@article{fdi:010082216, title = {{D}ust arriving in the {A}mazon basin over the past 7,500 years came from diverse sources}, author = {{N}ogueira, {J}. and {E}vangelista, {H}. and {V}aleriano, {C}. {D}. and {S}ifeddine, {A}bdelfettah and {N}eto, {C}. and {V}az, {G}. and {M}oreira, {L}. {S}. and {C}ordeiro, {R}. {C}. and {T}urcq, {B}runo and {A}niceto, {K}. {C}. and {N}eto, {A}. {B}. and {M}artins, {G}. and {B}arbosa, {C}. {G}. {G}. and {G}odoi, {R}. {H}. {M}. and {S}himizu, {M}. {H}.}, editor = {}, language = {{ENG}}, abstract = {{A} large amount of dust from the {S}ahara reaches the {A}mazon {B}asin, as observed with satellite imagery. {T}his dust is thought to carry micronutrients that could help fertilize the rainforest. {H}owever, considering different atmospheric transport conditions, different aridity levels in {S}outh {A}merica and {A}frica and active volcanism, it is not clear if the same pathways for dust have occurred throughout the {H}olocene. {H}ere we present analyses of {S}r-{N}d isotopic ratios of a lacustrine sediment core from remote {L}ake {P}ata in the {A}mazon region that encompasses the past 7,500 years before present, and compare these ratios to dust signatures from a variety of sources. {W}e find that dust reaching the western {A}mazon region during the study period had diverse origins, including the {A}ndean region and northern and southern {A}frica. {W}e suggest that the {S}ahara {D}esert was not the dominant source of dust throughout the vast {A}mazon basin over the past 7,500 years. {M}ineral dust deposited over the western {A}mazon region through the {H}olocene is not limited to a {S}aharan source and instead has diverse origins, according to geochemical fingerprinting of dust from lacustrine deposits.}, keywords = {{BRESIL} ; {AMAZONIE} ; {PATA} {LAC}}, booktitle = {}, journal = {{C}ommunications {E}arth and {E}nvironment}, volume = {2}, numero = {1}, pages = {5 [11 ]}, year = {2021}, DOI = {10.1038/s43247-020-00071-w}, URL = {https://www.documentation.ird.fr/hor/fdi:010082216}, }