Cave ferromanganese stromatolites and associated wall notches mark paleo-watertables.
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Paleomagnetism of cave Fe–Mn deposits: a new approach to date paleo-watertables
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Acidity produced by watertable Mn–Fe oxidation contributes to speleogenesis.
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Allogenic-sediment input controls watertable versus phreatic passage development.
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Matrix porosity in host dolostone induces spongework cave-wall mesomorphologies.
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