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. 2021 Jul 28;11:15340. doi: 10.1038/s41598-021-94695-3

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© The Author(s) 2021

Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/.

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Generalized logs of the stratigraphic sections investigated (youngest at top left, oldest at bottom right, but see description for details) with indication of paleomagnetic samples placed aside initial magnetic susceptibility, maximum angular deviation (MAD) values of the C component directions, virtual geomagnetic pole (VGP) latitudes, and polarity stratigraphy where black bars represent normal polarity and the white bar is reverse polarity. Cobb Mt.? is a possible record of the Cobb Mountain subchron. Red bars indicate archeological units ThI-L1 (bottom) and ThI-L5 (top) within OH1 Bed 2. Drawing G. Muttoni, S. Perini, and S. Sanz-Laliberté. This figure was created with Adobe Illustrator CS6 version (http://www.adobe.com).