Author:
Cockell Charles S.,Schaefer Bettina,Wuchter Cornelia,Coolen Marco J. L.,Grice Kliti,Schnieders Luzie,Morgan Joanna V.,Gulick Sean P. S.,Wittmann Axel,Lofi Johanna,Christeson Gail L.,Kring David A.,Whalen Michael T.,Bralower Timothy J.,Osinski Gordon R.,Claeys Philippe,Kaskes Pim,de Graaff Sietze J.,Déhais Thomas,Goderis Steven,Hernandez Becerra Natali,Nixon Sophie,
Abstract
We report on the effect of the end-Cretaceous impact event on the present-day deep microbial biosphere at the impact site. IODP-ICDP Expedition 364 drilled into the peak ring of the Chicxulub crater, México, allowing us to investigate the microbial communities within this structure. Increased cell biomass was found in the impact suevite, which was deposited within the first few hours of the Cenozoic, demonstrating that the impact produced a new lithological horizon that caused a long-term improvement in deep subsurface colonization potential. In the biologically impoverished granitic rocks, we observed increased cell abundances at impact-induced geological interfaces, that can be attributed to the nutritionally diverse substrates and/or elevated fluid flow. 16S rRNA gene amplicon sequencing revealed taxonomically distinct microbial communities in each crater lithology. These observations show that the impact caused geological deformation that continues to shape the deep subsurface biosphere at Chicxulub in the present day.
Subject
Microbiology (medical),Microbiology
Cited by
8 articles.
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