RT info:eu-repo/semantics/article T1 Magnetic susceptibility in the European Loess Belt: New and existing models of magnetic enhancement in loess A1 Bradák, Balázs A1 Seto, Yusuke A1 Stevens, Thomas A1 Újvári, Gábor A1 Fehér, K. A1 Költringer, Chiara K1 Magnetic susceptibility K1 Loess K1 Magnetic enhancement K1 Nano-scale fragmentation K1 Magnetic inclusion K1 Magnetismo K1 Magnetism K1 Geología K1 Geology AB Magnetic susceptibility measurements play a key role in Quaternary studies. Magnetic proxies, such as low field and frequency-dependent magnetic susceptibility, are widely applied in the reconstruction of terrestrial paleoclimate, e.g., in the study of loess-paleosol successions. In general, the interpretation of loess magnetic susceptibility signals is based on two commonly accepted models: the pedogenic magnetic enhancement and wind-vigour models. However, there are an increasing number of cases where such models cannot be used. These cases show unusual relationships between the two common loess magnetic susceptibility proxies: low field and frequency-dependent magnetic susceptibility. Such relationships have been attributed to various phenomena including the dissolution of fine-grain minerals and the formation of ultrafine magnetic rims on the surface of coarser grains by weathering. Despite the growing number of these exceptional cases of magnetic enhancement, our knowledge about the occurrence and potential causes of the unusual behaviour of magnetic susceptibility parameters is still limited. This, in turn, hinders the wider application of magnetic susceptibility parameters in loess. To fill this knowledge gap, magnetic susceptibility data of various profiles from the European Loess Belt were collected and compared to reveal various enhancement trends in loess. Along with the analysis of magnetic susceptibility parameters, combined scanning electron microscopy (SEM) and rock magnetic analyses were applied to samples from the Paks loess sequence in Hungary to describe some of the irregular cases, notably the cause of increasing frequency-dependent susceptibility in non-altered sediments. Analysis of loess, paleosol and common mineral samples separated from loess (e.g., muscovite) revealed that various features may be responsible for these increasing frequency-dependent susceptibility values: i) surface weathering (maghemitization) of coarser detrital grains, ii) nanofragmentation by physical weathering and iii) the appearance of significant amounts of ultrafine magnetic inclusions in micas. These special modes of magnetic enhancement of loess do not undermine the importance of the basic theories suggested above, but rather provide three mechanisms that account for some of the increasing number of unusual cases. To aid in the wider and more accurate use of magnetic susceptibility parameters in loess, we review the current magnetic enhancement models with special emphasis on the identification of unusual trends in magnetic enhancement and understanding their drivers. PB Elsevier SN 0031-0182 YR 2021 FD 2021-05 LK http://hdl.handle.net/10259/6100 UL http://hdl.handle.net/10259/6100 LA eng NO Project BU235P18 (Junta de Castilla y Leon, Spain) and the European Regional Development Fund (ERD), project PID2019-108753GB-C21/AECI/ 10.13039/501100011033 of the Agencia Estatal de Investigación and project PID2019-105796GB-100/AECI/ 10.13039/501100011033 of the Agencia Estatal de Investigación. Part of the measurements were conducted during a fellowship awarded to B. Bradák at Kobe University, Japan, by the Japan Society for the Promotion of Science (JSPS; P15328). Part of this study was conducted within the cooperative research programme of the Center for Advanced Marine Core Research, Kochi University (15A001, 16A002, 17A016), with the support of the Japan Agency for Marine-Earth Science and Technology (JAMSTEC). The Swedish Research Council is gratefully acknowledged for funding to TS for part of this project (2017-03888). DS Repositorio Institucional de la Universidad de Burgos RD 29-mar-2024