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American Journal of Science, Vol. 309, October 2009, P.633-660; doi:10.2475/08.2009.01

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Elemental release rates from dissolving basalt and granite with and without organic ligands

E. M. Hausrath*,**, A. Neaman*** and S. L. Brantley*

* Department of Geosciences, The Pennsylvania State University, University Park, Pennyslvania 16802, USA
** Present address: Department of Geoscience, University of Nevada, Las Vegas, Nevada 89154, USA
*** Facultad de Agronomía, Pontificia Universidad Católica de Valparaíso, Casilla 4-D, Quillota, Chile

Elisabeth.Hausrath{at}unlv.edu

Bacteria, fungi, lichen and plants all produce organic acids, which can strongly affect weathering by increasing the solubility and mobility of elements. Leaching by organic acids may therefore produce trace element signatures which could record the presence of life in the rock record from early Earth. To elucidate this effect, long term column experiments were performed with powdered granite and basalt with and without 0.01 M citrate at pH=6 for 45 weeks. Both granite (8.44 x 10–13, 3.39 x 10–13) and basalt (2.94 x 10–14, 6.47 x 10–14) dissolution rates mol (Ca, Mg) (m–2 s–1 respectively) were enhanced in the presence of citrate relative to the organic-free controls: granite (3.17 x 10–14, 4.4 x 10–15) and basalt (1.01 x 10–14, 1.04 x 10–14). Enhanced release of individual elements in the presence of citrate was strongly correlated with the stability constant of the citrate-element complex. Elements which might be useful as biosignatures are those elements that showed a strong enrichment in the presence of citrate: Zr, Sc and Mn (basalt), V and Zn (granite), and Y, La, Ce, Th, Ti, Al, P, Pb, Ni and Fe (both basalt and granite). Release of these elements from the rock material in the columns is consistent with dissolution of apatite + Fe sulfides + Fe oxides + augite in basalt and apatite + sphene + hornblende in granite. Similar groups of elements have been reported to be enriched in organic-rich rivers, suggesting leaching of strongly-complexed elements could be useful as biosignatures and may have left mineralogical traces on early Earth.

Key Words: Basalt • Granite • Weathering • Citrate • Biosignature • Trace elements




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O. S. Pokrovsky, L. S. Shirokova, P. Benezeth, J. Schott, and S. V. Golubev
Reply to Comment by R. A. Berner on "Effect of organic ligands and heterotrophic bacteria on Wollastonite dissolution kinetics", American Journal of Science, v. 309, p. 731-772
Am J Sci, May 1, 2010; 310(5): 425 - 426.
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