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Published on: August 2, 2021
U-Th dated speleothem recorded geomagnetic excursions in the Lower Brunhes
Jean-Pierre Pozzi1,2, Louis Rousseau2, Christophe Falguères2
1Ecole Normale Supérieure, Laboratoire de Géologie UMR CNRS 8538 PSL, Paris, 75005, France.
This study reveals four geomagnetic excursions, Basura 1-4, recorded in an Italian flowstone. Basura 4, dated to 417 ka, is a distinct event potentially representing a geomagnetic excursion.
Area of Science:
- Paleomagnetism
- Geophysics
- Quaternary Geology
Background:
- Understanding Earth's magnetic field behavior is crucial.
- Geomagnetic excursions provide insights into past magnetic field instabilities.
- Flowstone records offer continuous archives of geomagnetic variations.
Purpose of the Study:
- To present the geomagnetic record from a flowstone core in Liguria, Italy.
- To analyze geomagnetic excursions during the Lower Brunhes chron.
- To investigate the relationship between flowstone growth rate and climate stages.
Main Methods:
- A 2.29-m-long continuous flowstone core was sampled and dated using U-series.
- Magnetic remanence was measured using u-channel and deconvolved.
- High-resolution dating established the age of the flowstone from Marine Isotopic Stage (MIS) 13 to MIS 7.
Main Results:
- Four geomagnetic excursions (Basura 1, 2, 3, and 4) were identified within the flowstone.
- Basura 1, 2, and 3 exhibit overlapping ages due to U-Th dating uncertainties.
- Basura 4 is well-dated to 417 ± 7/8 ka and is distinguishable from the other events.
Conclusions:
- The flowstone provides a detailed record of geomagnetic behavior during the Lower Brunhes.
- Basura 4 represents a significant geomagnetic event, potentially a new excursion.
- The study highlights the importance of flowstones in paleomagnetic research.
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