Use of Stress Signals of Their Attached Bacteria to Monitor Sympagic Algae Preservation in Canadian Arctic Sediments

Type Article
Date 2021-12
Language English
Author(s) Amiraux RémiORCID1, 2, 3, Bonin PatriciaORCID1, Burot Christopher1, Rontani Jean-François1
Affiliation(s) 1 : CNRS/INSU/IRD, Mediterranean Institute of Oceanography (MIO), UM 110, Aix-Marseille University, Université de Toulon, 13288 Marseille, France
2 : UMR 6539 Laboratoire des Sciences de l’Environnement Marin, (CNRS, UBO, IRD, Ifremer) Institut, Universitaire Européen de la Mer (IUEM), 29280 Plouzané, France
3 : Takuvik Joint International Laboratory, Département de Biologie, Laval University (Canada)—CNRS, Université Laval, Québec, QC G1V 0A6, Canada
Source Microorganisms (2076-2607) (MDPI AG), 2021-12 , Vol. 9 , N. 12 , P. 2626 (15p.)
DOI 10.3390/microorganisms9122626
WOS© Times Cited 3
Note This article belongs to the Special Issue Polar Microbes
Keyword(s) sympagic algae, Arctic, bacterial stress, lipid tracers, sediments, preservation
Abstract

Based on the strong aggregation of sympagic (ice-associated) algae and the high mortality or inactivity of bacteria attached to them, it was previously hypothesized that sympagic algae should be significant contributors to the export of carbon to Arctic sediments. In the present work, the lipid content of 30 sediment samples collected in the Canadian Arctic was investigated to test this hypothesis. The detection of high proportions of trans vaccenic fatty acid (resulting from cis-trans isomerase (CTI) activity of bacteria under hypersaline conditions) and 10S-hydroxyhexadec-8(trans)-enoic acid (resulting from 10S-DOX bacterial detoxification activity in the presence of deleterious free palmitoleic acid) confirmed: (i) the strong contribution of sympagic material to some Arctic sediments, and (ii) the impaired physiological status of its associated bacterial communities. Unlike terrestrial material, sympagic algae that had escaped zooplanktonic grazing appeared relatively preserved from biotic degradation in Arctic sediments. The expected reduction in sea ice cover resulting from global warming should cause a shift in the relative contributions of ice-associated vs. pelagic algae to the seafloor, and thus to a strong modification of the carbon cycle

Full Text
File Pages Size Access
Publisher's official version 15 1 MB Open access
Supplementary File 1 49 KB Open access
Top of the page