Play Deep Time Earth is built on the following open datasets and tools.
Paleodigital Elevation Models (0–540 Ma heightmaps)
Scotese, C.R. and Wright, N.M. (2018). PALEOMAP Paleodigital Elevation Models (PaleoDEMS) for the Phanerozoic.
Modifications: NetCDF → 8-bit heightmap → 1024/2048px lossless WebP. Historical 0–50Ma strait dilation and age-dependent processing order retained; modern Natural Earth mask only at 0Ma
Ocean / marine polygons for shallow-sea correction at 0Ma (modern coastline)
Natural Earth — naturalearthdata.com
Modifications: ne_10m_ocean + ne_10m_marine_polys GeoJSON converted to 4096×2048 boolean mask, applied as sea overlay in the final heightmap stage
0–540 Ma surface temperature / precipitation / wind (55 snapshots, 10 Ma → 109 snapshots interpolated to 5 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. NetCDF → lossless RGB WebP on the native 288×192 grid (8-bit quantization), linearly interpolated from 10 Ma to 5 Ma. The global surface-temperature indicator is the area-weighted annual mean. 0 Ma is pre-industrial; Köppen is a simplified annual-mean approximation. Wind uses separate textures.
Paleobiology Database (fossil occurrence records)
Peters, S.E. and McClennen, M. (2016). The Paleobiology Database application programming interface. Paleobiology, 42(1), 1-7.
Modifications: Explicit overlap query in 5 Ma windows (0 Ma: 0–2.5 Ma). At most 10,000 sampled by group, region and collection; only valid reconstructed points shown. Age intervals and taxon/collection/reference IDs preserved. Counts are not abundance or biodiversity.
Plate-tectonic coordinate reconstruction (run locally)
Müller, R.D. et al. (2018). GPlates: Building a Virtual Earth Through Deep Time. G-cubed, 19.
DOI: 10.1029/2018GC007584
Modifications: Coordinates pre-computed locally with PyGPlates and stored as static JSON
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-boundary topology resolved with PyGPlates at 5 Ma intervals; coordinates rounded to 0.1° and stored as static JSON.
0–540 Ma coordinate reconstruction (Scotese 2016 reference frame; per-point validity checked)
Scotese, C.R. (2016). PALEOMAP PaleoAtlas for GPlates, v3. Zenodo.
Modifications: Pre-rotated fossil/city/geo_event coordinates with PyGPlates and stored as static JSON
200–540 Ma plate boundary topology
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-boundary topology resolved with PyGPlates at 5 Ma intervals; coordinates rounded to 0.1° and stored as static JSON.
Taxon silhouettes (on request in fossil details; also in creature cards — runtime API)
PhyloPic — phylopic.org
Modifications: Runtime API; preserves original attribution (distinct from uploader), artwork UUID/build and artwork/license links. Thumbnails resized.
Single source for geological boundaries and period names
International Commission on Stratigraphy, International Chronostratigraphic Chart, 2026/06.
Source ↗Modifications: Period boundaries extracted into JSON with display colors and localized names
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.
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.
CC0 examples from Smithsonian NMNH. 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
Hyracotherium tapirinum (Cope)
V1076 · Cenozoic / Paleogene / Eocene / Wasatchian
Smithsonian Institution, National Museum of Natural History
Platycarya americana Hickey
PAL606437 · Cenozoic / Paleogene / Eocene
Smithsonian Institution, National Museum of Natural History
Porzana astrictocarpus Olson
PAL175893 · Cenozoic / Recent
Smithsonian Institution, National Museum of Natural History
Neocaudites triplistriatus (Edwards, 1944)
PAL172753 · Cenozoic / Neogene / Miocene
Smithsonian Institution, National Museum of Natural History
Amphissa reticulata Dall
PAL651332 · Cenozoic
Smithsonian Institution, National Museum of Natural History
Geist Font
Google Fonts (Vercel)
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
Introduction edited into a 60-second loop with a crossfade and volume adjustment.
Impact: original noise and sine-wave sound design by Play Deep Time Earth.
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