Earth’s magnetic field remained weak for 40 million years after the Cambrian radiation.
Science Advances · 12(30), eaeg2325
DOI: 10.1126/sciadv.aeg2325
1,596 downloads on Science Advances · as at 25 September 2026
Research record / 2021–2026
11 peer-reviewed papers, including seven as first author. Research spanning Earth’s magnetic history, experimental methods, global datasets and the geodynamo.
Science Advances · 12(30), eaeg2325
DOI: 10.1126/sciadv.aeg2325
1,596 downloads on Science Advances · as at 25 September 2026
Nature Geoscience · 19(3), 345–352
DOI: 10.1038/s41561-025-01910-1
Geophysical Journal International · 244(2)
DOI: 10.1093/gji/ggaf490
Journal of Geophysical Research: Solid Earth · 130, e2024JB030314
DOI: 10.1029/2024JB030314
Earth and Planetary Science Letters · 648, 119110
DOI: 10.1016/j.epsl.2024.119110
Frontiers in Earth Science · 11, 1188528
DOI: 10.3389/feart.2023.1188528
Earth and Planetary Science Letters · 595, 117757
DOI: 10.1016/j.epsl.2022.117757
Geophysical Journal International · 229, 522–545
DOI: 10.1093/gji/ggab490
Geochemistry, Geophysics, Geosystems · 22(10), e2021GC009990
DOI: 10.1029/2021GC009990
Frontiers in Earth Science · 9, 701863
DOI: 10.3389/feart.2021.701863
Geophysical Journal International · 226(1)
DOI: 10.1093/gji/ggab090
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