Play Deep Time Earth is built on the following open datasets and tools.
Continental crust fragments and plate boundaries at 540–1800 Ma. Not elevations, climate or actual palaeocoastlines.
Cao et al. (2024), Earth's tectonic and plate boundary evolution over 1.8 billion years, model version 2.4
Source ↗Related study ↗Modifications: Reconstructed using the model's palaeomagnetic frame and valid source ages. A fixed +60° eastward display rotation aids continuity without changing source data. Latitudes and poles are preserved; display longitudes differ from the model's. Plate boundaries use 5 Ma intervals; interpolation does not improve scientific accuracy. Continental configuration and shape differences remain at 540 Ma.
⚠ The dataset is CC BY 4.0, distinct from the paper's CC BY-NC-ND license. Paper figures and supplemental videos are not redistributed.
A global ice-sheet and paleotopography model for the past 80,000 years. Source steps are 2,500 years apart and include Earth deformation and spatially varying sea-level change.
Gowan, E.J. (2019). Global ice sheet reconstruction for the past 80000 years. PANGAEA, DOI 10.1594/PANGAEA.905800. Study: Gowan et al. (2021), A new global ice sheet reconstruction for the past 80,000 years, Nature Communications 12, 1199, DOI 10.1038/s41467-021-21469-w.
Source ↗Related study ↗Modifications: Terrain and reconstructed ice-sheet margins from scenario a1 (Hudson Bay remains ice-covered through MIS 3) adapted for display. The nearest source step, spaced 2,500 years apart, is shown; the modern comparison uses the same model baseline. Derived data: CC BY 4.0. Smoother edges do not improve observational accuracy. The display can omit small islands and narrow straits and does not establish human movement or passability. Ice shows reconstructed extent, not sea ice or a definitive grounding map. 0 ka refers to 1950 CE. Not applied before 80,000 years ago; no warranty or author endorsement is implied.
Underlying sources credited by the model. The service uses PaleoMIST; the originals, papers and figures below are not separately redistributed.
Paleodigital Elevation Models (0–540 Ma heightmaps)
Scotese, C.R. and Wright, N.M. (2018). PALEOMAP Paleodigital Elevation Models (PaleoDEMS) for the Phanerozoic.
Modifications: Terrain adapted for visualization with narrow-strait corrections. Modern coastline data is applied only at 0 Ma.
81 global coastline reconstructions (0–535 Ma). PaleoDEM coastlines adjusted using fossil records to represent maximum marine flooding.
Kocsis, A.T. and Scotese, C.R. (2023). PaleoMAP PaleoCoastlines data, v7.3. Zenodo. Study: Mapping paleocoastlines and continental flooding during the Phanerozoic, Earth-Science Reviews, DOI 10.1016/j.earscirev.2020.103463.
Source ↗Related study ↗Modifications: Coastlines and inland waters at 5–535 Ma adapted for display, with interpolation between source ages. 0 Ma uses modern Natural Earth coastlines and existing inland water; 540 Ma uses terrain-based water. Derived water data is also CC BY 4.0. Water: these representative reconstructions show maximum marine flooding, not lake or coastline boundaries at an exact selected instant. Changes between source ages are visual estimates and do not establish when a basin became isolated or reconnected.
Ocean / marine polygons for shallow-sea correction at 0Ma (modern coastline)
Natural Earth — naturalearthdata.com
Modifications: Used to correct the display of modern coastlines and shallow seas.
Modeled surface temperature, precipitation and wind at 0–540 Ma
Li, X. et al. (2022). A high-resolution climate simulation dataset for the past 540 million years. Scientific Data, 9, 371.
DOI: 10.1038/s41597-022-01490-4
Modifications: Annual surface temperature from CESM (T): a model estimate, not a direct observation of the past. Adapted for visualization, with interpolation between source ages 10 Ma apart. Global surface temperature is an area-weighted annual mean. 0 Ma is pre-industrial; Köppen is an approximate classification based on annual means.
Paleobiology Database (fossil occurrence records)
Peters, S.E. and McClennen, M. (2016). The Paleobiology Database application programming interface. Paleobiology, 42(1), 1-7.
Modifications: Up to 10,000 records sampled per 5 Ma window (0 Ma: 0–2.5 Ma), with supported ancient locations reconstructed. Sampling varies by age, region and taxon; counts are not abundance or biodiversity. Original references are available through PBDB.
Tools for plate-tectonic and ancient-location reconstruction
Müller, R.D. et al. (2018). GPlates: Building a Virtual Earth Through Deep Time. G-cubed, 19.
DOI: 10.1029/2018GC007584
Modifications: Used to reconstruct ancient positions from the models.
0–200 Ma plate boundaries (separate model comparison)
Seton, M. et al. (2012). Global continental and ocean basin reconstructions since 200 Ma. Earth-Science Reviews, 113.
Modifications: Plate boundaries reconstructed at 5 Ma intervals and simplified for display.
0–540 Ma coordinate reconstruction (Scotese 2016 reference frame; per-point validity checked)
Scotese, C.R. (2016). PALEOMAP PaleoAtlas for GPlates, v3. Zenodo.
Modifications: Ancient locations reconstructed for fossils, cities and geological events, within the model's supported locations and ages.
200–540 Ma plate boundary reconstruction
Müller, R.D. et al. (2022). A tectonic-rules-based mantle reference frame since 1 billion years ago – implications for supercontinent cycles and plate–mantle system evolution. Solid Earth, 13, 1127–1159. Model v1.2.4.
Modifications: Plate boundaries reconstructed at 5 Ma intervals and simplified for display.
Taxon silhouettes in fossil details and creature cards
PhyloPic — phylopic.org
Modifications: Resized for display. Each image includes its original attribution and artwork/license links.
Single source for geological boundaries and period names
International Commission on Stratigraphy, International Chronostratigraphic Chart, 2026/06.
Source ↗Modifications: Geological boundaries adapted for the service with translated names and service-selected display colors.
1 Ma summaries of Cenozoic CO₂ proxy records
CenCO2PIP Consortium (2023), Science 382, eadi5177; vetted data v1.02 (2024).
Modifications: Eligible category 1/2 records; median of study medians. Ranges describe samples, not confidence intervals. Empty bins remain unavailable.
Sea-level reconstruction, 0.98–64.82 Ma
Miller, K.G. et al. (2020). Smoothed Cenozoic sea-level relative to modern from deep-sea geochemical and continental margin records [dataset]. PANGAEA.
Modifications: Linear interpolation of supplied smoothed series; no extrapolation. 0 Ma is a present-day 0 m reference.
Present-day map geology at 25 city centers
Macrostrat; Peters et al. (2018). Original map references retained and displayed for each city.
Source ↗Modifications: Selected geology information displayed for each city, retaining original unit names and ages. Not a paleomap or site survey.
Plate boundaries are a separate model comparison. Their reference frame differs from PALEOMAP terrain and coordinates; coastlines may not align.
A flow illustration derived from wind and sea temperature. It is not an ocean circulation simulation; particle speed is not a physical velocity.
Wind: CESM annual mean U/V, 1000 hPa. Atmospheric rim glow is decorative.
Event dates, places, evidence and uncertainties are independently summarized from the linked primary studies. Paper text, figures and genetic sequences are not redistributed. Each paper and its associated data retain their own rights.
Literature reviewed: 2026-09-25
Photographs of separate museum specimens. These are not asserted to be the same specimens as mapped PBDB occurrences. Names and ages retain museum catalog wording.

Anomalina beccariiformis (White, 1928)
CC46806 · Mesozoic / Cretaceous / Late
Smithsonian Institution, National Museum of Natural History

Neocaudites triplistriatus (Edwards, 1944)
PAL172753 · Cenozoic / Neogene / Miocene
Smithsonian Institution, National Museum of Natural History

Bivalvia
PAL653339 · Cenozoic / Quaternary / Pleistocene
Smithsonian Institution, National Museum of Natural History

Amphissa reticulata Dall
PAL651332 · Cenozoic
Smithsonian Institution, National Museum of Natural History

Genus sp
PAL572645b · Cenozoic / Paleogene / Eocene
Smithsonian Institution, National Museum of Natural History

Hyracotherium tapirinum (Cope)
V1076 · Cenozoic / Paleogene / Eocene / Wasatchian
Smithsonian Institution, National Museum of Natural History

Desmoscaphites erdmanni Cobban
PAL106724 · Age not supplied by the museum
Smithsonian Institution, National Museum of Natural History

Habrosaurus dilatus Gilmore, 1928
V17018 · Mesozoic / Cretaceous / Late / Maastrichtian
Smithsonian Institution, National Museum of Natural History

Kritosaurus sp
PAL358555 · Mesozoic / Cretaceous / Late / Campanian
Smithsonian Institution, National Museum of Natural History

Tracheophyta
PAL722538 · Cenozoic / Paleogene / Eocene / Middle
Smithsonian Institution, National Museum of Natural History

Anomalocaris canadensis Whiteaves, 1892
PAL213890 · Paleozoic / Cambrian / Middle
Smithsonian Institution, National Museum of Natural History

Stylemys nebrascensis Leidy, 1851
PAL358863 · Cenozoic / Paleogene / Oligocene
Smithsonian Institution, National Museum of Natural History
12 / 40 photos
Geist Font
Google Fonts (Vercel)
OFL 1.1
Noto Sans CJK Bold / Deep Time Share
Noto Project — modified font used in share images
OFL 1.1
O₂ literature ranges
Mills et al. (2023), Evolution of Atmospheric O₂ Through the Phanerozoic, Revisited, DOI 10.1146/annurev-earth-032320-095425
Original literature summary
생물군/계통수
Compiled from textbooks and literature
Editorially curated
Aurora — Scott Buckley · CC BY 4.0
Edited for looping playback with volume adjustment.
Impact sound: original sound design by Play Deep Time Earth.