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Communications Earth & Environment|December 15, 2025
Terrestrial atmospheric ion implantation occurred in the nearside lunar regolith during the history of Earth's dynamoShubhonkar Paramanick, Eric G Blackman, John A Tarduno, et al.Proceedings of the National Academy of Sciences of the United States of America|February 9, 2011
Formation of high-field magnetic white dwarfs from common envelopesJason Nordhaus, Sarah Wellons, David S Spiegel, et al.Communications Earth & Environment|December 7, 2020
Arrival and magnetization of carbonaceous chondrites in the asteroid belt before 4562 million years agoTimothy O'Brien, John A Tarduno, Atma Anand, et al.Communications Earth & Environment|September 9, 2024
A lunar core dynamo limited to the Moon's first ~140 million yearsTinghong Zhou, John A Tarduno, Rory D Cottrell, et al.Plos One|April 18, 2014
Persistent, long-term cerebral white matter changes after sports-related repetitive head impactsJeffrey J Bazarian, Tong Zhu, Jianhui Zhong, et al.Nature Communications|July 29, 2015
Antiquity of the South Atlantic Anomaly and evidence for top-down control on the geodynamoJohn A Tarduno, Michael K Watkeys, Thomas N Huffman, et al.Science Advances|August 5, 2021
Absence of a long-lived lunar paleomagnetosphereJohn A Tarduno, Rory D Cottrell, Kristin Lawrence, et al.Proceedings of the National Academy of Sciences of the United States of America|January 23, 2020
Paleomagnetism indicates that primary magnetite in zircon records a strong Hadean geodynamoJohn A Tarduno, Rory D Cottrell, Richard K Bono, et al.Pageof 2