The influence of alkalilnity and pco2 on caco3 nucleation from variable composition phanerozoic seawater
There is strong evidence that variations in seawater chemistry occurred during the Phanerozoic Eon. Of particular importance are the changes in the Mg2+/Ca2+ ratio because they have been attributed to the oscillations between “calcite” and “aragonite seas” over time. In addition to the Mg2+/Ca2+ rat...
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| Format: | Others |
| Language: | en_US |
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2010
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| Online Access: | http://hdl.handle.net/1969.1/ETD-TAMU-3216 http://hdl.handle.net/1969.1/ETD-TAMU-3216 |