Relative paleointensity (RPI) and oxygen isotope stratigraphy at IODP Site U1308: North Atlantic RPI stack for 1.2-2.2 Ma (NARPI-2200) and age of the Olduvai Subchron

Quaternary Science Reviews

Volumn 131, Issue , 2016, Pages 1-19

  Channell, J E T ^a   Hodell, D A ^b   Curtis, J H ^a  

^a UNIVERSITY OF FLORIDA   (United States)

^b UNIVERSITY OF CAMBRIDGE   (United Kingdom)

Author keywords

Age of Olduvai Subchron; Late Pliocene; North Atlantic; Quaternary; Relative paleointensity; Stable isotopes

Indexed keywords

CALIBRATION; GEOMAGNETISM; MAGNETIC POLARITY; OCEANOGRAPHY; OXYGEN; SEDIMENTATION; STRATIGRAPHY;

AGE OF OLDUVAI SUBCHRON; LATE PLIOCENE; NORTH ATLANTIC; QUATERNARY; RELATIVE PALEOINTENSITY; STABLE ISOTOPES;

ISOTOPES;

DEPOSITIONAL SEQUENCE; GEOCHRONOLOGY; GEOMAGNETISM; MAGNETIC REVERSAL; MARINE ISOTOPE STAGE; OXYGEN ISOTOPE; PALEOCEANOGRAPHY; PLEISTOCENE; PLIOCENE; SEDIMENTATION RATE; STABLE ISOTOPE; STRATIGRAPHIC CORRELATION; TIMESCALE;

ATLANTIC OCEAN; ATLANTIC OCEAN (NORTH); PORCUPINE ABYSSAL PLAIN;

EID: 84946020162     PISSN: 02773791     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.quascirev.2015.10.011     Document Type: Review

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