@article{fdi:010094061, title = {{E}nvironmental contamination by metals, metalloids, and cyanides in the historic and active {ASGM} area of {K}okumbo in {C}{\^o}te d'{I}voire}, author = {{K}ouadio, {K}.{B}. and {R}esongles, {E}l{\'e}onore and {A}houssi, {K}.{E}. and {O}uattara, {Z}. and {K}onat{\'e}, {I}. and {F}ayol, {N}. and {B}orschneck, {D}. and {B}aratoux, {D}avid and {D}elpoux, {S}. and {D}omeau, {A}. and {M}arie, {M}. and {Y}ao, {K}.{A}. and {B}runeel, {O}dile}, editor = {}, language = {{ENG}}, abstract = {{I}n {C}{\^o}te d'{I}voire, despite an intense development of artisanal and small-scale gold mining ({ASGM}) activities in the last two decades, the environmental impacts of this activity are poorly documented. {T}his study aimed to document the concentrations of geogenic and exogenous contaminants potentially released by {ASGM} (metals and cyanides) in different sources (ore, mining wastes) and environmental compartments (soils, surface and ground waters, sediments) in the {K}okumbo area, part of the {A}u-rich {B}irimian greenstone belt. {A}lluvial ore material is enriched in various metal(oid)s ({A}s, {C}o, {C}u, {C}r, {F}e, {M}n, {N}i, {S}b, and {V}) compared to the average composition of the upper continental crust while other metals ({C}d, {P}b, {T}i, {Z}n) show no geochemical anomalies. {H}igh {H}g concentrations were found in cyanidation residues (up to 8.32 mg/kg) and sediments (up to 20.4 mg/kg) compared to unprocessed alluvial ores (0.06?±?0.01 mg/kg) indicating that {H}g used in amalgamation is the source of {H}g contamination. {C}yanidation residues contain up to 100 mg/kg of total cyanides but generally less than 3% are in the form of free cyanides, the most mobile and toxic form. {A}rsenic concentrations in water are low (