifted as rotting carcases to their final site of deposition. The fauna comprises a variety of benthonic and nektonic fish including predators, scavengers and omnivorous forms. Fish such as Coccosteus represented almost exclusively by adults may have bred outside the area of the lake.

Keywords

Devonianfaunalacustrinelaminitemass mortalityOrcadian Basintaphonomythermoclineturbidite
Type
Research Article
Information
Earth and Environmental Science Transactions of The Royal Society of Edinburgh , Volume 77 , Issue 1 , 1986 , pp. 21 - 46
Copyright
Copyright © Royal Society of Edinburgh 1986

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References

Allen, J. R. L. 1979. Old Red Sandstone fades in external basins, with particular reference to southern Britain. In House, M. R., Scrutton, C. T. & Bassett, M. G. (eds) The Devonian System, 65–80. SPEC PAP PALAEONTOL 23, 65–80.Google Scholar
Anderson, R. V. & Kirkland, D. W. 1960. Origin, varves and cycles of Jurassic Todilto Formation, New Mexico. BULL AM ASSOC PET GEOL 44, 37–52.Google Scholar
Armstrong, M. 1977. The Old Red Sandstone of Easter Ross and the Black Isle. In Gill, G. (ed.) The Moray Firth area geological studies, 25–34. Inverness Field Club.Google Scholar
Beadle, L. C. 1981. The inland waters of tropical Africa. An introduction to tropical limnology, 2nd. edn. London: Longman.Google Scholar
Béland, P. & Arsenault, M. 1985. Scauménellisation de l'Acanthodii Trazeugacanthus affinis (Whiteaves) de la formation d'Escuminac (Dévonian supérieur de Miguasha, Québec): révision du Scaumanella mesacanthi Graham-Smith. CAN J EARTH SCI 22, 514–24.CrossRefGoogle Scholar
Bradley, W. H. 1929. The varves and climate of the Green River epoch. PROF PAP U S GEOL SURV 168.Google Scholar
Chaloner, W. G. & Macdonald, P. 1980. Plants invade the land. London: HMSO.Google Scholar
Crampton, C. B. & Carruthers, R. G. 1914. The geology of Caithness. MEM GEOL SURV SCOTLAND.Google Scholar
Donovan, R. N. 1971. The geology of the coastal tract near Wick, Caithness. Unpublished Ph.D. thesis Newcastle upon Tyne University.Google Scholar
Donovan, R. N. 1973. Basin margin deposits of the Middle Old Red Sandstone at Dirlot, Caithness. SCOTT J GEOL 9, 203–11.Google Scholar
Donovan, R. N. 1975. Devonian lacustrine limestones at the margin of the Orcadian Basin, Scotland. J GEOL SOC 131, 489–510.CrossRefGoogle Scholar
Donovan, R. N. 1980. Lacustrine cycles, fish ecology and stratigraphic zonation in the Middle Devonian of Caithness. SCOTT J GEOL 16, 35–50.Google Scholar
Donovan, R. N. & Collins, A. 1978. Mound structures from the Caithness Flagstones (Mid. Dev.) northern Scotland. J SEDIMENT PETROL 48, 171–4.Google Scholar
Donovan, R. N. & Foster, R. J. 1972. Subaqueous shrinkage cracks from the Caithness Flagstone Series (Middle Devonian) of north east Scotland. J SEDIMENT PETROL 42, 309–17.Google Scholar
Donovan, R. N., Foster, R. J. & Westoll, T. S. 1974. A stratigraphical revision of the Old Red Sandstone of north-eastern Caithness. TRANS R SOC EDINBURGH 69, 167–201.CrossRefGoogle Scholar
Fannin, N. G. T. 1969. Stromatolites from the Middle Old Red Sandstone of western Orkney. GEOL MAG 106, 77–88.CrossRefGoogle Scholar
Forey, P. L. & Gardiner, B. G. 1981. J. A. Moy-Thomas and his association with the British Museum (Natural History). BULL BR MUS NAT HIST (GEOL) 35, 131–44.Google Scholar
Forster-Cooper, C. 1937. The Middle Devonian fish fauna of Achanarras. TRANS R SOC EDINBURGH 59, 223–39.CrossRefGoogle Scholar
Fouch, T. D. & Dean, W. E. 1982. Lacustrine and associated clastic depositional environments. In Scholle, P. A. & Spearing, D. (eds) Sandstone Depositional Environments, 87–113. AM ASSOC PET GEOL MEM 31.Google Scholar
Friend, P. F. 1969. Tectonic features of Old Red Sandstone sedimentation in North Atlantic borders. AM ASSOC PET GEOL MEM 12, 707–10.Google Scholar
Friend, P. F. 1981. Devonian sedimentary basins and deep faults of the northernmost Atlantic borderlands. MEM CAN SOC PET GEOL 7, 149–65.Google Scholar
Graham-Smith, W. 1935. Scaumanella mesacanthi, gen. et sp. n., a peculiar organism from the Upper Devonian of Scaumenac Bay, P.Q., Canada. ANN MAG NAT HIST (10) 15, 473–6.CrossRefGoogle Scholar
Grande, L. 1980. Paleontology of the Green River Formation, with a review of the fish fauna. BULL GEOL SURV WYOMING 63.Google Scholar
Hamilton, R. F. M. & Trewin, N. H. 1985. Excursion guide to the Devonian of Caithness, 1–36. Petroleum Exploration Society of Great Britain, Aberdeen Branch.Google Scholar
Hemmings, S. K. & Rostron, J. 1972. A multivariate analysis of measurements on the Scottish Middle Old Red Sandstone antiarch fish genus Pterichthyodes Bleeker. BIOL J LINN SOC 4, 15–28.CrossRefGoogle Scholar
Hesselbo, S. & Trewin, N. H. 1984. Deposition, diagenesis and structures of the Cheese Bay shrimp bed, Lower Carboniferous, East Lothian. SCOTT J GEOL 20, 281–96.CrossRefGoogle Scholar
House, M. R., Richardson, J. B., Chaloner, W. G., Allen, J. R. L., Holland, C. H. & Westoll, T. S. 1977. A correlation of Devonian rocks of the British Isles. GEOL SOC LOND SPEC REP 8.Google Scholar
Hsu, K. J. & Kelts, K. 1978. Late Neogene chemical sedimentation in the Black Sea. In Matter, A. & Tucker, M. E. (eds) Modern and ancient lake sediments, 129–45. SPEC PUBL INT ASSOC SEDIMENTOL 2.Google Scholar
Jarvik, E. 1948. On the morphology and taxonomy of the Middle Devonian osteolepid fishes of Scotland. K SVENSKA VETENSKAKAD HANDL (3) 25, 1–301.Google Scholar
Jarvik, E. 1980. Basic structure and evolution of the vertebrates, vol. 1. London: Academic Press.Google Scholar
Kevan, P. G., Chaloner, W. G. & Savile, D. B. O. 1975. Interrelationships of early terrestrial arthropods and plants. PALAEONTOLOGY 18, 391–417.Google Scholar
Miles, R. S. 1967. The acanthodian fishes of the Devonian Plattenkalk of the Paffrath Trough in the Rhineland. ARK FOR ZOOL 19 (9), 147–94.Google Scholar
Miles, R. S. 1969. Features of placoderm diversification and the evolution of the arthrodire feeding mechanism. TRANS R SOC EDINBURGH 68, 123–70.CrossRefGoogle Scholar
Miles, R. S. 1976. Observations on the ptyctodont fish, Rhamphodopsis Watson. J LINN SOC (ZOOL) 47, 99–120.CrossRefGoogle Scholar
Miles, R. S. & Westoll, T. S. 1968. The placoderm fish Coccosteus cuspidatus Miller ex Agassiz from the Middle Old Red Sandstone of Scotland. Pt. 1. Descriptive morphology. TRANS R SOC EDINBURGH 67, 373–476.CrossRefGoogle Scholar
Moy-Thomas, J. A. & Miles, R. S. 1971. Palaeozoic Fishes, 2nd edn. (revised by R. S. Miles). London: Chapman and Hall.Google Scholar
Müller, G. & Wagner, F. 1978. Holocene carbonate evolution in Lake Balaton (Hungary): a response to climate and impact of man. In Matter, A. & Tucker, M. E. (eds) Modern and ancient lake sediments, 57–81. SPEC PUBL INT ASSOC SEDIMENTOL 2.Google Scholar
Mykura, W. 1976. British Regional Geology. Orkney and Shetland. Edinburgh: HMSO.Google Scholar
Mykura, W. 1983. Old Red Sandstone. In Craig, G. Y. (ed.) Geology of Scotland, 205–51. Edinburgh: Scottish Academic Press.Google Scholar
Olsen, P. E., Remington, C. L., Cornet, B. & Thomson, K. S. 1978. Cyclic change in Late Triassic lacustrine communities. SCIENCE 201, 729–33.CrossRefGoogle ScholarPubMed
Ørvig, T. 1960, 1961. New finds of Acanthodians, Arthrodires, Crossopterygians, Ganoids and Dipnoans in the Upper Middle Devonian Calcareous Flags (Oberer Plattenkalk) of the Bergisch Gladbach–Paffrath Trough. PALAONTOL Z 34, 295–335 & 35, 10–27.CrossRefGoogle Scholar
Pennington, J. J. 1975. The geology of the Argyll field. In Woodland, A. W. (ed.) Petroleum and the continental shelf of north-west Europe, vol. 1, Geology, 285–91. Barking, Essex: Applied Science Publishers.Google Scholar
Pollard, J. E., Steel, R. J. & Undersrud, E. 1982. Facies sequences and trace fossils in lacustrine/fan delta deposits, Hornelen Basin (M. Devonian), Western Norway. SEDIMENT GEOL 32, 63–87.Google Scholar
Rayner, D. H. 1963. The Achanarras limestone of the Middle Old Red Sandstone, Caithness. PROC YORKSHIRE GEOL SOC 34, 117–38.CrossRefGoogle Scholar
Read, H. H. 1923. The geology of the country around Banff, Huntly and Turriff. MEM GEOL SURV SCOTLAND.Google Scholar
Richardson, J. B. 1965. Middle Old Red Sandstone spore assemblages from the Orcadian Basin, north-east Scotland. PALAEONTOLOGY 7, 559–605.Google Scholar
Rolfe, W. D. I. 1980. Early terrestrial vertebrate faunas. In Panchen, A. L. (ed.) The terrestrial environment and the origin of land vertebrates, 117–157. London: Academic Press.Google Scholar
Saxon, J. 1975. The fossil fishes of the North of Scotland, 2nd edn. Thurso: John Humphries, Caithness Books.Google Scholar
Schafer, W. 1972. Ecology and palaeoecology of marine environments. Edinburgh: Oliver & Boyd.Google Scholar
Smith, A. G., Briden, J. C. & Drewry, G. E. 1973. Phanerozoic world maps. In Hughes, N. F. (ed.) Organisms and continents through time, 1–42. SPEC PAP PALAEONTOL 12.Google Scholar
Smith, J. 1909. Upland fauna of the Old Red Sandstone of Carrick, Ayrshire. Kilwinning: A. W. Cross.Google Scholar
Sturm, M. & Matter, A. 1978. Turbidites and varves in Lake Brienz (Switzerland): deposition of clastic detritus by density currents. In Matter, A. & Tucker, M. E. (eds) Modern and ancient lake sediments, 147–68. SPEC PUBL INT ASSOC SEDIMENTOL 2.Google Scholar
Thomson, G. 1896. The Enzie–a field for the geologist. TRANS NORTHERN ASSOC LIT SCI SOC 2, 54–9.Google Scholar
Thomson, K. S. 1969. The biology of the lobe-finned fishes. BIOL REV 44, 91–154.Google Scholar
Thomson, K. S. 1975. On the biology of cosmine. PEABODY MUS NAT HIST BULL 40, 1–59.Google Scholar
Thomson, K. S. 1980. The ecology of Devonian lobe-finned fishes In Panchen, A. L. (ed.) The terrestrial environment and the origin of land vertebrates, 187–222. SYST ASSOC SPEC VOL 15.Google Scholar
Traquair, R. H. 1888. Notes on the nomenclature of the fishes of the Old Red Sandstone of Great Britain. GEOL MAG 5, 507–17.CrossRefGoogle Scholar
Traquair, R. H. 1890. On the fossil fishes at Achanarras Quarry, Caithness. ANN MAG NAT HIST (6) 6, 479–86.Google Scholar
Traquair, R. H. 1892. On the British species of Asterolepidae. PROC R PHYS SOC EDINBURGH 11, 283–6.Google Scholar
Traquair, R. H. 1894. Achanarras revisited. PROC R PHYS SOC EDINBURGH 12, 279–86.Google Scholar
Traquair, R. H. 1894–1914. A monograph of the fishes of the Old Red Sandstone of Britain. PALAEONTOGR SOC MONOGR 1904 (2), 91–118.Google Scholar
Traquair, R. H. 1909. Note on the fossil fishes from the Niandt limestone, one-eighth of a mile S. W. of the mouth of Forse Burn. MEM GEOL SURV SUMM PROG 1908, 92–3.Google Scholar
Trewin, N. H. 1976a. Isopodichnus in a trace fossil assemblage from the Old Red Sandstone. LETHAIA 9, 29–37.Google Scholar
Trewin, N. H. 1976b. Correlation of the Achanarras and Sandwick fish beds, Middle Old Red Sandstone, Scotland, SCOTT J GEOL 12, 205–8.CrossRefGoogle Scholar
Van Houten, F. B. 1962. Cyclic sedimentation and the origin of analcime-rich upper Triassic Lockatong Formation, westcentral New Jersey and adjacent Pennsylvania. AM J SCI 260, 561–76.Google Scholar
Vincent, C. E., Davies, T. D. & Beresford, A. K. C. 1979. Recent changes in the level of Lake Naivasha, Kenya, as an indicator of equatorial westerlies over East Africa. CLIM CHANGE 2, 175–89.CrossRefGoogle Scholar
von, Wahlert G. 1965. The role of ecological factors in the origin of higher levels of organisation. SYST ZOOL 14, 288–300.Google Scholar
Waldman, M. 1971. Fish from the freshwater Lower Cretaceous of Victoria, Australia, with comments on the palaeo-environment. SPEC PAP PALAEONTOL 9, 1–124.Google Scholar
Watson, D. M. S. 1937. The acanthodian fishes. PHIL TRANS R SOC LONDON B228, 49–146.Google Scholar
Westoll, T. S. 1936. On the structure of the dermal ethmoid shield of Osteolepis. GEOL MAG 73, 157–71.Google Scholar
Westoll, T. S. 1951. The vertebrate-bearing strata of Scotland. In Swinton, H. E. (ed.) The correlation of continental vertebrate-bearing rocks, 5–21. PROC 18TH INT GEOL CONGR LONDON 1948, 11.Google Scholar
Westoll, T. S. 1958. The origin of continental vertebrate faunas. TRANS GEOL SOC GLASGOW 23, 1–27.Google Scholar
Wilson, M. V. H. 1980. Eocene lake environments; depth and distance-from-shore variation in fish, insect and plant assemblages. PALAEOGEOGR PALAEOCLIMATOL PALAEOECOL 32, 21–44.Google Scholar