Matuyama reversed chron

E675179

The Matuyama reversed chron is a long interval of predominantly reversed geomagnetic polarity that followed the Gauss–Matuyama reversal and lasted from about 2.58 to 0.78 million years ago.

All labels observed (2)

Label Occurrences
Matuyama reversed chron canonical 2
Matuyama chron 1

How this entity was disambiguated

Statements (30)

Predicate Object
instanceOf geomagnetic chron
reversed polarity interval
boundaryEvent Brunhes–Matuyama reversal
chronCode C2r
contains Jaramillo subchron
Olduvai subchron
duration about 1.8 million years
endTime about 0.78 million years ago
era Cenozoic
evidenceFrom lava flow magnetization
marine magnetic anomalies
sedimentary rock remanent magnetization
fieldType dipolar-dominated geomagnetic field
follows Gauss–Matuyama reversal
hasPolarity reversed
includesAge Pleistocene
lowerBoundaryDefinedBy Gauss–Matuyama reversal
magneticFieldConfiguration south magnetic pole near geographic north
namedAfter Motonori Matuyama
partOf Cenozoic geomagnetic polarity timescale
period Quaternary
polarityRelativeToPresent opposite
precededBy Gauss normal chron
precedes Brunhes normal chron
startTime about 2.58 million years ago
upperBoundaryDefinedBy Brunhes–Matuyama reversal
usedFor dating sedimentary sequences
dating volcanic rocks
geologic time correlation
usedIn magnetostratigraphy

How these facts were elicited

Referenced by (3)

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

Gauss normal chron precedes Matuyama reversed chron
C2r relatedTo Matuyama chron
linked to: Matuyama reversed chron