List of flood basalt provinces
Representative continental flood basalts and oceanic plateaus, together forming a listing of large igneous provinces:
Era | Period | Epoch | Age | Start, mya | Event | Notes |
Cenozoic | Quaternary | Holocene | 0.0117 | |||
Cenozoic | Quaternary | Pleistocene | Upper | 0.126 | ||
Cenozoic | Quaternary | Pleistocene | Middle | 0.781 | Australasian strewnfield Lake Bosumtwi | Brunhes–Matuyama reversal Jaramillo reversal |
Cenozoic | Quaternary | Pleistocene | Calabrian | 1.806* | Olduvai reversal | |
Cenozoic | Quaternary | Pleistocene | Gelasian | 2.588* | Chilcotin Plateau Basalts | Ice age Gauss-Matuyama reversal |
Cenozoic | Neogene | Pliocene | Piacenzian/Blancan | 3.600* | Gilbert-Gauss geomagnetic reversal | |
Cenozoic | Neogene | Pliocene | Zanclean | 5.333* | Zanclean flood | |
Cenozoic | Neogene | Miocene | Messinian | 7.246* | Chilcotin Plateau Basalts | |
Cenozoic | Neogene | Miocene | Tortonian | 11.62* | ||
Cenozoic | Neogene | Miocene | Serravallian | 13.82* | ||
Cenozoic | Neogene | Miocene | Langhian | 15.97 | M. Miocene disruption Columbia River Basalt Group Chilcotin Plateau Basalts | Increased Antarctic deep waters Yellowstone hotspot Nördlinger Ries |
Cenozoic | Neogene | Miocene | Burdigalian | 20.44 | ||
Cenozoic | Neogene | Miocene | Aquitanian | 23.03* | Shield volcanoes of Ethiopia | Antarctic ice sheet complete |
Cenozoic | Paleogene | Oligocene | Chattian | 28.1 | Ethiopian and Yemen traps | Fish Canyon Tuff |
Cenozoic | Paleogene | Oligocene | Rupelian | 33.9* | Chesapeake Bay impact crater | Antarctic ice sheet expands Eocene–Oligocene extinction event |
Cenozoic | Paleogene | Eocene | Priabonian | 38.0 | - | |
Cenozoic | Paleogene | Eocene | Bartonian | 41.3 | ||
Cenozoic | Paleogene | Eocene | Lutetian | 47.8* | Antarctic ice sheet begins | |
Cenozoic | Paleogene | Eocene | Ypresian | 56.0* | N. Atlantic IP Phase II | |
Cenozoic | Paleogene | Paleocene | Thanetian | 59.2* | ||
Cenozoic | Paleogene | Paleocene | Selandian | 61.6* | N. Atlantic IP | Iceland hotspot |
Cenozoic | Paleogene | Paleocene | Danian | 65.5 ± 0.3* | Chicxulub Crater Deccan Traps | Cretaceous–Paleogene extinction event Shiva crater |
Mesozoic | Cretaceous | Upper | Maastrichtian | 72.1 ± 0.2* | ||
Mesozoic | Cretaceous | Upper | Campanian | 83.6 ± 0.2 | Caribbean lIP Caribbean lIP | |
Mesozoic | Cretaceous | Upper | Santonian | 86.3 ± 0.5 | ||
Mesozoic | Cretaceous | Upper | Coniacian | 89.8 ± 0.3 | High Arctic LIP Caribbean lIP Ontong Java Plateau | Galápagos hotspot |
Mesozoic | Cretaceous | Upper | Turonian | 93.5 ± 0.8* | Cenomanian-Turonian boundary event Madagascar flood basalt | |
Mesozoic | Cretaceous | Upper | Cenomanian | 100.5* | ||
Mesozoic | Cretaceous | Lower | Albian | c. 113.0 | Kerguelen Plateau Rajmahal Traps | Kerguelen hotspot |
Mesozoic | Cretaceous | Lower | Aptian | c. 125.0 | Selli Event Ontong Java Plateau | Louisville hotspot |
Mesozoic | Cretaceous | Lower | Barremian | c. 129.4 | High Arctic LIP | |
Mesozoic | Cretaceous | Lower | Hauterivian | c. 132.9 | ||
Mesozoic | Cretaceous | Lower | Valanginian | c. 139.8 | Paraná and Etendeka traps | Tristan hotspot |
Mesozoic | Cretaceous | Lower | Berriasian | c. 145.0 | Glaciations End-Jurassic extinction | |
Mesozoic | Jurassic | Upper | Tithonian | 152.1 ± 0.9 | ||
Mesozoic | Jurassic | Upper | Kimmeridgian | 157.3 ± 1.0 | ||
Mesozoic | Jurassic | Upper | Oxfordian | 163.5 ± 1.0 | ||
Mesozoic | Jurassic | Middle | Callovian | 166.1 ± 1.2 | ||
Mesozoic | Jurassic | Middle | Bathonian | 168.3 ± 1.3* | ||
Mesozoic | Jurassic | Middle | Bajocian | 170.3 ± 1.4* | ||
Mesozoic | Jurassic | Middle | Aalenian | 174.1 ± 1.0* | ||
Mesozoic | Jurassic | Lower | Toarcian | 182.7 ± 0.7 | early Toarcian anoxic event Karoo-Ferrar | Pliensbachian-Toarcian extinction Formed as Gondwana broke up |
Mesozoic | Jurassic | Lower | Pliensbachian | 190.8 ± 1.0* | ||
Mesozoic | Jurassic | Lower | Sinemurian | 199.3 ± 0.3* | C. Atlantic magmatic province | |
Mesozoic | Jurassic | Lower | Hettangian | 201.3 ± 0.2* | Central Atlantic magmatic province | Formed as Pangea broke up Triassic–Jurassic extinction event |
Mesozoic | Triassic | Upper | Rhaetian | c. 208.5 | ||
Mesozoic | Triassic | Upper | Norian | c. 228 | Wrangellia flood basalts | |
Mesozoic | Triassic | Upper | Carnian | c. 235* | ||
Mesozoic | Triassic | Middle | Ladinian | c. 242* | ||
Mesozoic | Triassic | Middle | Anisian | 247.2 | ||
Mesozoic | Triassic | Lower | Olenekian | 251.2 | ||
Mesozoic | Triassic | Lower | Induan | 252.2 ± 0.5* | Siberian Traps | Permian–Triassic extinction event |
Paleozoic | Permian | Lopingian | Changhsingian | 254.2 ± 0.1* | ||
Paleozoic | Permian | Lopingian | Wuchiapingian | 259.9 ± 0.4* | Emeishan Traps | end-Capitanian/Guadalupian Extinction |
Paleozoic | Permian | Guadalupian | Capitanian | 265.1 ± 0.4* | ||
Paleozoic | Permian | Guadalupian | Wordian/Kazanian | 268.8 ± 0.5* | ||
Paleozoic | Permian | Guadalupian | Roadian/Ufimian | 272.3 ± 0.5* | Olson's Extinction Late Devonian extinction | |
Paleozoic | Permian | Cisuralian | Kungurian | 279.3 ± 0.6 | ||
Paleozoic | Permian | Cisuralian | Artinskian | 290.1 ± 0.1 | ||
Paleozoic | Permian | Cisuralian | Sakmarian | 295.5 ± 0.4 | ||
Paleozoic | Permian | Cisuralian | Asselian | 298.9 ± 0.2* | Skagerrak-Centered LIP | Pangaea |
Paleozoic | Carbon- iferous/ Pennsyl- vanian | Upper | Gzhelian | 303.7 ± 0.1 | ||
Paleozoic | Carbon- iferous/ Pennsyl- vanian | Upper | Kasimovian | 307.0 ± 0.1 | Carboniferous Rainforest Collapse | |
Paleozoic | Carbon- iferous/ Pennsyl- vanian | Middle | Moscovian | 315.2 ± 0.2 | ||
Paleozoic | Carbon- iferous/ Pennsyl- vanian | Lower | Bashkirian | 323.2 ± 0.4* | ||
Paleozoic | Carbon- iferous/ Missis- sippian | Upper | Serpukhovian | 330.9 ± 0.2 | ||
Paleozoic | Carbon- iferous/ Missis- sippian | Middle | Viséan | 346.7 ± 0.4* | ||
Paleozoic | Carbon- iferous/ Missis- sippian | Lower | Tournaisian | 358.9 ± 0.4* | Hangenberg event | Late Devonian extinction |
Paleozoic | Devonian | Upper | Famennian | 372.2 ± 1.6* | Kellwasser_event Viluy traps | Late Devonian extinction |
Paleozoic | Devonian | Upper | Frasnian | 382.7 ± 1.6* | ||
Paleozoic | Devonian | Middle | Givetian | 387.7 ± 0.8* | ||
Paleozoic | Devonian | Middle | Eifelian | 393.3 ± 1.2* | ||
Paleozoic | Devonian | Lower | Emsian | 407.6 ± 2.6* | ||
Paleozoic | Devonian | Lower | Pragian | 410.8 ± 2.8* | ||
Paleozoic | Devonian | Lower | Lochkovian | 419.2 ± 3.2* | ||
Paleozoic | Silurian | Pridoli | 423.0 ± 2.3* | Lau event | ||
Paleozoic | Silurian | Ludlow/Cayugan | Ludfordian | 425.6 ± 0.9* | ||
Paleozoic | Silurian | Ludlow/Cayugan | Gorstian | 427.4 ± 0.5* | Mulde event | |
Paleozoic | Silurian | Wenlock | Homerian/Lockportian | 430.5 ± 0.7* | ||
Paleozoic | Silurian | Wenlock | Sheinwoodian/Tonawandan | 433.4 ± 0.8* | Ireviken event | |
Paleozoic | Silurian | Llandovery/ Alexandrian | Telychian/Ontarian | 438.5 ± 1.1* | ||
Paleozoic | Silurian | Llandovery/ Alexandrian | Aeronian | 440.8 ± 1.2* | ||
Paleozoic | Silurian | Llandovery/ Alexandrian | Rhuddanian | 443.4 ± 1.5* | Ordovician–Silurian extinction event | |
Paleozoic | Ordovician | Upper | Hirnantian | 445.2 ± 1.4* | Pre-Devonian Traps | |
Paleozoic | Ordovician | Upper | Katian | 453.0 ± 0.7* | ||
Paleozoic | Ordovician | Upper | Sandbian | 458.4 ± 0.9* | ||
Paleozoic | Ordovician | Middle | Darriwilian | 467.3 ± 1.1* | ||
Paleozoic | Ordovician | Middle | Dapingian | 470.0 ± 1.4* | ||
Paleozoic | Ordovician | Lower | Floian | 477.7 ± 1.4* | ||
Paleozoic | Ordovician | Lower | Tremadocian | 485.4 ± 1.9* | ||
Paleozoic | Cambrian | Furongian | Stage 10 | c. 489.5 | Cambrian–Ordovician extinction event | |
Paleozoic | Cambrian | Furongian | Jiangshanian | c. 494* | ||
Paleozoic | Cambrian | Furongian | Paibian | c. 497* | ||
Paleozoic | Cambrian | Series 3 | Guzhangian | c. 500.5* | ||
Paleozoic | Cambrian | Series 3 | Drumian | c. 504.5* | ||
Paleozoic | Cambrian | Series 3 | Stage 5 | c. 509 | ||
Paleozoic | Cambrian | Series 2 | Stage 4 | c. 514 | ||
Paleozoic | Cambrian | Series 2 | Stage 3 | c. 521 | ||
Paleozoic | Cambrian | Terreneuvian | Stage 2 | c. 529 | Cambrian explosion | |
Paleozoic | Cambrian | Terreneuvian | Fortunian | 541.0 ± 1.0* | End-Ediacaran extinction | |
Neo- proterozoic | Ediacaran | c. 635* | Long Range dikes | formed as Iapetus Ocean began | ||
Neo- proterozoic | Cryogenian | 850 | Franklin LIP | Snowball Earth | ||
Neo- proterozoic | Tonian | 1000 | Warakurna LIP | |||
Meso- proterozoic | Stenian | 1200 | Midcontinent Rift System Mackenzie LIP | Rodinia | ||
Meso- proterozoic | Ectasian | 1400 | ||||
Meso- proterozoic | Calymmian | 1600 | ||||
Paleo- proterozoic | Statherian | 1800 | Circum-Superior Belt Winagami sill complex | |||
Paleo- proterozoic | Orosirian | 2050 | Kapuskasing and Marathon dike swarm Fort Frances dike swarm Vredefort crater | |||
Paleo- proterozoic | Rhyacian | 2300 | Ungava magmatic event | Huronian glaciation | ||
Paleo- proterozoic | Siderian | 2500 | Matachewan dike swarm Mistassini dike swarm | Great Oxygenation Event | ||
Neoarchean | 2800 | |||||
Mesoarchean | 3200 | |||||
Paleoarchean | 3600 | Kaapvaal craton | Vaalbara | |||
Eoarchean | ||||||
Early Imbrian | c. 3850 | |||||
Nectarian | c. 3920 | lunar basins form | ||||
Basin Groups | c. 4150 | Acasta Gneiss | Late Heavy Bombardment | |||
Cryptic | c. 4600 | Oldest minerals. Earth surface solidifies. |