22 citations as recorded by crossref.

1. Weichselian Upper Pleniglacial environmental variability in north-western Europe reconstructed from terrestrial mollusc faunas and its relationship with the presence/absence of human settlements O. Moine https://doi.org/10.1016/j.quaint.2014.02.030
2. La séquence lœssique de Morcourt (Somme, France) : un enregistrement remarquable du Pléniglacaire weichselien en contexte de versant E. Sambourg et al. https://doi.org/10.4000/14vgx
3. The turnover of dental microwear texture: Testing the” last supper” effect in small mammals in a controlled feeding experiment D. Winkler et al. https://doi.org/10.1016/j.palaeo.2020.109930
4. Austrian MIS 3/2 loess–palaeosol records—Key sites along a west–east transect B. Terhorst et al. https://doi.org/10.1016/j.palaeo.2014.10.020
5. What do dust sinks tell us about their sources and past environmental dynamics? A case study for oxygen isotope stages 3–2 in the Middle Rhine Valley, Germany M. Vinnepand et al. https://doi.org/10.5194/egqsj-72-163-2023
6. Accuracy of ESR dating of small gastropods from loess and fluvial deposits in the Bavarian Alpine Foreland G. Schellmann et al. https://doi.org/10.1016/j.quaint.2019.07.026
7. Reevaluation of Late Pleistocene loess profiles at Remizovka (Kazakhstan) indicates the significance of topography in evaluating terrestrial paleoclimate records T. Sprafke et al. https://doi.org/10.1017/qua.2017.103
8. Late Pleistocene loess of the Lower Rhine W. Schirmer https://doi.org/10.1016/j.quaint.2016.01.034
9. Millennial-scale terrestrial ecosystem responses to Upper Pleistocene climatic changes: 4D-reconstruction of the Schwalbenberg Loess-Palaeosol-Sequence (Middle Rhine Valley, Germany) P. Fischer et al. https://doi.org/10.1016/j.catena.2020.104913
10. Millennial-timescale quantitative estimates of climate dynamics in central Europe from earthworm calcite granules in loess deposits C. Prud’homme et al. https://doi.org/10.1038/s43247-022-00595-3
11. High‐resolution quantification of earthworm calcite granules from western European loess sequences reveals stadial–interstadial climatic variability during the Last Glacial C. Prud'homme et al. https://doi.org/10.1111/bor.12359
12. Geochemistry unravels MIS 3/2 paleoenvironmental dynamics at the loess–paleosol sequence Schwalbenberg II, Germany J. Profe et al. https://doi.org/10.1016/j.palaeo.2016.07.022
13. Late Pleistocene paleosols in the extra-glacial regions of Northwestern Eurasia: Pedogenesis, post-pedogenic transformation, paleoenvironmental inferences A. Rusakov et al. https://doi.org/10.1016/j.quaint.2018.03.020
14. Combining Inorganic and Organic Carbon Stable Isotope Signatures in the Schwalbenberg Loess-Palaeosol-Sequence Near Remagen (Middle Rhine Valley, Germany) M. Vinnepand et al. https://doi.org/10.3389/feart.2020.00276
15. Luminescence dating of loess deposits from the Remagen-Schwalbenberg site, Western Germany N. Klasen et al. https://doi.org/10.1515/geochr-2015-0008
16. The loess-palaeosol sequence of novyi tik: a new middle and upper pleistocene record for volyn’ upland (North-West Ukraine) O. Bonchkovskyi https://doi.org/10.4000/quaternaire.14308
17. Geochronological reconsideration of the eastern European key loess section at Stayky in Ukraine A. Kadereit & G. Wagner https://doi.org/10.5194/cp-10-783-2014
18. The MIS 3/2 transition in a new loess profile at Krems-Wachtberg East – A multi-methodological approach S. Meyer-Heintze et al. https://doi.org/10.1016/j.quaint.2017.11.048
19. The impact of Last Glacial climate variability in west-European loess revealed by radiocarbon dating of fossil earthworm granules O. Moine et al. https://doi.org/10.1073/pnas.1614751114
20. The Pleniglacial Weichselian loess sequence of Amiens-Renancourt 2 (France): stratigraphy, palaeoenvironment, geochronology and Gravettian occupation S. Coutard et al. https://doi.org/10.4000/16noo
21. The loess-palaeosol sequence of Datthausen, SW Germany: Characteristics, chronology, and implications for the use of the Lohne Soil as a marker soil D. Sauer et al. https://doi.org/10.1016/j.catena.2016.06.024
22. Enhanced weathering potentials—the role of in situ CO2 and grain size distribution T. Amann et al. https://doi.org/10.3389/fclim.2022.929268