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- W1964373009 abstract "Dissolved carbonates in interstitial waters of Lake Kinneret sediments (Galilee, Israel) are enriched in 13C by 10– 20‰ over the dissolved carbonate in the lake water. The increase of alkalinity which accompanies this enrichment indicates in situ formation of dissolved carbonate. The interstitial waters are slightly undersaturated in respect to calcite, but dissolution of CaCO3 cannot explain the enriched 13C values. The enrichment of 13C in the pore water carbonate is probably related to the anaerobic decomposition of organic matter in the sediments." @default.
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- W1964373009 date "1974-09-01" @default.
- W1964373009 modified "2023-09-27" @default.
- W1964373009 title "Carbon-13 enriched carbonate in interstitial waters of Lake Kinneret sediments" @default.
- W1964373009 doi "https://doi.org/10.4319/lo.1974.19.5.0849" @default.
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