Rock-magnetic and paleomagnetic study on a 27-m-long core from Lake Chapala, western Mexico: Paleoenvironmental implications for the last 10 ka
Autor: | Eva Pérez Izazaga, Ma. Magdalena Velázquez Bucio, Avto Goguitchaichvili, Pedro F. Zárate del Valle, Juan Morales, Isabel Israde Alcántara, Iván Rosario Espinoza Encinas |
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Rok vydání: | 2019 |
Předmět: |
Paleomagnetism
010504 meteorology & atmospheric sciences Physics and Astronomy (miscellaneous) Natural remanent magnetization Diatoms Geomagnetic global models Holocene Paleoclimate modeling Secular variation Magnetic dip 010502 geochemistry & geophysics 01 natural sciences law.invention Paleontology law Radiocarbon dating 0105 earth and related environmental sciences Volcanic belt Astronomy and Astrophysics Geophysics Earth's magnetic field Space and Planetary Science Magnetic mineralogy Geology |
Zdroj: | Physics of the Earth and Planetary Interiors. 289:90-105 |
ISSN: | 0031-9201 |
DOI: | 10.1016/j.pepi.2019.02.001 |
Popis: | We report detailed rock-magnetic and paleomagnetic results from a 27-m-long sedimentary core collected at depocenter of Lake Chapala, western Trans-Mexican Volcanic Belt. Rock-magnetic parameters point to PSD grain-size titanomagnetites as the dominant magnetic mineralogy. Observed variations, in both concentration and grain-size dependent magnetic parameters, reflect changes in the sediment supply through the studied depth, but mainly during the last half century. Stable characteristic remanent magnetization, representative of secular variation of the geomagnetic field, was retrieved after alternating field demagnetization of the natural remanent magnetization (NRM). The comparison of the obtained magnetic inclination and declination logs against the corresponding curves predicted by the Global Geomagnetic Field Model SHA.DIF.14k enables to establish an alternative sedimentation-rate independent age-depth model for the whole core, in reasonably good agreement with the one calculated using conventional radiocarbon dating. This approach works not only for Lake Chapala, but also for Lake Chalco. The correlation established between rock-magnetic parameters and paleoenvironments, based on diatom identification of representative samples within specific zones, can be considered as a novel proxy methodology. This approach opens a new perspective for new, more detailed rock-magnetic, paleomagnetic and paleoenvironmental investigations for better paleoclimatic reconstructions. |
Databáze: | OpenAIRE |
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