Rapid Australian Plate Motion across Dynamic Topography Promotes Last Interglacial Reef Subsidence and the Long-Term Development of the Great Barrier Reef

Data shown in the tables and figures of the manuscript: Rapid Australian Plate Motion across Dynamic Topography Promotes Last Interglacial Reef Subsidence and the Long-Term Development of the Great Barrier Reef, submitted to AGU Advances. Data include: (1) Previously published data on the depth of the Pleistocene/Holocene boundary in the Great Barrier Reef (from Table S1 and shown in Fig. 1 of the manuscript); (2) Fits to geodynamic observables provided by tomography-based flow models (from Table S2); (3) Elastic flexural modification of ECM1 advected residual/non-isostatic topography (from Table S3) (4) Decomposition of dynamic topography predictions at Stanley Reef over the same LIG interval (from Table S4); (5) Previously published coral U-Th ages and elevations shown in Figure 2 of the manuscript from the Great Barrier Reef and from (6) Western Australia; (7) Subsidence calculations plotted in Figure 3 of the manuscript.