The evolution of the Levantine Iron Age geomagnetic anomaly captured in Mediterranean sediments
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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 [37]
The Introduction describes the LIAA as having non-GAD directions, field strengths above 140 ZAm², and two short-lived spikes above 160 ZAm². Section 6.5 reports a large directional deviation in the Taranto Gulf core, but says the Levant core’s directions were within normal paleosecular variation. The paper does not establish a general averaged range of 130–160 ZAm² or quantify fast secular-variation rates for the LIAA. (LLM, conf=0.84)
Experimental — accuracy not yet measured586 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 [37]
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 [37]
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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
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- Authors
- Béguin, A., Filippidi, A., de Lange, G. J., & de Groot, L. V.
- Affiliations
- Utrecht University (NL)
- Corresponding author
- Béguin, Annemarieke
- Venue
- Earth and Planetary Science Letters
- Publisher
- Elsevier BV
- Published
- 2019-04
- Volume
- 511
- Pages
- 55-66
- ISSN
- 0012-821X (ISSN-L)
- OpenAlex
- W2912611800
- Cited by
- 21
- References
- 37
- Citations by year
- 2024: 2 · 2023: 4 · 2022: 4 · 2021: 4 · 2020: 5 · 2019: 2
- FWCI
- 1.24
- Type
- journal article
- Language
- en
- Open access
- bronze
- doi.org
- Licence
- Locations
- Earth and Planetary Science Letters (publishedVersion)
- Utrecht University Repository (Utrecht University) (submittedVersion, other-oa)
- Utrecht University Repository (Utrecht University) (submittedVersion)
- Funders
- Nederlandse Organisatie voor Wetenschappelijk Onderzoek (863.15.003)
- Topics
- Life Sciences › Biochemistry, Genetics and Molecular Biology › Molecular Biology › Geomagnetism and Paleomagnetism Studies
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Geology and Paleoclimatology Research
- Physical Sciences › Earth and Planetary Sciences › Geology › Geological and Geophysical Studies
- Keywords
- geomagnetic field variations, paleointensity, marine sediment core, Alboran Sea, Levant, rock magnetic properties, geomagnetic field evolution
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