Gauss–Matuyama geomagnetic reversal

E179503

The Gauss–Matuyama geomagnetic reversal was a major event in Earth's history when the planet's magnetic field flipped polarity around 2.6 million years ago, marking a key boundary used in geological time scales.

All labels observed (5)

How this entity was disambiguated

Statements (44)

Predicate Object
instanceOf geological event ⓘ
geomagnetic reversal ⓘ
affects orientation of remanent magnetization in rocks ⓘ
documentedIn International Commission on Stratigraphy timescales ⓘ
evidenceFoundIn lava flows ⓘ
marine sediment cores ⓘ
oceanic crust magnetic anomalies ⓘ
hasAgeUncertainty tens of thousands of years ⓘ
hasApproximateTime about 2.6 million years ago ⓘ
hasCause dynamics of Earth’s liquid outer core ⓘ
hasEffect reversal of geomagnetic field direction at Earth’s surface ⓘ
hasEndTime approximately 2.58 million years ago ⓘ
hasFollowingEvent Matuyama reversed chron ⓘ
hasGlobalExtent global ⓘ
hasMagneticChronCode C2r ⓘ
hasPolarityChangeFrom normal polarity ⓘ
hasPolarityChangeTo reversed polarity ⓘ
hasPreviousEvent Gauss normal chron ⓘ
hasStartTime approximately 2.72 million years ago ⓘ
hasTimescaleDesignation C2An–C2r boundary ⓘ
identifiedBy paleomagnetic studies ⓘ
isKeyMarkerFor Pliocene–Pleistocene climate transition ⓘ
onset of Northern Hemisphere glaciation ⓘ
locatedIn Earth’s outer core magnetic field system ⓘ
marksBoundaryBetween Pleistocene ⓘ
linked to: Pleistocene epoch

Pliocene ⓘ
linked to: Pliocene epoch
namedAfter Carl Friedrich Gauss ⓘ
Motonori Matuyama ⓘ
occursIn Pleistocene epoch ⓘ
Pliocene epoch ⓘ
partOf geomagnetic polarity timescale ⓘ
precedes Olduvai normal subchron ⓘ
linked to: Olduvai Gorge
relatedTo Matuyama–Brunhes geomagnetic reversal ⓘ
separates Gauss normal chron ⓘ
Matuyama reversed chron ⓘ
studiedInDiscipline geochronology ⓘ
paleomagnetism ⓘ
stratigraphy ⓘ
usedAsBoundaryIn geomagnetic polarity timescale ⓘ
global stratigraphic charts ⓘ
usedAsChronostratigraphicMarkerFor Quaternary onset ⓘ
usedFor dating of geological and climatic records ⓘ
global correlation of sedimentary sequences ⓘ
usedToDefine Pliocene–Pleistocene boundary ⓘ
linked to: Pliocene epoch

How these facts were elicited

Referenced by (7)

Full triples — surface form annotated when it differs from this entity's canonical label.

Quaternary period → baseDefinedBy → Gauss–Matuyama geomagnetic reversal ⓘ
Gauss–Matuyama geomagnetic reversal → relatedTo → Matuyama–Brunhes geomagnetic reversal ⓘ
linked to: Gauss–Matuyama geomagnetic reversal
Motonori Matuyama → hasHonorificEponym → Matuyama–Brunhes boundary ⓘ
linked to: Gauss–Matuyama geomagnetic reversal
Matuyama reversed chron → follows → Gauss–Matuyama reversal ⓘ
linked to: Gauss–Matuyama geomagnetic reversal
Matuyama reversed chron → lowerBoundaryDefinedBy → Gauss–Matuyama reversal ⓘ
linked to: Gauss–Matuyama geomagnetic reversal
C2r → assignedTo → Gauss–Matuyama geomagnetic reversal interval ⓘ
linked to: Gauss–Matuyama geomagnetic reversal
C2r → correspondsTo → Gauss–Matuyama geomagnetic reversal ⓘ