摘要 : Major ion compositions of primary fluid inclusions from terminal Proterozoic (ca. 544 Ma) and Early Cambrian (ca. 515 Ma) marine halites indicate that seawater Ca2+ concentrations increased approximately threefold during the Early... 展开
作者 | Brennan ST Lowenstein TK Horita J |
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作者单位 | |
期刊名称 | 《Geology》 |
总页数 | 4 |
语种/中图分类号 | 英语 / P5 |
关键词 | seawater evaporites fluid inclusions biomineralization Cambrian explosion SECULAR VARIATION FLUID INCLUSIONS MARINE CALCIFICATION OSCILLATIONS EVAPORITES MAGNESIUM STRONTIUM EVOLUTION CALCIUM |
馆藏号 | N2008EPST0000793 |