Consistent and Contrasting Aspects of the Geomagnetic Field Across Epochs With Distinct Reversal Frequencies Revealed by Modeling the Kiaman Superchron

Abstract This work presents an extensive directional paleomagnetic database of the Kiaman reversed superchron. It is composed of 1,459 paleomagnetic directions from igneous rocks corresponding to 91 data sets (or paleomagnetic poles). An almost constant behavior of more concentrated and circular dis...

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Main Authors: Daniele Brandt, Marcia Ernesto, Catherine Constable
Format: Article
Language:English
Published: Wiley 2021-07-01
Series:Geochemistry, Geophysics, Geosystems
Subjects:
Online Access:https://doi.org/10.1029/2021GC009866
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author Daniele Brandt
Marcia Ernesto
Catherine Constable
author_facet Daniele Brandt
Marcia Ernesto
Catherine Constable
author_sort Daniele Brandt
collection DOAJ
description Abstract This work presents an extensive directional paleomagnetic database of the Kiaman reversed superchron. It is composed of 1,459 paleomagnetic directions from igneous rocks corresponding to 91 data sets (or paleomagnetic poles). An almost constant behavior of more concentrated and circular distributions for latitudes higher than 10° was found, which contrasts strongly with predictions of the representative models for the past few million years. We searched for simplified and spatially covariant Giant Gaussian Process (GGP) models that best explain the directional distribution of the Kiaman database. We used the mean strength based on the mean of virtual dipole moment (VDM) results for the period drawn from the available databases. Among the tested models, the one that best explains the directional paleosecular variation of the Kiaman database is the covariant type. According to this model, the correlations between the Gaussian coefficients are valid for the last 10 Myr and the Kiaman superchron. The resulting GGP models have β parameters similar to the 0–10 Ma models, which indicates that the relation between symmetric and antisymmetric families appears unchanged in the geological past. The relative variability of the Kiaman field, as inferred from the ratio αg10¯ from GGP models, is lower than for the past 10 Myr. Thus, as well as the paleointensity, αg10¯ seems to be a proxy that can be used for evaluating the geomagnetic development along the geological time.
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spelling doaj.art-1e5fe420aca0445e8857b066f826bc812023-11-03T17:01:09ZengWileyGeochemistry, Geophysics, Geosystems1525-20272021-07-01227n/an/a10.1029/2021GC009866Consistent and Contrasting Aspects of the Geomagnetic Field Across Epochs With Distinct Reversal Frequencies Revealed by Modeling the Kiaman SuperchronDaniele Brandt0Marcia Ernesto1Catherine Constable2Departamento de Geofísica Instituto de Astronomia Geofísica e Ciências Atmosféricas Universidade de São Paulo São Paulo BrazilDepartamento de Geofísica Instituto de Astronomia Geofísica e Ciências Atmosféricas Universidade de São Paulo São Paulo BrazilInstitute of Geophysics and Planetary Physics Scripps Institution of Oceanography University of California at San Diego La Jolla CA USAAbstract This work presents an extensive directional paleomagnetic database of the Kiaman reversed superchron. It is composed of 1,459 paleomagnetic directions from igneous rocks corresponding to 91 data sets (or paleomagnetic poles). An almost constant behavior of more concentrated and circular distributions for latitudes higher than 10° was found, which contrasts strongly with predictions of the representative models for the past few million years. We searched for simplified and spatially covariant Giant Gaussian Process (GGP) models that best explain the directional distribution of the Kiaman database. We used the mean strength based on the mean of virtual dipole moment (VDM) results for the period drawn from the available databases. Among the tested models, the one that best explains the directional paleosecular variation of the Kiaman database is the covariant type. According to this model, the correlations between the Gaussian coefficients are valid for the last 10 Myr and the Kiaman superchron. The resulting GGP models have β parameters similar to the 0–10 Ma models, which indicates that the relation between symmetric and antisymmetric families appears unchanged in the geological past. The relative variability of the Kiaman field, as inferred from the ratio αg10¯ from GGP models, is lower than for the past 10 Myr. Thus, as well as the paleointensity, αg10¯ seems to be a proxy that can be used for evaluating the geomagnetic development along the geological time.https://doi.org/10.1029/2021GC009866Giant Gaussian processKiaman Superchronpaleomagnetic databasepaleosecular variation
spellingShingle Daniele Brandt
Marcia Ernesto
Catherine Constable
Consistent and Contrasting Aspects of the Geomagnetic Field Across Epochs With Distinct Reversal Frequencies Revealed by Modeling the Kiaman Superchron
Geochemistry, Geophysics, Geosystems
Giant Gaussian process
Kiaman Superchron
paleomagnetic database
paleosecular variation
title Consistent and Contrasting Aspects of the Geomagnetic Field Across Epochs With Distinct Reversal Frequencies Revealed by Modeling the Kiaman Superchron
title_full Consistent and Contrasting Aspects of the Geomagnetic Field Across Epochs With Distinct Reversal Frequencies Revealed by Modeling the Kiaman Superchron
title_fullStr Consistent and Contrasting Aspects of the Geomagnetic Field Across Epochs With Distinct Reversal Frequencies Revealed by Modeling the Kiaman Superchron
title_full_unstemmed Consistent and Contrasting Aspects of the Geomagnetic Field Across Epochs With Distinct Reversal Frequencies Revealed by Modeling the Kiaman Superchron
title_short Consistent and Contrasting Aspects of the Geomagnetic Field Across Epochs With Distinct Reversal Frequencies Revealed by Modeling the Kiaman Superchron
title_sort consistent and contrasting aspects of the geomagnetic field across epochs with distinct reversal frequencies revealed by modeling the kiaman superchron
topic Giant Gaussian process
Kiaman Superchron
paleomagnetic database
paleosecular variation
url https://doi.org/10.1029/2021GC009866
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AT marciaernesto consistentandcontrastingaspectsofthegeomagneticfieldacrossepochswithdistinctreversalfrequenciesrevealedbymodelingthekiamansuperchron
AT catherineconstable consistentandcontrastingaspectsofthegeomagneticfieldacrossepochswithdistinctreversalfrequenciesrevealedbymodelingthekiamansuperchron