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- W2040726454 abstract "The ca. 2000 Ma Tulomozerskaya Formation, Russian Karelia, is composed of an 800 m-thick magnesite-stromatolite-dolostone-'red bed' succession with the most 13 C-rich dolostones (up to +18 V-PDB) that have ever been reported. Terrigenous 'red beds' are developed throughout the sequence and represent three main depositional settings: (1) a braided fluvial system over a lower energy, river-dominated coastal plain, (2) a low-energy, barred lagoon or bight, and (3) a non-marine, playa lake. A significant component of the sequence consists of biostromal and biohermal columnar stromatolites accreted in shallow-water, low-energy, intertidal zones, barred evaporitic lagoons and peritidal evaporitic environments. Only a small portion of stromatolites might have been accreted in relatively 'open' marine environments. The red, flat-laminated, dolomitic and magnesite stromatolites formed in evaporative ephemeral ponds, coastal sabkhas and playa lakes. Tepees, mudcracks, pseudomorphs after calcium sulphate, halite ca..." @default.
- W2040726454 created "2016-06-24" @default.
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- W2040726454 date "2000-01-01" @default.
- W2040726454 modified "2023-10-10" @default.
- W2040726454 title "Palaeoproterozoic magnesite-stromatolite-dolostone-'red bed' association, Russian Karelia: Palaeoenvironmental constraints on the 2.0 Ga-positive carbon isotope shift" @default.
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