Palaeogeography, Palaeoclimatology, Palaeoecology

Faith et al. R Code 4FEB2019: R code used for analyses used to generate Figure 3 and Figure 7. Supplementary Table: modern African ungulate communities analyzed in Figure 5.

57Fe Mössbauer spectra of all samples from radiolarian-bearing siliceous limestones and carbonate-poor cherts from the Zliechov Basin, the Carpathian domain of the Alpine Tethys; percentage distribution (relative abundances) of iron corresponds to: ankerite-like Fe2+-(C) , aluminosilicate (chlorite-like) Fe2+-(Si) and Fe3+-(Si), hematite Fe2O3, and metallic iron α-Fe

Raw X and Y measurements of Astarte shells from the Pliocene of the Atlantic Coastal Plain of North America. The measurements were taken from digital photographs, and were used in a 2D morphometrics analysis.

List of specimens used from the National Museum of Wales to reconstruct bivalve diversity during the Early Jurassic.

Isotopes data include oxygen and carbon isotope. IRD include all types of minerogenic grains and data of detrital carbonate is given separately.

Bioerosion intensity, average bioerosion intensity and estimated bioerosion rates.

In this study, a regional storm reconstruction is performed based on a grain-size analysis (1450 samples) and stratigraphic modelling of the accelerator mass spectrometry radiocarbon dates of benthic foraminifera (19 samples) from two neighbouring lagoon cores from Lingyang Reef in the Xisha Islands located in the northern South China Sea of the western Pacific.

Netcdf files of coupled Antarctic ice sheet-sediment simulations over the last 40 Myr. A polar stereographic projection is used, centered on South Pole. Spatial fields of selected mode variables are saved every 100,000 years. fort.92_sedi23_seltime.nc is the main non-iterative simulation described in the paper (sections 3-5, horizontal resolution = 80 km). fort.92_sedi25_seltime.nc is the main iterative simulation in the paper (sections 6-7, last iteration, horizontal resolution = 160 km). The main 2-D model fields in the Netcdf files are: alatd (latitudes at grid centers) alond (longitudes at grid centers) h (ice thickness, m) hs (surface elevation above sea level, m) hb (bed elevation including sediment, m) hw (thickness of ocean water column) topbed (hard bedrock elevation below sediment, m) maskwater (0 is grounded ice or land, 1 if floating ice or open ocean) quarryacc (total bedrock eroded since start of simulation , m) sedim (sediment thickness, m)

Appendix A. CaCO3 content, δ13C and δ18O isotopes of bulk sediments, rock magnetic properties (IRM, ARM, HIRM300, and S-ratio300) and coarse fraction. Appendix B. Results of normalized magnetic susceptibility analysis. Appendix C. Assemblage count data for calcareous nannofossil taxa and groups expressed as percentages. Appendix D. Assemblage count data for Heliolithus genus expressed as N° of specimens/300 fields. Appendix E. Assemblage count data for selected planktonic foraminiferal taxa, P/(P+B) ratio, and fragmentation index. Appendix F. Assemblage count data for benthic foraminiferal assemblages: density, agglutinans vs. calcareous ratio, infauna vs. epifauna ratio, and the relative abundance of Spiroplectammina spp.

A compendium of bivalve body size data spanning the latest Triassic through the Early Jurassic.