Fast geomagnetic field intensity variations between 1400 and 400 BCE: New archaeointensity data from Germany
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586 BCE was believed to follow a period of an intense high-field anomaly identified in the Near East and Western Europe.
“From a geomagnetic perspective, 586 BCE was believed to follow a period of an intense high-field anomaly identified in the Near East [32, 35] and in Western Europe [5, 36, 37].”
From The Earth’s magnetic field in Jerusalem during the Babylonian destruction: A unique reference for field behavior and an anchor for archaeomagnetic dating (2020) · cites this paper as [36]
The LIAA is characterized by generally high averaged field values (130-160 ZAm2), with short episodes of higher field values and geomagnetic spikes, fast secular variation rates and large angular deviations from the GAD field.
“This anomaly is characterized by generally high averaged field values (130–160 ZAm2), with short episodes of higher field values and geomagnetic spikes, fast secular variation rates and large angular deviations from the GAD field.”
From The Earth’s magnetic field in Jerusalem during the Babylonian destruction: A unique reference for field behavior and an anchor for archaeomagnetic dating (2020) · cites this paper as [36]
The Levantine Iron Age Anomaly (LIAA) spanned from the 10th century BCE until at least the 5th century BCE in the Near East and Europe.
“a high field anomaly, which spanned from the 10th century BCE until at least the 5th century BCE in the Near East and Europe [5, 21, 35–37].”
From The Earth’s magnetic field in Jerusalem during the Babylonian destruction: A unique reference for field behavior and an anchor for archaeomagnetic dating (2020) · cites this paper as [36]
Cites
A geomagnetic field model for the Holocene based on archaeomagnetic and lava flow data
Pavón-Carrasco, F. J., Osete, M. L., Torta, J. M., & De Santis, A. (2014) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2013.11.046 · Cited by 384 · see citing works
Persistent high paleosecular variation activity in southern hemisphere for at least 10,000 years
Constable, C., Korte, M., & Panovska, S. (2016) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2016.08.015 · Cited by 277 · see citing works
Usoskin, I. G., Gallet, Y., Lopes, F., Kovaltsov, G. A., & Hulot, G. (2016) · Astronomy & Astrophysics · doi:10.1051/0004-6361/201527295 · Cited by 176 · see citing works
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Osete, M. L., Molina-Cardín, A., Campuzano, S. A., Aguilella-Arzo, G., Barrachina-Ibañez, A., Falomir-Granell, F., Oliver Foix, A., Gómez-Paccard, M., Martín-Hernández, F., Palencia-Ortas, A., et al. (2020) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2019.116047 · Cited by 62 · see citing works
Vaknin, Y., Shaar, R., Gadot, Y., Shalev, Y., Lipschits, O., & Ben-Yosef, E. (2020) · PLOS ONE · doi:10.1371/journal.pone.0237029 · Cited by 25 · see citing works
The evolution of the Levantine Iron Age geomagnetic anomaly captured in Mediterranean sediments
Béguin, A., Filippidi, A., de Lange, G. J., & de Groot, L. V. (2019) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2019.01.021 · Cited by 21 · see citing works
- Authors
- Hervé, G., Faβbinder, J., Gilder, S. A., Metzner-Nebelsick, C., Gallet, Y., Genevey, A., Schnepp, E., Geisweid, L., Pütz, A., Reuβ, S., Wittenborn, F., Flontas, A., Linke, R., Riedel, G., Walter, F., & Westhausen, I.
- Affiliations
- Ludwig-Maximilians-Universität München (DE)
- Centre National de la Recherche Scientifique (FR)
- Montanuniversität Leoben (AT)
- Heidelberg University (DE)
- Corresponding author
- Hervé, Gwenaël
- Venue
- Physics of the Earth and Planetary Interiors
- Publisher
- Elsevier BV
- Published
- 2017-09
- Volume
- 270
- Pages
- 143-156
- ISSN
- 0031-9201 (ISSN-L)
- OpenAlex
- W2738017896
- Cited by
- 49
- References
- 3
- Citations by year
- 2026: 2 · 2025: 2 · 2024: 2 · 2023: 3 · 2022: 5 · 2021: 11 · 2020: 9 · 2019: 8 · 2018: 5 · 2017: 2
- FWCI
- 2.68
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Physics of The Earth and Planetary Interiors (publishedVersion)
- HAL (submittedVersion)
- Funders
- AGE-WELL
- Deutsche Forschungsgemeinschaft
- Topics
- Life Sciences › Biochemistry, Genetics and Molecular Biology › Molecular Biology › Geomagnetism and Paleomagnetism Studies
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Archaeology and ancient environmental studies
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Geology and Paleoclimatology Research
- Keywords
- archaeointensity, geomagnetic field intensity, secular variation, Iron Age, virtual axial dipole moment, dipole tilt, pottery sherds, Bayesian inversion, Western Europe, Middle East, Central Asia
About these checks
Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
Statistics and arithmetic are recomputed, not judged.
Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.
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