Institut des Sciences de la Terre d'Orléans, UMR CNRS 6113,
Université d'Orléans, Campus Géosciences, 1A, rue de la
Férollerie, 45071 Orléans cedex 2, France
Muriel Andreani
Laboratoire de Géologie de Lyon, École Normale Supérieure
de Lyon et Université Claude Bernard Lyon 1, UMR 5276 CNRS, 2 rue
Raphaël Dubois, 69622 Villeurbanne cedex, France
Anne-Marie Boullier
CNRS, ISTerre, Université Grenoble Alpes, 38041 Grenoble,
France
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2,286
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Total: 2,286
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Views and downloads (calculated since 12 May 2021)
Cumulative views and downloads
(calculated since 12 May 2021)
Total article views: 1,671 (including HTML, PDF, and XML)
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1,417
230
24
1,671
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18
HTML: 1,417
PDF: 230
XML: 24
Total: 1,671
BibTeX: 13
EndNote: 18
Views and downloads (calculated since 13 Sep 2021)
Cumulative views and downloads
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Total article views: 615 (including HTML, PDF, and XML)
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394
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615
5
4
HTML: 394
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Total: 615
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Cumulative views and downloads
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Viewed (geographical distribution)
Total article views: 2,286 (including HTML, PDF, and XML)
Thereof 2,186 with geography defined
and 100 with unknown origin.
Total article views: 1,671 (including HTML, PDF, and XML)
Thereof 1,619 with geography defined
and 52 with unknown origin.
Total article views: 615 (including HTML, PDF, and XML)
Thereof 567 with geography defined
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Sediments accumulated in accretionary prisms are deformed by the compression imposed by plate subduction. Here we show that deformation of the sediments transforms some minerals in them. We suggest that these mineral transformations are due to the proliferation of microorganisms boosted by deformation. Deformation-enhanced microbial proliferation may change our view of sedimentary and tectonic processes in subduction zones.
Sediments accumulated in accretionary prisms are deformed by the compression imposed by plate...