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      Financiación
      This study was funded by the Iniciativa Científica Milenio through Millennium Nucleus for Metal Tracing along Subduction Grant NC130065. Additional funding for analytical work was provided by the FONDAP project 15090013 “Centro de Excelencia en Geotermia de Los Andes, CEGA.” ST acknowledges CONICYT for support through a Ph.D. scholarship #21170857. Grants RTI2018-099157-A-100 and RYC-2015-1796 provided funding for sample preparation and EPMA analyses. This research used resources of the Advanced Photon Source, a U.S. Department of Energy (DOE) Office of Science User Facility operated for the DOE Office of Science by Argonne National Laboratory under Contract No. DE-AC02-06CH11357. The DID-UACh project #S-201505 financed the fieldwork. [1]
      This study was possible thanks to the financial support of Junta de Andalucía Research Group RNM179 and Research Project MAT2016-75889-R. [1]
      This work has been funded by an Initiative D’EXcellence (IDEX) grant 16C538 to S.A. The University of Granada is acknowledged for partial funding. Part of this work was also supported by the TelluS Program of CNRS/INSU. This is Institut de Physique du Globe de Paris contribution 4124. [1]
      This work has been supported by the Spanish CICYT project CGL2005-05863. [1]
      This work has been supported by the Spanish grants CGL2006-07938 and CLG2005-05863, and the Andalucian grant RNM1595. [1]
      This work is a contribution of the research group RNM-179 of the Junta de Andalucía, Spain. ASN and AC wish to express their gratitude for the financial support received from projects CGL2012-32169 and PID2021-126347NB-I00. Funding for open access charge: Universidad de Granada / CBUA. Antonio Sanchez-Navas reports was provided by University of Granada. [1]
      This work is included in the objectives and supported by the CGL2016–78796 project of the Spanish Ministerio de Ciencia, Innovación y Universidades (MICINN) and the UCM 910492 group. González-Jiménez acknowledges financial support of the Ramón y Cajal Fellowship RYC-2015–17596, granted by the Spanish Ministerio de Economía y Empresa (MINECO). [1]
      This work was financed by Projects MARM 200800050084447, MICINN CGL2009-07603, Junta de Andalucía RNM-5212 and Research Group RNM 179 (Junta de Andalucía), We also thank Project CSD2006-00041 Topoberia. We would also like to thank the “Plan Propio de Investigación (UGR)” for financial support (postdoctoral fellowship D. Gallego-Torres). [1]
      This work was financially supported by the Spanish grant CLG2005-05863/BTE and the Andalucian grant RNM1595. This is the Nordsim publication nº 209. The Nordsim facility is operated and financed under a contract between the research funding agencies of Denmark, Norway and Sweden, the Swedish Museum of Natural History and the Geological Survey of Finland. [1]
      This work was financially supported supported by the Spanish DGCYT grant BTE2002-04618-C02-01, the SYNTHESIS grant SE-TAF 528 and the NATO Collaborative Project EST-CLG-978997. [1]
      This work was supported by a grant from the Canadian Institutes of Health Research (no. MOP-142330) and the Natural Sciences and Engineering Research Council of Canada (NSERC; no. RGPIN-2016-05031) to M.D.M., an NSERC (no. RGPIN-2016-04410) Discovery grant to M.T.H., a Spanish Government grant (CGL2015-64683-P) to A.B.R.-N., an Emmy Noether research grant from the German Research Foundation (no. WO1712/3-1) to S.E.W., and an NSF grant (NSF BMAT; no. 1507736) to J.J.G. M.D.M. is a member of the Fonds de Recherche Quebec–Sante Network for Oral and Bone Health Research and the McGill Centre for Bone and Periodontal Research [1]
      This work was supported by the Earth and Life Sciences Division of the Netherlands Organization for Scientific Research (NWO-ALW) by a grant (ALW 820.01.013) to J. S. Sinninghe Damsté. The research leading to these results has received funding from the European Research Council (ERC) under the European Union’s Seventh Framework Program (FP7/2007-2013) ERC grant agreement 226600. [1]