Secular oscillations in the carbonate mineralogy of reef-building and sediment-producing organisms driven by tectonically forced shifts in seawater chemistry

The primary mineralogy of oolites and early marine carbonate cements led Sandberg [Nature 305 (1983), 19–22] to divide the Phanerozoic Eon into three intervals of `aragonite seas' and two intervals of `calcite seas'. Hardie [Geology 24 (1996), 279–283] has shown that these oscillations, to...

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Veröffentlicht in:	Palaeogeography, palaeoclimatology, palaeoecology palaeoclimatology, palaeoecology, 1998-11, Vol.144 (1), p.3-19
Hauptverfasser:	Stanley, Steven M, Hardie, Lawrence A
Format:	Artikel
Sprache:	eng
Schlagworte:	biomineralization Bryozoa carbonates chalk Coccolithophoridae Corallinales Dasycladales Discoastera Halimeda limestone Marine reefs seawater chemistry
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