36 citations as recorded by crossref.

1. Early to mid-Holocene hydroclimate trends in the western Carpathians of Romania A. Ruskál et al. 10.1016/j.palaeo.2020.109608
2. The provenance of Danubian loess K. Fenn et al. 10.1016/j.earscirev.2022.103920
3. Millennial-scale fluctuations in Saharan dust supply across the decline of the African Humid Period C. Zielhofer et al. 10.1016/j.quascirev.2017.07.010
4. Past anthropogenic impacts revealed by trace elements in cave guano F. Forray et al. 10.1016/j.chemosphere.2024.142447
5. Disentangling Sedimentary Pathways for the Pleniglacial Lower Danube Loess Based on Geochemical Signatures S. Pötter et al. 10.3389/feart.2021.600010
6. Mid-Holocene intensification of Southern Hemisphere westerly winds and implications for regional climate dynamics J. Tamhane et al. 10.1016/j.quascirev.2023.108007
7. Holocene environmental changes as recorded in the geochemistry of glacial lake sediments from Retezat Mountains, South Carpathians K. Hubay et al. 10.1016/j.quaint.2018.02.024
8. Relations of fire, palaeohydrology, vegetation succession, and carbon accumulation, as reconstructed from a mountain bog in the Harz Mountains (Germany) during the last 6200 years M. Gałka et al. 10.1016/j.geoderma.2022.115991
9. Loess landscapes of Europe – Mapping, geomorphology, and zonal differentiation F. Lehmkuhl et al. 10.1016/j.earscirev.2020.103496
10. A critical reevaluation of palaeoclimate proxy records from loess in the Carpathian Basin I. Obreht et al. 10.1016/j.earscirev.2019.01.020
11. Holocene vegetation history and environmental change in the Lăpuş Mountains, north-west Romania M. Peters et al. 10.1080/01916122.2019.1615567
12. Nd isotopes as a tracer of dust trapped by peat bogs: A reminder of basics. Comment on: « Neodymium isotopes in peat reveal past local environmental disturbances » by G. Le Roux et al. 10.1016/j.scitotenv.2023.163379
13. Imprints of Holocene aridity variability in the Aegean Sea and interconnections with north-latitude areas A. Noti et al. 10.1177/09596836241247300
14. Origin and Holocene geomorphological evolution of the landslide-dammed basin of la Narse de la Sauvetat (Massif Central, France) A. Mayoral et al. 10.1016/j.geomorph.2018.08.015
15. Disentangling dust and sand deposition using a peat record in CE Europe (northern Romania): A multiproxy approach A. Panait et al. 10.1016/j.palaeo.2019.109257
16. XRF core scanning yields reliable semiquantitative data on the elemental composition of highly organic-rich sediments: Evidence from the Füramoos peat bog (Southern Germany) O. Kern et al. 10.1016/j.scitotenv.2019.134110
17. Carbon accumulation rates of Holocene peatlands in central–eastern Europe document the driving role of human impact over the past 4000 years J. Longman et al. 10.5194/cp-17-2633-2021
18. Ultra-distal fine ash occurrences of the Icelandic Askja-S Plinian eruption deposits in Southern Carpathian lakes: New age constraints on a continental scale tephrostratigraphic marker R. Kearney et al. 10.1016/j.quascirev.2018.03.035
19. OSL-dating of the Pleistocene-Holocene climatic transition in loess from China, Europe and North America, and evidence for accretionary pedogenesis D. Constantin et al. 10.1016/j.earscirev.2021.103769
20. Diversity and peculiarities of soil formation in eolian landscapes – Insights from the mineral magnetic records D. Jordanova & N. Jordanova 10.1016/j.epsl.2019.115956
21. Holocene paleoclimate inferred from stable isotope (δ18O and δ13C) values in Sphagnum cellulose, Mohos peat bog, Romania M. Túri et al. 10.1007/s10933-021-00202-z
22. Utilisation of XRF core scanning on peat and other highly organic sediments J. Longman et al. 10.1016/j.quaint.2018.10.015
23. A multi-proxy analysis of hydroclimate trends in an ombrotrophic bog over the last millennium in the Eastern Carpathians of Romania A. Diaconu et al. 10.1016/j.palaeo.2019.109390
24. Challenges in Interpreting Geochemical Data: An Appraisal of Analytical Techniques Applied to a Karstic Lake Sediment Record A. Haliuc et al. 10.3390/w14050806
25. Holocene aeolian dust accumulation rates across the Chinese Loess Plateau S. Zhao et al. 10.1016/j.gloplacha.2021.103720
26. Peatbog resilience to pollution and climate change over the past 2700 years in the Harz Mountains, Germany M. Gałka et al. 10.1016/j.ecolind.2018.10.015
27. Past African dust inputs in the western Mediterranean area controlled by the complex interaction between the Intertropical Convergence Zone, the North Atlantic Oscillation, and total solar irradiance P. Sabatier et al. 10.5194/cp-16-283-2020
28. Storm chasing: Tracking Holocene storminess in southern Sweden using mineral proxies from inland and coastal peat bogs M. Kylander et al. 10.1016/j.quascirev.2022.107854
29. At an important tephrostratigraphic crossroads: cryptotephra in Late Glacial to Early Holocene lake sediments from the Carpathian Mountains, Romania R. Kearney et al. 10.1016/j.quascirev.2024.108558
30. Plant succession in a peatland in the Eastern Carpathian Mts. (CE Europe) during the last 10,200 years: Implications for peatland development and palaeoclimatic research M. Gałka et al. 10.1016/j.revpalbo.2017.05.014
31. Lipid biomarker (brGDGT)- and pollen-based reconstruction of temperature change during the Middle to Late Holocene transition in the Carpathians M. Ramos-Román et al. 10.1016/j.gloplacha.2022.103859
32. Runoff events and related rainfall variability in the Southern Carpathians during the last 2000 years J. Longman et al. 10.1038/s41598-019-41855-1
33. Holocene climate dynamics on the European scale: Insights from a coastal archaeological record from the temperate Bay of Biscay (SW France) F. Eynaud et al. 10.1016/j.quaint.2021.09.018
34. Short-term soil formation events in last glacial east European loess, evidence from multi-method luminescence dating D. Veres et al. 10.1016/j.quascirev.2018.09.037
35. The 4.2 ka BP Event in the Mediterranean region: an overview M. Bini et al. 10.5194/cp-15-555-2019
36. Post-eruptive sedimentary processes in volcanic crater lakes: implications for deciphering the Samoan sedimentary record A. Fepuleai et al. 10.1007/s10933-018-0035-y