Resumen: This work introduces for the first time the concept of using sinkholes in fluvial valleys as recorders of past floods. The notion is illustrated through the investigation of a complex sinkhole located in a broad floodplain underlain by salt-bearing Cenozoic evaporites. This active sinkhole comprises a large subsidence depression affecting the floodplain and the edge of a terrace, and a nested collapse sinkhole that used to host a sinkhole pond. A borehole drilled in the buried sinkhole pond revealed an ~7.8-m-thick fill that records around 2700 yr of clayey lacustrine deposition interrupted by three types of detrital facies. Two thick pebble gravel beds have been attributed to major high-competence floods: a paleoflood that occurred in Visigothic times (1537–1311 cal yr BP) and the 1961 Great Ebro River Flood, which is the largest event of the instrumental record. A trench dug in the portion of the terrace affected by subsidence exposed a mid-Holocene slack-water paleoflood deposit. The disadvantages and advantages of sinkholes as archives of past flood histories are discussed. Idioma: Inglés DOI: 10.1017/qua.2017.23 Año: 2017 Publicado en: Quaternary Research (United States) 88, 1 (2017), 71-88 ISSN: 0033-5894 Factor impacto JCR: 2.329 (2017) Categ. JCR: GEOSCIENCES, MULTIDISCIPLINARY rank: 76 / 189 = 0.402 (2017) - Q2 - T2 Categ. JCR: GEOGRAPHY, PHYSICAL rank: 26 / 49 = 0.531 (2017) - Q3 - T2 Factor impacto SCIMAGO: 1.216 - Arts and Humanities (miscellaneous) (Q1) - Earth-Surface Processes (Q1) - Earth and Planetary Sciences (miscellaneous) (Q1)