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Effects of peat decomposition on δ 13 C and δ 15 N depth profiles of Alpine bogs of stable carbon and nitrogen isotopes (δ 13 C and δ 15 N) in soils and peats. However, the applicability

Effects of peat decomposition on δ 13 C and δ 15 N depth profiles of Alpine bogs for the signatures of stable carbon and nitrogen isotopes (δ 13 C and δ 15 N) in soils and peats. However

Effects of peat decomposition on δ 13 C and δ 15 N depth profiles of Alpine bogsEffects of peat decomposition on δ 13 C and δ 15 N depth profiles of Alpine

Land use change decreases soil carbon stocks in Tibetan grasslands to cropland. Detailed SOC measurements up to 30-cm depth were combined with analysis of δ13C, δ15N, bulk

Land use change decreases soil carbon stocks in Tibetan grasslands to cropland. Detailed SOC measurements up to 30-cm depth were combined with analysis of δ13C, δ15N, bulk

The δ13C, δ18O and Δ47records in biogenic, pedogenic and geogenic carbonate types from paleosol-loess sequence and their paleoenvironmental meaning investigate the effects of carbonate type on δ13C, δ18O, and clumped isotope-derived paleotemperature [T(Δ47

The δ13C, δ18O and Δ 47 records in biogenic, pedogenic and geogenic carbonate types from paleosol-loess sequence and their paleoenvironmental meaning investigate the effects of carbonate type on δ13C, δ18O, and clumped isotope-derived paleotemperature [T(Δ47

The δ13C, δ18O and Δ 47 records in biogenic, pedogenic and geogenic carbonate types from paleosol-loess sequence and their paleoenvironmental meaning investigate the effects of carbonate type on δ13C, δ18O, and clumped isotope-derived paleotemperature [T(Δ47

Some new data on isotope stratigraphy of the permian rocks at the east of the Russian platform© 2006-2015 Asian Research Publishing Network (ARPN). Variations of δ13C, δ18
Isotope (δ13C and δ18O) compositions of dolomites from the Permian evaporitic sequences of the Eastern Russian Plate: Evidence from the Syukeevo gypsum deposit located in the Eastern Russian Plate. Values of δ13C in the dolomites vary from 0.3 to 6.6 ‰; δ18O, from

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