Methane-rich water springs and seeps discovered in the Ronda peridotite massif.
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Stable C and H isotope ratios indicate a predominant abiotic origin of methane.
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Methane is not generated from the C in the hyperalkaline water.
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Methane is released as bubbles and diffuse seepages.
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Gas follows migration pathways independent from the hyperalkaline springs.
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