Abstract
[Perry et al. (2006)][1] contribute a fourth alternative, of silica binding, to three prior hypotheses of varnish formation: 1) abiotic Mn-Fe enhancement (e.g., [Engel and Sharp, 1958][2]); 2) biotic Mn-Fe enhancement (e.g., [Dorn and Oberlander, 1982][3]; [Allen et al., 2004][4]); and 3) a
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