Magnetic paleointensity stratigraphy and high-resolution Quaternary geochronology: Successes and future challenges
Magnetic paleointensity stratigraphy is used to detect variations in the strength of Earth's ancient magnetic field. Paleointensity studies have demonstrated that a dominantly dipolar geomagnetic signal can be recorded in a globally coherent manner in different types of sediments and in non-sed...
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ftanucanberra:oai:digitalcollections.anu.edu.au:1885/84570 2023-05-15T16:39:11+02:00 Magnetic paleointensity stratigraphy and high-resolution Quaternary geochronology: Successes and future challenges Roberts, Andrew Tauxe, Lisa Heslop, David 2015-12-13T23:01:45Z http://hdl.handle.net/1885/84570 unknown Pergamon-Elsevier Ltd 0277-3791 http://hdl.handle.net/1885/84570 Quaternary Science Reviews Journal article 2015 ftanucanberra 2015-12-28T23:38:37Z Magnetic paleointensity stratigraphy is used to detect variations in the strength of Earth's ancient magnetic field. Paleointensity studies have demonstrated that a dominantly dipolar geomagnetic signal can be recorded in a globally coherent manner in different types of sediments and in non-sedimentary archives, including ice core records and marine magnetic anomaly profiles. The dominantly dipolar nature of geomagnetic paleointensity variations provides a global geophysical signal that has come to be widely used to date Quaternary sediments. Despite the many successful applications of paleointensity-assisted chronology, the mechanisms by which sediments become magnetized remain poorly understood and there is no satisfactory theoretical foundation for paleointensity estimation. In this paper, we outline past successes of sedimentary paleointensity analysis as well as remaining challenges that need to be addressed to place such work on a more secure theoretical and empirical foundation. We illustrate how common concepts for explaining sedimentary remanence acquisition can give rise to centennial to millennial offsets between paleomagnetic and other signals, which is a key limitation for using paleointensity signals for geochronology. Our approach is intended to help non-specialists to better understand the legitimate uses and limitations of paleointensity stratigraphy, while pointing to outstanding problems that require concerted specialist efforts to resolve. Article in Journal/Newspaper ice core Australian National University: ANU Digital Collections |
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Open Polar |
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Australian National University: ANU Digital Collections |
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ftanucanberra |
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description |
Magnetic paleointensity stratigraphy is used to detect variations in the strength of Earth's ancient magnetic field. Paleointensity studies have demonstrated that a dominantly dipolar geomagnetic signal can be recorded in a globally coherent manner in different types of sediments and in non-sedimentary archives, including ice core records and marine magnetic anomaly profiles. The dominantly dipolar nature of geomagnetic paleointensity variations provides a global geophysical signal that has come to be widely used to date Quaternary sediments. Despite the many successful applications of paleointensity-assisted chronology, the mechanisms by which sediments become magnetized remain poorly understood and there is no satisfactory theoretical foundation for paleointensity estimation. In this paper, we outline past successes of sedimentary paleointensity analysis as well as remaining challenges that need to be addressed to place such work on a more secure theoretical and empirical foundation. We illustrate how common concepts for explaining sedimentary remanence acquisition can give rise to centennial to millennial offsets between paleomagnetic and other signals, which is a key limitation for using paleointensity signals for geochronology. Our approach is intended to help non-specialists to better understand the legitimate uses and limitations of paleointensity stratigraphy, while pointing to outstanding problems that require concerted specialist efforts to resolve. |
format |
Article in Journal/Newspaper |
author |
Roberts, Andrew Tauxe, Lisa Heslop, David |
spellingShingle |
Roberts, Andrew Tauxe, Lisa Heslop, David Magnetic paleointensity stratigraphy and high-resolution Quaternary geochronology: Successes and future challenges |
author_facet |
Roberts, Andrew Tauxe, Lisa Heslop, David |
author_sort |
Roberts, Andrew |
title |
Magnetic paleointensity stratigraphy and high-resolution Quaternary geochronology: Successes and future challenges |
title_short |
Magnetic paleointensity stratigraphy and high-resolution Quaternary geochronology: Successes and future challenges |
title_full |
Magnetic paleointensity stratigraphy and high-resolution Quaternary geochronology: Successes and future challenges |
title_fullStr |
Magnetic paleointensity stratigraphy and high-resolution Quaternary geochronology: Successes and future challenges |
title_full_unstemmed |
Magnetic paleointensity stratigraphy and high-resolution Quaternary geochronology: Successes and future challenges |
title_sort |
magnetic paleointensity stratigraphy and high-resolution quaternary geochronology: successes and future challenges |
publisher |
Pergamon-Elsevier Ltd |
publishDate |
2015 |
url |
http://hdl.handle.net/1885/84570 |
genre |
ice core |
genre_facet |
ice core |
op_source |
Quaternary Science Reviews |
op_relation |
0277-3791 http://hdl.handle.net/1885/84570 |
_version_ |
1766029521782308864 |