geo 16 - Oxygen and Carbonate Precipitation , Herringbone...

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Carbonate Precipitation Experiments Previous experimental work (Dromgoole and Walter, 1990a, b; refs ) has shown that Fe 2+ dramatically slows calcite precipitation rates. The abundance of banded iron-formations * suggests that deep Archean seawater contained abundant Fe 2+ . If surface water was also anoxic, Fe 2+ may have been present in calcite- precipitating environments. Based on textures in Archean carbonates * , John Grotzinger and I proposed that Fe 2+ affected both the dynamics carbonate precipitation and the morphology of resulting crystals (see
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Unformatted text preview: Oxygen and Carbonate Precipitation , Herringbone Calcite , and Archean Carbonate Precipitation and Oxygen ). To test this hypothesis, Ryoji is running calcite precipitation experiments under various conditions that may replicate Archean ocean conditions. Preliminary results show that Fe 2+ significantly reduces crystal nucleation rates, slows calcite precipitation, and strongly affects crystal morphology (see photo at right, AGU 1999 abstract and photos , and IGC 2000 abstract )....
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This note was uploaded on 01/31/2011 for the course GEL 1 taught by Professor Barfod during the Spring '08 term at UC Davis.

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