The Snowball Earth hypothesis can be confirmed or refuted through paleomagnetic data
Paleomagnetic data are routinely used in geological studies to constrain the latitude, timing, and global extent of Neoproterozoic glacial deposits associated with the Snowball Earth hypothesis.
The claim is specific, empirical, and testable. The retrieved literature directly applies paleomagnetic and rock magnetic data to test and refine global paleogeographic reconstructions during the Cryogenian and Ediacaran periods, supporting the premise that paleomagnetism is instrumental for evaluating the hypothesis.
Wang R, Shen B, Lang X, Wen B, Mitchell RN, Ma H, Yin Z, Peng Y, Liu Y, Zhou C. A Great late Ediacaran ice age.. 2023. https://doi.org/10.1093/nsr/nwad117
Paper [0] utilizes paleomagnetic constraints to evaluate low-latitude glaciations and test the global synchronicity of Neoproterozoic glacial deposits.
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Thales Pescarini, et al.. Supplemental Material: Paleomagnetic investigation of the basal Maieberg Formation (Namibia) cap carbonate sequence (635 Ma): Implications for Snowball Earth postglacial dynamics. 2024. https://doi.org/10.1130/gsab.s.25571712.v1
Paper [9] conducts a paleomagnetic investigation of postglacial cap carbonate sequences to examine Snowball Earth dynamics.
Thales Pescarini, et al.. Supplemental Material: Paleomagnetic investigation of the basal Maieberg Formation (Namibia) cap carbonate sequence (635 Ma): Implications for Snowball Earth postglacial dynamics. 2024. https://doi.org/10.1130/gsab.s.25571712
Paper [10] provides complementary rock magnetism and paleomagnetic directional statistics relevant to Snowball Earth reconstructions.
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