Compilation of total burial subsidence of intracratonic basins modified from literature showing periods of acceleration (ALRS: Acceleration of the Low Rate subsidence), deceleration (DLRS: Deceleration of the Low Rate Subsidence) and inversion (ILRS: Inversion of the Low Rate Subsidence) of the low rate subsidence. 1: New York, USA, well 7-6 (Adkinson, 1966 from Sleep et al., 1980); 2: Ohio, USA, well 6-6 (Adkinson, 1966 from Sleep et al., 1980); 3: Johnson County, USA, Illinois well (Sleep et al., 1980); 4: Michigan Basin well, USA (Sleep and Sloss, 1978); 5: Ahnet Basin, Algeria, well W1 (Kracha, 2011); 6: Ghadames/Berkine Basin, Algeria (Yahi, 1999); 7: Illizi Basin well, Algeria (Wells et al., 2018); 8: Mouydir Basin, Algeria Well W21 (Perron et al., 2018); 9: Tyumen SG-6 section, Urengoy region, Russia (Nikishin et al., 2002); 10: North Dakota, Williston Basin, USA, well 11 (Smith, 1967 from Fowler and Nisbet, 1985); 11: Williston Basin, Saskatchewan, USA, well 1 (Fowler and Nisbet, 1985); 12: Paris Basin, France, well CFX-1 (Brunet and Pichon, 1982); 13: Parnaíba Basin, Brazil, well 2-BAC (Tozer et al., 2017); 14: Northeast German Basin, Germany (Scheck and Bayer, 1999). The dashed line represents thermal seafloor subsidence from Xie and Heller (2009). For 7 (well W1, Ahnet Basin) and 19 (well W21, Mouydir Basin) see Figure 2 for localisation. Notice that this is a compilation of worldwide intracratonic basins, where different explanations from the literature (e.g. Xie and Heller, 2009; Allen and Armitage, 2011) can be invoked to capture the origin of their subsidence.