| mya | Event | % Correct |
|---|---|---|
| 252 | Permian-Triassic | 96%
|
| 66 | Cretaceous–Paleogene | 91%
|
| 201 | Triassic-Jurassic | 87%
|
| 488 | Cambrian-Ordovician | 78%
|
| 145 | End-Jurassic | 78%
|
| 0 | Holocene | 78%
|
| 445 | Late Ordovician | 74%
|
| 372 | Late Devonian | 70%
|
| 2 | Pliocene–Pleistocene | 48%
|
| 305 | Carboniferous rainforest collapse | 43%
|
| 33.9 | Eocene–Oligocene | 43%
|
| 14.5 | Middle Miocene | 43%
|
| 0.129 | Quaternary | 35%
|
| 2400 | Great Oxidation | 30%
|
| 94 | Cenomanian-Turonian | 22%
|
| 542 | End-Ediacaran | 22%
|
| 230 | Carnian Pluvial | 17%
|
| 117 | Aptian | 13%
|
| 260 | Captinian | 9%
|
| 517 | End-Botomian | 9%
|
| 359 | Hangenburg | 9%
|
| 388 | Kačak | 9%
|
| 420 | Lau | 9%
|
| 273 | Olson's extinction | 9%
|
| 325 | Serpukhovian | 9%
|
| 384 | Taghanic | 9%
|
| 186 | Toarcian Oceanic Anoxic Event | 9%
|
| 502 | Dresbachian | 4%
|
| 428 | Ireviken | 4%
|
| 424 | Mulde | 4%
|
| 247 | Olenekian-Anisian | 4%
|
| 249 | Smithian-Spathian | 4%
|