Please use this identifier to cite or link to this item: http://hdl.handle.net/2445/98241
Title: Paleomagnetic and paleoenvironmental implications of magnetofossil occurrences in late Miocene marine sediments from the Guadalquivir Basin, SW Spain.
Author: Larrasoaña, J.C.
Liu, Q.
Hu, P.
Roberts, A.P.
Mata, M. Pilar
Civis Llovera, J.
Sierro Sánchez, Francisco Javier
Pérez-Asensio, José N. (José Noel)
Keywords: Paleomagnetisme
Paleoclimatologia
Sediments marins
Bajo Guadalquivir (Andalusia)
Miocè
Paleomagnetism
Paleoclimatology
Marine sediments
Bajo Guadalquivir Region (Andalusia)
Miocene
Issue Date: 4-Mar-2014
Publisher: Frontiers Media
Abstract: Although recent studies have revealed more widespread occurrences of magnetofossils in pre-Quaternary sediments than have been previously reported, their significance for paleomagnetic and paleoenvironmental studies is not fully understood. We present a paleo- and rock-magnetic study of late Miocene marine sediments recovered from the Guadalquivir Basin (SW Spain). Well-defined paleomagnetic directions provide a robust magnetostratigraphic chronology for the two studied sediment cores. Rock magnetic results indicate the dominance of intact magnetosome chains throughout the studied sediments. These results provide a link between the highest-quality paleomagnetic directions and higher magnetofossil abundances. We interpret that bacterial magnetite formed in the surface sediment mixed layer and that these magnetic particles gave rise to a paleomagnetic signal in the same way as detrital grains. They, therefore, carry a magnetization that is essentially identical to a post-depositional remanent magnetization, which we term a bio-depositional remanent magnetization. Some studied polarity reversals record paleomagnetic directions with an apparent 60-70 kyr recording delay. Magnetofossils in these cases are interpreted to carry a biogeochemical remanent magnetization that is locked in at greater depth in the sediment column. A sharp decrease in magnetofossil abundance toward the middle of the studied boreholes coincides broadly with a major rise in sediment accumulation rates near the onset of the Messinian salinity crisis (MSC), an event caused by interruption of the connection between the Mediterranean Sea and the Atlantic Ocean. This correlation appears to have resulted from dilution of magnetofossils by enhanced terrigenous inputs that were driven, in turn, by sedimentary changes triggered in the basin at the onset of the MSC. Our results highlight the importance of magnetofossils as carriers of high-quality paleomagnetic and paleoenvironmental signals even in dominantly terrigenous sediments.
Note: Reproducció del document publicat a: http://dx.doi.org/10.3389/fmicb.2014.00071
It is part of: Frontiers in Microbiology, 2014, vol. 5, num. 71, p. 1-15
Related resource: http://dx.doi.org/10.3389/fmicb.2014.00071
URI: http://hdl.handle.net/2445/98241
ISSN: 1664-302X
Appears in Collections:Articles publicats en revistes (Dinàmica de la Terra i l'Oceà)

Files in This Item:
File Description SizeFormat 
660999.pdf3.02 MBAdobe PDFView/Open


This item is licensed under a Creative Commons License Creative Commons