RT info:eu-repo/semantics/article T1 Three archaeomagnetic applications of archaeological interest to the study of burnt anthropogenic cave sediments A1 Carrancho Alonso, Ángel A1 Herrejón Lagunilla, Ángela A1 Vergés, Josep Maria . K1 Fumiers K1 Holocene K1 Thermoremanent magnetization K1 Secular variation K1 Ashes K1 Bronze Age K1 Physics K1 Paleontology K1 Física K1 Paleontología AB Recent archaeomagnetic studies carried out on Mid-to Late Holocene burnt anthropogenic cave sedimentshave shown that under certain conditions, these materials are suitable geomagnetic field recorders.Archaeomagnetic analyses carried out on these contexts constitute a rich source of informationnot only for geophysical purposes -in terms of reconstructing the variation of Earth's magnetic field inthe past- but also from the archaeological point of view, for example by archaeomagnetic dating. Here,we report three different archaeomagnetic applications to the study of burnt cave sediments: (i)archaeomagnetic dating; (ii) determining palaeotemperatures and (iii) assessing post-depositionalprocesses. The first case study is a dating attempt carried out on a Late Holocene (Bronze Age) burntlevel from El Mirador Cave (Burgos, Spain). Using the directional European secular variation curve,several dating intervals were obtained for the last burning of this combustion feature. Considering thearchaeological evidence and the independent radiometric (14C) dating available the possible ages obtainedare discussed. This is the first archaeomagnetic dating obtained in these contexts so far. Thesecond case study is an application of the method to determine the last heating temperatures reached bythe carbonaceous facies of these fires. Stepwise thermal demagnetization of oriented samples can beused to quantitatively estimate heating temperatures. An intermediate normal polarity componentinterpreted as a partial thermo-remanence (pTRM) with maximum unblocking temperatures of 400e450 C was systematically identified, revealing the last heating temperatures experienced by this facies.These temperatures were confirmed with partial thermomagnetic curve experiments. Finally, archaeomagneticanalyses on a partially bioturbated burning event were performed in order to evaluate untilwhat spatial extent the burnt sediments were affected by post-depositional mechanical alteration processes.For each case study, the archaeological implications are discussed highlighting the potential ofarchaeomagnetic methods to retrieve archaeological information. PB Elsevier SN 1040-6182 YR 2016 FD 2016-09 LK http://hdl.handle.net/10259/4594 UL http://hdl.handle.net/10259/4594 LA eng NO MINECO projects CGL2012-32149 and CGL2012-38481 DS Repositorio Institucional de la Universidad de Burgos RD 27-abr-2024