Pore water evolution during sediment burial from isotopic and mineral chemistry of calcite, dolomite and siderite concretions
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Cited by (206)
Environmental shifts in and around Lake Pannon during the Tortonian Thermal Maximum based on a multi-proxy record from the Vienna Basin (Austria, Late Miocene, Tortonian)
2023, Palaeogeography, Palaeoclimatology, PalaeoecologyModern analogs reveal the origin of Carboniferous coal balls
2021, Palaeogeography, Palaeoclimatology, PalaeoecologyCitation Excerpt :There is clayey material below the ganister, but it is separated by a disconformity, so not part of an Ultisol paleosol. The δ18O and δ13C isotopic composition of the calcite and dolomite coal balls, as well as siderite nodules in overlying shales, were provided by Curtis et al. (1986), and show two distinct patterns (Fig. 6A–B). The calcite-dolomite shows a δ18O and δ13C correlation, with two distinct populations, like the Hitchcox limey peat (Fig. 6A), but the siderite shows δ18O-invariance, like modern siderite nodules (Moore et al., 1992).
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