A fast «granularization» of lath-like bainite is observed in an Fe5Ni0.13C (wt pct) alloy during isothermal holding at Ms+ 20 K (+20°C). The microstructure evolution with holding time is characterized by Scanning Electron Microscopy and Electron BackScatter Diffraction. Granularization starts once the bainitic transformation is finished and degrades the mechanical properties. The granularization involves a rapid decrease in 60 deg h111i misoriented bainite laths to a dislocated granular bainite, followed by a slower dislocation rearrangement to sub-grain boundaries and more random boundaries. During the granularization, the carbides go through a ripening process.Bainitic steels have always provided a rich field of study, with many types of bainite already described in the literature. In many cases, these types of bainite have been discovered by virtue of industrial application progresses, resulting in several proposed classifications of bainite. Each classification approach has its own viewpoint and aims at clarifying the links between the observed bainitic microstructures (phases, textures, morphology, and topology) and either the processing conditions (transformation temperatures, cooling rates) or the associated steel properties (toughness, hardness…).Mehl's classification, [1] for instance, pays special attention to the nature of the constituent phases and their relative locations in bainite. The classification distinguishes upper bainite consisting of aggregates of ferrite plates separated by untransformed austenite, martensite, or cementite, [2] from lower bainite that contains additionally intra-lath cementite particles. The classifications of Aaronson et al., Ohmori et al., or Bramfitt et al. are based on similar concepts derived from thermo-kinetic analysis. [3][4][5] Recently, Zajac et al. [6] suggested a new definition or classification of bainites that is based on the misorientation angle distribution between bainitic sub-units. Neighboring grains or laths with different crystallographic variants inherited from the same austenite grain exhibits characteristic misorientations fully determined by the cfia orientation relationships (OR). [7] The relative frequency of these variants depends on the transformation conditions. Zajac and coworkers showed that this frequency differs significantly in upper and lower bainites. Upper bainite presents a high proportion of low-misorientation boundaries (with a high peak for misorientation angles in the range of 8 to 20 deg) and a small proportion of high-misorientation boundaries (small peak at misorientations >50 deg). The opposite distribution characterizes lower bainite. The angular domain between 20 and 50 deg contains no characteristic misorientations and instead reveals misorientation angles between sub-units inherited from differently oriented austenite grains. More recently, advanced crystallographic analysis confirmed differences in variant pairing of bainitic ferrite with transformation temperature. [8,9] Regardless of the classification approach, bainiti...