Late Cretaceous

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Late/Upper Cretaceous
100.5 – 66.0 Ma PreꞒ Ꞓ O S D C P T J K Pg N
A map of Earth as it appeared 85 million years ago during the Late Cretaceous Epoch, Santonian Age
Chronology
−140 — – −130 — – −120 — – −110 — – −100 — – −90 — – −80 — – −70 — – Mesozoic C Z J Cretaceous P g Late J Early Late Paleocene Berriasian Valanginian Hauterivian Barremian Aptian Albian Cenomanian Turonian Coniacian Santonian Campanian Maastrichtian         ← K-Pg mass extinction Subdivision of the Cretaceous according to the ICS, as of 2023.[1] Vertical axis scale: millions of years ago.
Etymology
Chronostratigraphic name	Upper Cretaceous
Geochronological name	Late Cretaceous
Name formality	Formal
Usage information
Celestial body	Earth
Regional usage	Global (ICS)
Time scale(s) used	ICS Time Scale
Definition
Chronological unit	Epoch
Stratigraphic unit	Series
Time span formality	Formal
Lower boundary definition	FAD of the Planktonic Foraminifer Rotalipora globotruncanoides
Lower boundary GSSP	Mont Risoux, Hautes-Alpes, France 44°23′33″N 5°30′43″E / 44.3925°N 5.5119°E / 44.3925; 5.5119
Lower GSSP ratified	2002[2]
Upper boundary definition	Iridium enriched layer associated with a major meteorite impact and subsequent K-Pg extinction event
Upper boundary GSSP	El Kef Section, El Kef, Tunisia 36°09′13″N 8°38′55″E / 36.1537°N 8.6486°E / 36.1537; 8.6486
Upper GSSP ratified	1991

The Late Cretaceous (100.5–66 Ma) is the younger of two epochs into which the Cretaceous Period is divided in the geologic time scale. Rock strata from this epoch form the Upper Cretaceous Series. The Cretaceous is named after creta, the Latin word for the white limestone known as chalk. The chalk of northern France and the white cliffs of south-eastern England date from the Cretaceous Period.^[3]