Subaqueous silicification of the contents of small ponds in an Early Devonian hot spring complex, Rhynie, Scotland

Nigel Harvey Trewin, Stephen Fayers, R. Kelman, R. Kelman

    Research output: Contribution to journalArticle

    59 Citations (Scopus)

    Abstract

    The Early Devonian Rhynie and Windyfield cherts of northeast Scotland originated as siliceous sinters deposited by hot springs. Silicification affected both subaerial and subaqueous environments, preserving a diverse terrestrial and freshwater biota. Cherts originally deposited in small shallow pools can be recognised on the basis of both texture and fossil content. Textures comprise clotted and microcoprolitic textures, bacterial coatings on plant axes that can be stromatolitic, and a variety of bacterial and fungal meshworks. The crustacean Lepidocaris, the euthycarcinoid Heterocrania, the charophyte alga Palaeonitella, and chytrid fungi are typical elements of the aquatic biota. Observations of modern hot springs in Yellowstone National Park, Wyoming, U.S.A., demonstrate that shallow ponds and streams on low-angle outwash areas and dormant vent orifices provide suitable environmental analogues. Textures comparable to those described from Rhynie are recorded from Yellowstone sinters, but examples of the rapid and complete silicification of delicate organic structures as seen in a few of the Rhynie chert beds have not been noted. Petrographic textures comparable to those seen in the cherts of freshwater origin from Rhynie occur in modern stream sinters at Yellowstone, where they form from waters at 20-28degreesC and with a pH of 8.7. This similarity occurs despite differences in environment at Yellowstone, such as the oxidizing surface environment, water table fluctuations, complex modern vegetation, fixing of silica by diatoms, and climatic extremes. Thus there are close similarities between textures seen in the Rhynie cherts and Yellowstone sinters deposited in freshwater pools and streams by hot springs.

    Original languageEnglish
    Pages (from-to)1697-1712
    Number of pages15
    JournalCanadian Journal of Earth Sciences
    Volume40
    Issue number11
    DOIs
    Publication statusPublished - Nov 2003

    Keywords

    • Yellowstone-National-Park
    • land plants
    • chert
    • Aberdeenshire
    • fossilization
    • preservation
    • sinter

    Cite this

    Subaqueous silicification of the contents of small ponds in an Early Devonian hot spring complex, Rhynie, Scotland. / Trewin, Nigel Harvey; Fayers, Stephen; Kelman, R.; Kelman, R.

    In: Canadian Journal of Earth Sciences, Vol. 40, No. 11, 11.2003, p. 1697-1712.

    Research output: Contribution to journalArticle

    Trewin, Nigel Harvey ; Fayers, Stephen ; Kelman, R. ; Kelman, R. / Subaqueous silicification of the contents of small ponds in an Early Devonian hot spring complex, Rhynie, Scotland. In: Canadian Journal of Earth Sciences. 2003 ; Vol. 40, No. 11. pp. 1697-1712.
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    abstract = "The Early Devonian Rhynie and Windyfield cherts of northeast Scotland originated as siliceous sinters deposited by hot springs. Silicification affected both subaerial and subaqueous environments, preserving a diverse terrestrial and freshwater biota. Cherts originally deposited in small shallow pools can be recognised on the basis of both texture and fossil content. Textures comprise clotted and microcoprolitic textures, bacterial coatings on plant axes that can be stromatolitic, and a variety of bacterial and fungal meshworks. The crustacean Lepidocaris, the euthycarcinoid Heterocrania, the charophyte alga Palaeonitella, and chytrid fungi are typical elements of the aquatic biota. Observations of modern hot springs in Yellowstone National Park, Wyoming, U.S.A., demonstrate that shallow ponds and streams on low-angle outwash areas and dormant vent orifices provide suitable environmental analogues. Textures comparable to those described from Rhynie are recorded from Yellowstone sinters, but examples of the rapid and complete silicification of delicate organic structures as seen in a few of the Rhynie chert beds have not been noted. Petrographic textures comparable to those seen in the cherts of freshwater origin from Rhynie occur in modern stream sinters at Yellowstone, where they form from waters at 20-28degreesC and with a pH of 8.7. This similarity occurs despite differences in environment at Yellowstone, such as the oxidizing surface environment, water table fluctuations, complex modern vegetation, fixing of silica by diatoms, and climatic extremes. Thus there are close similarities between textures seen in the Rhynie cherts and Yellowstone sinters deposited in freshwater pools and streams by hot springs.",
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