Abstract
The symbiotic partnership of plants and fungi was a critical means of nutrient uptake during colonization of the terrestrial surface. The Lower Devonian Rhynie Chert shows evidence for extensive phosphorus mobilization in plant debris that was pervasively colonized by fungi. Sandy sediment entrapped with fungi-rich phytodebris contains grains of the phosphate mineral monazite which exhibit alteration to highly porous and leached surfaces. Mixed manganese-iron oxide
precipitates contain up to 2 % P2O5. The mobilization of Mn, Fe and P are all features of mycorrhizal nutrient concentration. However, the ecosystem was also exposed to toxic elements from hot spring hydrothermal activity. The oxide precipitates include titanium and iron-titanium oxide which sequestered potentially toxic tungsten and antimony. Abundant pyrite framboids in the Rhynie Chert indicate that plant decomposition included microbial sulphate reduction. This caused the removal of some of the arsenic from the groundwaters into the pyrite, which reduced toxicity while leaving enough for putative arsenic metabolism. These relationships show the mineral component of the ecosystem modified the geochemistry of ambient waters.
precipitates contain up to 2 % P2O5. The mobilization of Mn, Fe and P are all features of mycorrhizal nutrient concentration. However, the ecosystem was also exposed to toxic elements from hot spring hydrothermal activity. The oxide precipitates include titanium and iron-titanium oxide which sequestered potentially toxic tungsten and antimony. Abundant pyrite framboids in the Rhynie Chert indicate that plant decomposition included microbial sulphate reduction. This caused the removal of some of the arsenic from the groundwaters into the pyrite, which reduced toxicity while leaving enough for putative arsenic metabolism. These relationships show the mineral component of the ecosystem modified the geochemistry of ambient waters.
Original language | English |
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Article number | e2022GC010647 |
Number of pages | 15 |
Journal | Geochemistry, Geophysics, Geosystems |
Volume | 23 |
Issue number | 12 |
Early online date | 16 Dec 2022 |
DOIs | |
Publication status | Published - 16 Dec 2022 |
Bibliographical note
AcknowledgementsJGTA is supported by the Natural Environment Research Council (grant NE/T003677/1). Samples were archived at the University of Aberdeen by N.H. Trewin, S.R. Fayers and C.M. Rice. Skilled technical support was provided by J. Johnston, J. Bowie, W. Ritchie and C. Taylor. We are grateful for the comments of two reviewers which improved the manuscript.
Data Availability Statement
Data reported in Tables 1–3 is managed by the University of Aberdeen (https://doi.org/10.20392/eed913d7-12eb-4c5d-a276-e1920eecd43f).Keywords
- Rhynie Chert
- Devonian
- Scotland
- Fungi
- Arsenic
- Phosphorus
- fungi
- arsenic
- phosphorus
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Data tables for mineral phases, Rhynie Chert
Parnell, J. (Creator), University of Aberdeen, 2022
DOI: 10.20392/eed913d7-12eb-4c5d-a276-e1920eecd43f
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Providing an evidence base for a maximum permissible level of inorganic arsenic in rice
Jörg Feldmann (Participant), Andrew Alexander Meharg (Participant), Andrea Raab (Participant) & Eva Maria Krupp (Participant)
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