Siderophore production of African dust microorganisms over Trinidad and Tobago

Iron (Fe) deposition from African dust has been implicated in a variety of environmental impacts on downwind terrestrial and marine ecosystems throughout the Caribbean. The most abundant form of Fe in African dust is Fe^III, which is often not bioavailable. The objective of this study was to determine to what degree microorganisms isolated from African dust collected in Trinidad and Tobago are capable of producing siderophores that mobilize bioavailable Fe into the environment. Aerosol samples were collected for microbial analyses during African dust conditions in the source region (Mali) and downwind sites (Trinidad and Tobago). Microbial community fingerprints, obtained by means of terminal restriction fragment length polymorphism analysis, were compared among aerosol samples and possible Trinidadian sources of locally aerosolized microorganisms (sea water and soils). Ordination of the fingerprint data revealed similarities between aerosols from the source region and the aerosols and soils of downwind regions. Aerosol isolates from the downwind sites were screened for siderophore production using a modified chrome azurol-S (CAS) assay. Twenty-five percent of isolates tested that were sampled under non-dust conditions and 65% of African dust isolates produced at least one type of siderophore; among African dust isolates, all known classes of siderophores were produced. These data support African dust microorganism siderophore production as a viable mechanism by which Fe bioavailability may be increased in downwind locations, given appropriate conditions for microbial proliferation.