In 1969, Dr. Opdyke & Ken Henry used marine core data for a convincing test of the GAD
hypothesis that is central to the use of paleomagnetism in continental
reconstruction. Opdyke’s work with Nick Shackleton in 1973 marked the
beginning of the integration of oxygen isotope stratigraphy and
magnetostratigraphy that has led to current methods of tuning
timescales. Neil pioneered magnetic stratigraphy in terrestrial
(non-marine) sediments and produced some of the most impressive records, notably from Pakistan and southwestern United States. These studies led to a vastly improved time frame for vertebrate evolution and allowed the documentation of mammal migration.
Research interests
Paleomagnetism and its application to tectonics and magnetostratigraphy.
European Geosciences Union Petrus Peregrinus Medal 2008 for pioneering work in magnetic stratigraphy of marine and continental sediments and its contribution to our understanding of the history of the magnetic field and its geological applications.[4]