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The δ13C, δ18O and Δ47records in biogenic, pedogenic and geogenic carbonate types from paleosol-loess sequence and their paleoenvironmental meaning
Zamanian K., Lechler A.R., Schauer A.J., Kuzyakov Y., Huntington K.W.
of carbonate types, including rhizoliths and land-snail shells, present in paleosol-loess sequences. However
The delta C-13, delta O-18 and Delta(47) records in biogenic, pedogenic and geogenic carbonate types from paleosol-loess sequence and their paleoenvironmental meaning
Zamanian K., Lechler A.R., Schauer A.J., Kuzyakov Y., Huntington K.W.
of carbonate types, including rhizoliths and land-snail shells, present in paleosol-loess sequences. However
The δ13C, δ18O and Δ 47 records in biogenic, pedogenic and geogenic carbonate types from paleosol-loess sequence and their paleoenvironmental meaning
Zamanian K., Lechler A.R., Schauer A.J., Kuzyakov Y., Huntington K.W.
of carbonate types, including rhizoliths and land-snail shells, present in paleosol-loess sequences. However
The δ13C, δ18O and Δ 47 records in biogenic, pedogenic and geogenic carbonate types from paleosol-loess sequence and their paleoenvironmental meaning
Zamanian K., Kuzyakov Y., Lechler A.R., Schauer A.J., Huntington K.W.
of carbonate types, including rhizoliths and land-snail shells, present in paleosol-loess sequences. However
Cryogenic-lateral hypothesis of the formation of the parent rock of soddy-podzolic soils using the example of the Ryshkovo paleosol (mis 5e) in the Taneyev quarry, Kursk Region
Sycheva, S. A., Khokhlova, O. S., Ershova, E. G., Myakshina, T. N., Ukrainskiy, P. A.
The Ryshkovo paleosol of the Mikulino Interglacial (MIS 5e), Late Moscow loess (MIS 6), and buried
Detrital and pedogenic magnetic mineral phases in the loess/palaesol sequence at Lingtai (Central Chinese Loess Plateau)
Spassov S., Heller F., Kretzschmar R., Evans M., Yue L., Nourgaliev D.
A detailed rock magnetic investigation of loess/palaeosol samples from the section at Lingtai
Transport of late pleistocene loess particles by katabatic winds during the lowstands of the english channel
Lefort J., Monnier J., Danukalova G.
the cementation of stony beaches under a loess blanket. Although the loess cover was later washed out by younger
Early Pleistocene climate in western arid central Asia inferred from loess-palaeosol sequences
Wang X., Wei H., Taheri M., Khormali F., Danukalova G., Chen F.
, chronological and climatic studies of early Pleistocene loess-palaeosol sequences (LPS) from the northeastern
Detrital and pedogenic magnetic mineral phases in the loess/palaesol sequence at Lingtai (Central Chinese Loess Plateau)
Spassov S., Heller F., Kretzschmar R., Evans M., Yue L., Nourgaliev D.
A detailed rock magnetic investigation of loess/palaeosol samples from the section at Lingtai
Early Pleistocene climate in western arid central Asia inferred from loess-palaeosol sequences
Wang X., Wei H., Taheri M., Khormali F., Danukalova G., Chen F.
, chronological and climatic studies of early Pleistocene loess-palaeosol sequences (LPS) from the northeastern

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