Journal
PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
Volume 455, Issue -, Pages 53-64Publisher
ELSEVIER
DOI: 10.1016/j.palaeo.2016.02.002
Keywords
Clay minerals; Smectite; Paleoprecipitation; Paleoclimate; Stable isotopes
Funding
- EUROCORES scheme by the program TOPO-Alps/Topo-Europe (DFG) [Mu2845/2-1]
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The hydrogen and oxygen isotope compositions of bentonites and smectite-rich tuffs from the North Alpine Foreland Basin were measured for samples dated between 9 and 21 Ma. Assuming clay mineral formation shortly after the deposition of the volcanic ash layers and at surface temperatures estimated from paleoclimatic studies, the H and O isotope composition of water in equilibrium with the clay minerals can be calculated. A comparison with values derived from other proxies of paleoprecipitation in the Molasse Basin (such as pedogenic carbonates and mammal remains) and delta O-18 values of carbonate in the bentonite beds, suggests that the delta O-18 values of water estimated by this method are typical for foreland precipitation at this time and for this region. Therefore, the delta O-18 value of smectite in bentonites and altered tuff layers can be a useful tool for studies of paleoclimate and -topography. There are, however, indications that the clay minerals did not retain their initial hydrogen isotopic composition, but that a postformational exchange of H isotopes has occurred. (c) 2016 Elsevier B.V. All rights reserved.
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