about
Clay mineralogy indicates a mildly warm and humid living environment for the Miocene hominoid from the Zhaotong Basin, Yunnan, ChinaInsolation driven biomagnetic response to the Holocene Warm Period in semi-arid East AsiaOrigin of microbial biomineralization and magnetotaxis during the ArcheanPalaeomagnetic field intensity variations suggest Mesoproterozoic inner-core nucleation.Bulk magnetic domain stability controls paleointensity fidelity.Reply to Wang and Chen: An ancient origin of magnetotactic bacteria.Genomic expansion of magnetotactic bacteria reveals an early common origin of magnetotaxis with lineage-specific evolution.
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description
researcher ORCID ID = 0000-0002-6864-7420
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wetenschapper
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name
Greig A Paterson
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Greig A Paterson
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Greig A Paterson
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type
label
Greig A Paterson
@ast
Greig A Paterson
@en
Greig A Paterson
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prefLabel
Greig A Paterson
@ast
Greig A Paterson
@en
Greig A Paterson
@nl
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0000-0002-6864-7420