The stable isotopic composition of pedogenic carbonate forms in equilibrium with environmental parameters and, thus, records palaeoenvironmental signals. The aims of this study are to synthesize available data on the stable isotopic composition of Quaternary pedogenic carbonates in calcareous parent materials of Iran and to decipher paleoenvironmental implications of the isotopic data for the country. Isotopic composition and microfabric of pedogenic carbonates in 18 pedons in both gravelly (calcareous alluvium in central Iran) and non-gravelly deposits (calcareous loess in northeastern Iran) have been investigated. The results indicate that in limestone-derived soils of central Iran in situ weathering of calcareous pebbles is a major sourc...
Pedogenic calcretes are abundant in arid and semi-arid regions, and they are widely used as proxy re...
EASPEBIOmEAGROSUPPedogenic carbonates (calcretes) have often been proposed as possible markers of th...
Stable isotope compositions of pedogenic carbonates (δ13Ccarb, δ18Ocarb) are widely used in paleoenv...
The stable isotopic composition of pedogenic carbonate forms in equilibrium with environmental param...
Despite the occurrence of pedogenic carbonates in loess/paleosol sequences of northern and northeast...
Stable isotopes in pedogenic carbonates can provide information for geomorphic evolution of landscap...
Although central Iran is pivotal for palaeoclimatic correlations, palaeoenvironmental data for this ...
In the high plateau region of central Iran, there is both a lack of information on calcic soil proce...
Gypsum accumulation is one of the prominent pedogenic processes occurring in many arid regions of t...
The influence of the pedogenic and climatic contexts on the formation and preservation of pedogenic ...
Non-pedogenic carbonates, such as carbonate cement and nodules in the sandstones, are quite common i...
Paleoclimatic investigation of loess-paleosol sequences from northern Iran is important for understa...
The influence of the pedogenic and climatic contexts on the formation and preservation of pedogenic ...
Soil carbonates are key features in soils of arid and semiarid environment, playing an important rol...
Stable isotope C analysis is the most reliable method used for the distinction and understanding of ...
Pedogenic calcretes are abundant in arid and semi-arid regions, and they are widely used as proxy re...
EASPEBIOmEAGROSUPPedogenic carbonates (calcretes) have often been proposed as possible markers of th...
Stable isotope compositions of pedogenic carbonates (δ13Ccarb, δ18Ocarb) are widely used in paleoenv...
The stable isotopic composition of pedogenic carbonate forms in equilibrium with environmental param...
Despite the occurrence of pedogenic carbonates in loess/paleosol sequences of northern and northeast...
Stable isotopes in pedogenic carbonates can provide information for geomorphic evolution of landscap...
Although central Iran is pivotal for palaeoclimatic correlations, palaeoenvironmental data for this ...
In the high plateau region of central Iran, there is both a lack of information on calcic soil proce...
Gypsum accumulation is one of the prominent pedogenic processes occurring in many arid regions of t...
The influence of the pedogenic and climatic contexts on the formation and preservation of pedogenic ...
Non-pedogenic carbonates, such as carbonate cement and nodules in the sandstones, are quite common i...
Paleoclimatic investigation of loess-paleosol sequences from northern Iran is important for understa...
The influence of the pedogenic and climatic contexts on the formation and preservation of pedogenic ...
Soil carbonates are key features in soils of arid and semiarid environment, playing an important rol...
Stable isotope C analysis is the most reliable method used for the distinction and understanding of ...
Pedogenic calcretes are abundant in arid and semi-arid regions, and they are widely used as proxy re...
EASPEBIOmEAGROSUPPedogenic carbonates (calcretes) have often been proposed as possible markers of th...
Stable isotope compositions of pedogenic carbonates (δ13Ccarb, δ18Ocarb) are widely used in paleoenv...