The Effect of Magnetotactic Bacteria on the Magnetic Properties of Marine Sediments View Full Text


Ontology type: schema:Chapter     


Chapter Info

DATE

1989

AUTHORS

John F. Stolz , Shih-Bin R. Chang , Joseph L. Kirschvink

ABSTRACT

Magnetotactic bacteria have been studied in three distinct sedimentary marine environments: a hypersaline lagoon, an intertidal CO3 marsh, and an open ocean basin. The bacteria and the ultra-fine grained, single domain magnetite (Fe3O4) they produce were extracted from the sediments and studied with transmission electron microscopy. Magnetic properties of the sediments were measured by rock magnetic techniques using a SQUID magnetometer. Our results show that magnetotactic bacteria contribute a significant fraction of the natural remanent magnetization to their sedimentary environment and in some cases may be the sole source of the stable remanence carrying mineral. The occurrence and abundance of these bacteria in a diversity of marine environments implies that they may also play a role in the microbial iron cycle. More... »

PAGES

497-506

References to SciGraph publications

Book

TITLE

Origin, Evolution, and Modern Aspects of Biomineralization in Plants and Animals

ISBN

978-1-4757-6116-0
978-1-4757-6114-6

Identifiers

URI

http://scigraph.springernature.com/pub.10.1007/978-1-4757-6114-6_38

DOI

http://dx.doi.org/10.1007/978-1-4757-6114-6_38

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1008854284


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