mya | Event | % Correct |
---|---|---|
66 | Cretaceous–Paleogene | 91%
|
252 | Permian-Triassic | 91%
|
488 | Cambrian-Ordovician | 82%
|
145 | End-Jurassic | 73%
|
0 | Holocene | 73%
|
372 | Late Devonian | 73%
|
445 | Late Ordovician | 73%
|
201 | Triassic-Jurassic | 73%
|
2 | Pliocene–Pleistocene | 45%
|
33.9 | Eocene–Oligocene | 36%
|
14.5 | Middle Miocene | 36%
|
305 | Carboniferous rainforest collapse | 27%
|
0.129 | Quaternary | 27%
|
117 | Aptian | 9%
|
230 | Carnian Pluvial | 9%
|
94 | Cenomanian-Turonian | 9%
|
542 | End-Ediacaran | 9%
|
2400 | Great Oxidation | 9%
|
388 | Kačak | 9%
|
420 | Lau | 9%
|
325 | Serpukhovian | 9%
|
384 | Taghanic | 9%
|
186 | Toarcian Oceanic Anoxic Event | 9%
|
260 | Captinian | 0%
|
502 | Dresbachian | 0%
|
517 | End-Botomian | 0%
|
359 | Hangenburg | 0%
|
428 | Ireviken | 0%
|
424 | Mulde | 0%
|
247 | Olenekian-Anisian | 0%
|
273 | Olson's extinction | 0%
|
249 | Smithian-Spathian | 0%
|
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