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Economic Geology; July 2001; v. 96; no. 4; p. 885-890; DOI: 10.2113/96.4.885
© 2001 Society of Economic Geologists
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Scientific Communications

BACTERIA WERE RESPONSIBLE FOR THE MAGNITUDE OF THE WORLD-CLASS HYDROTHERMAL BASE METAL SULFIDE OREBODY AT NAVAN, IRELAND

Anthony E. Fallick

Scottish Universities Environmental Research Centre, Rankine Avenue, East Kilbride, Glasgow G75 0QF, Scotland

John H. Ashton

Outokumpu Tara Mines Ltd, Knockumber, Navan, County Meath, Ireland

Adrian J. Boyce{dagger}, Rob M. Ellam and Michael J. Russell

Scottish Universities Environmental Research Centre, Rankine Avenue, East Kilbride, Glasgow G75 0QF, Scotland

{dagger} Corresponding author: e-mail, a.boyce{at}suerc.gla.ac.uk

We report sulfur and lead isotope analyses of mine concentrates from Navan, the largest zinc deposit in Ireland. These samples, each representing up to a million tonnes of ore, show very limited isotopic variation, with mean {delta}34S = –13.6 ± 2 per mil (n = 20), and galena concentrate mean 206Pb/204Pb = 18.19 ± 0.03 (n = 7). Calculations suggest >90 percent of the Navan sulfides were derived through bacteriogenic reduction of Mississippian seawater sulfate, whereas metals were acquired from a local, orogenic crustal source beneath the orebody. Enhanced bacterial activity was fundamental to ore deposition at Navan: no bacteria, no giant ore deposit.




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