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carbon isotopes from paleosols of the Southern Chinese loess
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Variations in Chinese Loess. Nature, 346, 737–739.
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174.
Rousseau, D.-D. et al. (2007b). Link Between European and North
Atlantic Abrupt Climate Changes over the Last Glaciation.
Geophysical Research Letters, 34, https://doi.org/10.1029/
2007gl031716.
Rousseau, D. D., et al. (2013). Major dust events in Europe during
marine isotope stage 5 (130–74 ka): A climatic interpretation of the
‘markers. Climate of the Past, 9, 2213–2230.
Rousseau, D.-D., et al. (2014). European Glacial Dust Deposits:
Geochemical Constraints on Atmospheric Dust Cycle Modeling.
Geophysical Research Lettters, 41, 7666–7674. https://doi.org/10.
1002/2014GL061382.
Sima, A., et al. (2009). Imprint of North-Atlantic millennial-timescale
variability on Western European loess deposits as viewed in a dust
emission model. Quaternary Science Reviews, 28, 2851–2866.
Sun, Y. et al. (2008). Tracing the provenance of fine-grained dust
deposited on the central Chinese loess plateau. Geophysical
Research Letters, 35. https://doi.org/10.1029/2007GL031672.
Taylor, S. N., et al. (2014). Mineral magnetic characterization of the
Upper Pleniglacial Nussloch loess sequence (Germany): an insight
into local environmental processes. Geophysical Journal International, 199, 1463–1480.
Wang, H., & Follmer, L. R. (1998). Proxy of monsoon seasonality in
carbon isotopes from paleosols of the Southern Chinese loess
plateau. Geology, 26, 987–990.
Wu, N. Q. et al., (2001). Orbital forcing of terrestrial mollusks and
climatic changes from the loess plateau of China during the past
350 ka. Journal of Geophysical Research—Atmospheres, 106, 20
045–20 054.
Zhou, L. P., et al. (1990). Partly Pedogenic Origin of Magnetic
Variations in Chinese Loess. Nature, 346, 737–739.
13 Ground-Air Interface: The Loess Sequences, Markers …
167