<<

of the

Age Eon Period Period Paleogeographic Maps Earth History (Ma) Era (Ma) * / 2.6 5.3 L 100 M E

Jurassic Neogene 200 23 L E 34 Early Neogene 300 L Cenozoic M

400 E Paleogene L 56 PaleozoicOrdovician M 500 E 66

Ediacaran 600 Late 700 100

800

900

Tonian Cretaceous Early 1000 1100 146 1200 Late 161 Mesozoic 1300 Middle 176 1400 Early 1500 200 1600

Proterozoic Late 1700 228 1800 Triassic Middle 1900 245 Early 251 2000 260 / 2100 271

Paleoproterozoic 2200

Permian Middle Permian

2300 299 Late 2400 Middle Moscovian Penn-

sylvanian Early 318 2500 Late

2600 Middle Visean Carboniferous

2700

Neoarchean Early Middle Mississippian

2800 359

2900 Late 385 3000 Middle 398 3100 Devonian

Paleozoic Early 3200 416 Early Middle Devonian Pridoli 419 / 423 3300 Wenlock / 428 Llandovery 3400 Silurian / 444

3500

Paleoarchean Late 461 3600 Middle 472

3700 Early Middle Ordovician 488 3800 Stage 10 Stage 9 501

Eoarchean Stage 7 3900 3 Stage 5 510 Stage 4 Map Legend 4000 Series 2 Stage 3 Spreading Center O Mountain Belt Or 521 (mountain- Lower limit is Zone building episode) AFR IND 4100 not defined Series 1 NAM AUS SAM BAL SIB Stage 1 542 Gon

International divisions of geologic (, periods, epochs, stages) are standardized by the International Commission on Stratigraphy (ICS, www.stratigraphy.org). The color scheme of the Commission for the Geological Map of the World is shown for these divisions, This poster was developed in collaboration with the United States and their numerical ages are from "A 2004" (Gradstein et al., Cambridge University Press). Paleogeographic maps Geological Survey and with the CHRONOS program (sponsored by Copyright © 2007, were provided courtesy of Ron Blakey with plate positions modified from Chris Scotese. The of is modified from John the U.S. National Science Foundation). Gurche’s painting “Tower of Time” (© Smithsonian Institution). This chart was compiled and drafted by Gabi Ogg and Bruce Wardlaw. International Commission * The status of the Quaternary is not yet decided. Its base may be assigned as the base of the Gelasian and extend the base of the on Stratigraphy ICS Pleistocene to 2.6 Ma.