Valanginian

In the geologic timescale, the Valanginian is an age or stage of the Early or Lower Cretaceous.It is named after Valangin, a small town north of Neuchâtel in the Jura Mountains of Switzerland.The base of the Valanginian is at the first appearance of calpionellid species Calpionellites darderi in the stratigraphic column.The top of the Valanginian (the base of the Hauterivian) is at the first appearance of the ammonite genus Acanthodiscus.The Upper substage begins at the first appearance of ammonite species Saynoceras verrucosum and the major marine transgression Va3.
PreꞒMesozoicCretaceousTithonianBerriasianHauterivianBarremianAptianAlbianCenomanianTuronianConiacianSantonianCampanianMaastrichtianDanianK-Pg massextinctionMillions of years agoCalpionellidCalpionellites darderiMontbrun-les-BainsDrômeFranceBetic CordilleraAmmoniteAcanthodiscusLa Charcegeologic timescaleEarly or Lower CretaceousValanginNeuchâtelJura MountainsSwitzerlandmarine transgressionTethys domainbiozonesNeocomites peregrinusAngiospermaeInternational Commission on StratigraphyBibcodeCambridge University PressCretaceous PeriodLower/Early CretaceousUpper/Late CretaceousGeological history of EarthCenozoic Era(present–66.0 Ma)Quaternary (present–2.58 Ma)Holocene (present–11.7 ka)Pleistocene (11.7 ka–2.58 Ma)Neogene (2.58–23.0 Ma)Pliocene (2.59–5.33 Ma)Miocene (5.33–23.0 Ma)Paleogene (23.0–66.0 Ma)Oligocene (23.0–33.9 Ma)Eocene (33.9–56.0 Ma)Paleocene (56.0–66.0 Ma)Mesozoic Era(66.0–252 Ma)Cretaceous (66.0–145 Ma)Late (66.0–100 Ma)Early (100–145 Ma)Jurassic (145–201 Ma)Late (145–164 Ma)Middle (164–174 Ma)Early (174–201 Ma)Triassic (201–252 Ma)Late (201–237 Ma)Middle (237–247 Ma)Early (247–252 Ma)Paleozoic Era(252–539 Ma)Permian (252–299 Ma)Lopingian (252–260 Ma)Guadalupian (260–272 Ma)Cisuralian (272–299 Ma)Carboniferous (299–359 Ma)Pennsylvanian (299–323 Ma)Mississippian (323–359 Ma)Devonian (359–419 Ma)Late (359–383 Ma)Middle (383–393 Ma)Early (393–419 Ma)Silurian (419–444 Ma)Pridoli (419–423 Ma)Ludlow (423–427 Ma)Wenlock (427–433 Ma)Llandovery (433–444 Ma)Ordovician (444–485 Ma)Late (444–458 Ma)Middle (458–470 Ma)Early (470–485 Ma)Cambrian (485–539 Ma)Furongian (485–497 Ma)Miaolingian (497–509 Ma)Series 2 (509–521 Ma)Terreneuvian (521–539 Ma)Proterozoic Eon(539 Ma–2.5 Ga)Neoproterozoic (539 Ma–1 Ga)Ediacaran (539–635 Ma)Cryogenian (635–720 Ma)Tonian (720 Ma–1 Ga)Mesoproterozoic (1–1.6 Ga)Stenian (1–1.2 Ga)Ectasian (1.2–1.4 Ga)Calymmian (1.4–1.6 Ga)Paleoproterozoic (1.6–2.5 Ga)Statherian (1.6–1.8 Ga)Orosirian (1.8–2.05 Ga)Rhyacian (2.05–2.3 Ga)Siderian (2.3–2.5 Ga)Archean Eon (2.5–4 Ga)Neoarchean (2.5–2.8 Ga)Mesoarchean (2.8–3.2 Ga)Paleoarchean (3.2–3.6 Ga)Eoarchean (3.6–4 Ga)Hadean Eon (4–4.6 Ga)Geologic time scalegeochronology