Gold cycle
Biogeochemical cycle
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Through Gold, Lithosphere and Hydrosphere
Lithosphere
The lithosphere is the dominant reservoir of gold, containing an estimated 2.6 × 1013 Mg. Today, gold exists primarily as electrum, in hard rock deposits like tellurides, and as particles in placers in Earth's crust. Gold cycling starts with the microbial weathering of gold-bearing rocks and minerals which mobilizes gold in the environment via release of elemental gold and solubilization. The Witwatersrand gold deposits host approximately 30% of the world's gold resources, a large proportion of which is directly associated with organic carbon derived from microbial mats. Gold ore has been mined in many countries, including Japan, India, Spain, Yugoslavia, South Africa, Australia, the United States of America, Canada, Colombia, Mexico, and Brazil.
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Ocean
The ocean reservoir contains an estimated 5.6 × 109 Mg of gold and oceanic gold concentration is about 4 ng Au/L with higher values in some coastal waters. Au(I/III)-ions and Au(0)-colloids are unstable under surface conditions in aqueous solutions and commonly form ligand complexes with substances excreted by microorganisms. Similar to silver and mercury, these mobile Au(I/III)-complexes are toxic in nature. Some bacteria that live in biofilms on placer gold particle surfaces deal with this toxicity by precipitating Au(I/III)-complexes which leads to the biomineralization of gold. Other archaea, iron-reducing bacteria, and some sulfate-reducing bacteria have developed methods to regulate and detoxify their immediate environment when Au(III)-ions are present at toxic levels. Iron- and sulfur-oxidizing litho-autotrophic bacteria break down gold-hosting sulfide minerals, releasing gold as alloy particles or Au(I)-thiosulfate complexes. Eventually, gold nanoparticles released by these processes undergo transformation, are dispersed in oceans, or accumulate in sediments.
Atmosphere
The atmosphere is the smallest reservoir of gold, containing an estimated 370 Mg. The most volatile gold compounds are Au2Cl6, which may occur in volcanic gases, and AuF3.
Influences and interactions of other biogeochemical cycles
The biogeochemical cycle of gold is affected by the carbon, nitrogen, sulfur, and iron cycles. Decomposition of organic carbon under anoxic conditions creates a wide range of organic intermediates, e.g., organic acids, that are important determinants of gold mobility. Key microbial processes in the nitrogen cycle can be influenced by gold and vice versa; for example autotrophic denitrifying bacteria can destabilize Au-complexes and may play a role in gold cycling. Overall, it is likely that gold mobility, biomineralization, and ore forming processes are impacted by the reactive nitrogen-containing compounds. Gold is commonly incorporated in iron-sulfides and adsorbed by Fe(III)-oxyhydroxide precipitates; oxidation of gold-bearing pyrite can lead to the mobilization of soluble gold complexes.
Ancient Earth
Throughout Earth's history, the interplay of gold, microorganisms, and physicochemical conditions such as pH and redox potential have led to the aggregation of gold particles to form grains and nuggets. Cyanobacteria in shallow surface waters on early anoxic Earth accumulated gold complexes dissolved in the water and geochemical modeling indicates that gold solubility in ancient waterbodies was much higher than today. Experimental evidence suggests that on early Earth, Fe(III)-reducing extremophiles and sulfate-reducing bacteria may have been contributed to formation of gold-bearing deposits.