Magnetostratigraphic constraints on the late Ediacaran paleomagnetic enigma

Paleogeography of the Ediacaran Period has remained poorly understood because of paleomagnetic studies commonly yielding perplexing or conflicting data. Here, we report new magnetostratigraphic data from the Ediacaran Ouarzazate Group in the Anti-Atlas Mountains of Morocco, which have primary magnetizations supported by a positive conglomerate test and stratigraphically consistent directions within volcanic units across multiple localities. Comprehensive magnetostratigraphic sampling shows highly variable directions, consistent with a rapidly changing geomagnetic field along a longitudinally preferred band. High-precision geochronology constrains the geomagnetic variability to ~568 to 562 million years and suggests rates that are likely too rapid for true polar wander or plate tectonic interpretations. Comparison of igneous- and sedimentary-derived data, using a new statistical approach combining Bingham and Fisher distributions, indicates a high-inclination paleomagnetic direction that is compatible with independent evidence for regional glaciation. Our analysis produces a late Ediacaran paleogeographic reconstruction that is consistent with paleomagnetic and geologic constraints.

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Publication Details

Journal
Science Advances
Published
2025-10-03
DOI
https://doi.org/10.1126/sciadv.ady3258
Citations
3
Primary Topic
Geological and Geophysical Studies Worldwide
Type
article
Field-Weighted Citation Impact
5.60

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article

Magnetostratigraphic constraints on the late Ediacaran paleomagnetic enigma

Moulay Ahmed Boumehdi, Jörn‐Frederik Wotzlaw, James L. Pierce, David A.D. Evans et al.
3 citations
Science Advances
Geological and Geophysical Studies Worldwide
5.60
article

Magnetostratigraphic constraints on the late Ediacaran paleomagnetic enigma

Moulay Ahmed Boumehdi, Jörn‐Frederik Wotzlaw, James L. Pierce, David A.D. Evans, Nasrrddine Youbi, Ulf Linnemann, Justin V. Strauss, Andreas Gärtner, Rachid Oukhro, mohamed Achraf Mediany, C. Brenhin Keller, Dana Polomski, Jihane Ounar, Maria Ovtcharova
article en
3 citations

Abstract

Paleogeography of the Ediacaran Period has remained poorly understood because of paleomagnetic studies commonly yielding perplexing or conflicting data. Here, we report new magnetostratigraphic data from the Ediacaran Ouarzazate Group in the Anti-Atlas Mountains of Morocco, which have primary magnetizations supported by a positive conglomerate test and stratigraphically consistent directions within volcanic units across multiple localities. Comprehensive magnetostratigraphic sampling shows highly variable directions, consistent with a rapidly changing geomagnetic field along a longitudinally preferred band. High-precision geochronology constrains the geomagnetic variability to ~568 to 562 million years and suggests rates that are likely too rapid for true polar wander or plate tectonic interpretations. Comparison of igneous- and sedimentary-derived data, using a new statistical approach combining Bingham and Fisher distributions, indicates a high-inclination paleomagnetic direction that is compatible with independent evidence for regional glaciation. Our analysis produces a late Ediacaran paleogeographic reconstruction that is consistent with paleomagnetic and geologic constraints.

Science AdvancesVol. 11(40)
Dartmouth College (US), University of Geneva (CH), Cadi Ayyad University (MA), University of Lisbon (PT), National Research Tomsk State University (RU), Whitney Museum of American Art (US), Yale University (US), ETH Zurich (CH), Senckenberg Natural History Collections Dresden (DE)
National Science Foundation, Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung, Université Cadi Ayyad
Openalex Percentile: Top 4%
Geological and Geophysical Studies Worldwide
5.60
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