The Rhynie chert contains exceptionally preserved material covered by an overlying volcanic deposit. Most of the fossil bed has primitive plants (which had water-conducting cells and sporangia, but no true leaves), along with arthropods, lichens, algae and fungi.
Second, these cherts are famous for their exceptional state of preservation, with individual cell walls easily visible in polished specimens. Stomata have been counted and lignin remnants detected in the plant material. The book lungs of some early spiders can be seen in cross-sections. Fungal hyphae can be seen entering plant material, acting as decomposers and mycorrhizal symbionts.
History of researchEdit
The chert was discovered by William Mackie while mapping the western margin of the Rhynie basin in 1910–1913.
Since 1980, the chert has been examined by the Münster group, and from 1987 by Aberdeen University. They showed the chert was indeed produced by a hot spring setting. Cores were drilled in 1988 and 1997.
Conditions of formationEdit
The chert was formed when silica-rich water from volcanic springs rose and rapidly petrified the early terrestrial ecosystem in situ. Organisms are petrified that way by hot springs today, although that quality of preservation has not been found in recent deposits. Hot springs, with temperatures between 90 to 120 °C (194 to 248 °F), were active; the water had probably cooled to under 30 °C (86 °F) before it reached the fossilised organisms. The deposits are interbedded with sands, shales and tuffs, which speaks of local volcanic activity. Deposition was very rapid.
- "Rhynie Chert Learning Resource". University of Aberdeen.
- Rice C.M.; et al. (1995). "A Devonian auriferous hot spring system, Rhynie, Scotland". Journal of the Geological Society, London. 152: 229–250. doi:10.1144/gsjgs.152.2.0229.
- Natural Environment Research Council
- Whalley, Paul; Jarzembowski, Ed (1981). "A new assessment of Rhyniella, the earliest known insect, from the Devonian of Rhynie, Scotland". Nature. 291: 317. doi:10.1038/291317a0. Cite has empty unknown parameter:
- Engel, Michael S.; Grimaldi, DA (2004). "New light shed on the oldest insect". Nature. 427 (6975): 627–30. doi:10.1038/nature02291. PMID 14961119.
- Trewin N.H. (2003). "History of research on the geology and palaeontology of the Rhynie area, Aberdeenshire, Scotland". Transactions of the Royal Society of Edinburgh Earth Sciences. 94. doi:10.1017/S0263593300000699.
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- Trewin N.H. (2003). "Subaqueous silicification of the contents of small ponds in an early Devonian hot-spring complex, Rhynie, Scotland". Canadian Journal of Earth Sciences. 40 (11): 1697–1712. doi:10.1139/e03-065. Retrieved 2008-05-15. Unknown parameter
- Trewin N.H. (2004). "Correlation of the early Devonian Rhynie chert beds between three boreholes at Rhynie, Aberdeenshire". Scottish Journal of Geology. 40 (1): 73–81. doi:10.1144/sjg40010073. Unknown parameter
- Powell C.L.; Trewin, N. H.; Edwards, D. (2000). "Palaeoecology and plant succession in a borehole through the Rhynie cherts, Lower Old Red Sandstone, Scotland". Geological Society London Special Publications. 180: 439. doi:10.1144/GSL.SP.2000.180.01.23.
- Rice C.M. (2002). "Geological setting of the early Devonian Rhynie cherts, Aberdeenshire, Scotland: an early terrestrial hot spring system" (abstract). Journal of Geological Society. 159 (2): 203. doi:10.1144/0016-764900-181. Retrieved 2008-05-15. Unknown parameter
- Wellman, Charles H. (2006). "Spore assemblages from the Lower Devonian 'Lower Old Red Sandstone' deposits of the Rhynie outlier, Scotland". Transactions of the Royal Society of Edinburgh Earth Sciences. 97. doi:10.1017/S0263593300001449.
- Fayers S.R.; Trewin, Nigel H. (2003). "A review of the palaeoenvironments and biota of the Windyfield chert". Transactions of the Royal Society of Edinburgh Earth Sciences. 94. doi:10.1017/S0263593300000729.
- Contains useful reconstructions of both the plant associations, and the regional setting.