Trace Element Geochemistry in the Earliest Terrestrial Ecosystem, the Rhynie Chert
Trace Element Geochemistry in the Earliest Terrestrial Ecosystem, the Rhynie Chert
复制标题
最早陆生生态系统的微量元素地球化学
DOI:
10.1029/2022gc010647
复制
发表时间:
2022-12
期刊:
影响因子:
3.7
通讯作者:
J. Parnell;T. O. Akinsanpe;J. Armstrong;A. Boyce;J. Still;S. Bowden;David Clases;Raquel González de Vega;J. Feldmann
中科院分区:
文献类型:
--
作者:
J. Parnell;T. O. Akinsanpe;J. Armstrong;A. Boyce;J. Still;S. Bowden;David Clases;Raquel González de Vega;J. Feldmann
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 sulfate 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.