期刊
FRONTIERS IN MARINE SCIENCE
卷 8, 期 -, 页码 -出版社
FRONTIERS MEDIA SA
DOI: 10.3389/fmars.2021.587748
关键词
CellTracker(TM) Green CMFDA; Rose Bengal; gas hydrate; Vestnesa Ridge; Storfjordrenna; cold seep; Arctic
资金
- Research Council of Norway through its Centers of Excellence funding scheme [2232]
This study examined modern foraminiferal assemblages from a gas hydrate province and another marine area, finding that metabolically active foraminifera can inhabit methane-enriched sediments, but there was no clear evidence that methane significantly affected the carbon isotopic signature of living specimens.
Highly negative delta C-13 values in fossil foraminifera from methane cold seeps have been proposed to reflect episodes of methane release from gas hydrate dissociation or free gas reservoirs triggered by climatic changes in the past. Because most studies on live foraminifera are based on the presence of Rose Bengal staining, that colors the cytoplasm of both live and recently dead individuals it remains unclear if, and to what extent live foraminifera incorporate methane-derived carbon during biomineralization, or whether the isotopic signature is mostly affected by authigenic overgrowth. In this paper, modern foraminiferal assemblages from a gas hydrate province Vestnesa Ridge (similar to 1,200 m water depth, northeastern Fram Strait) and from Storfjordrenna (similar to 400 m water depth in the western Barents Sea) is presented. By using the fluorescent viability assays CellTracker(TM) Green (CTG) CMFDA and CellHunt Green (CHG) together with conventional Rose Bengal, it was possible to examine live and recently dead foraminifera separately. Metabolically active foraminifera were shown to inhabit methane-enriched sediments at both investigated locations. The benthic foraminiferal faunas were dominated by common Arctic species such as Melonis barleeanus, Cassidulina neoteretis, and Nonionellina labradorica. The combined usage of the fluorescence probe and Rose Bengal revealed only minor shifts in species compositions and differences in ratios between live and recently dead foraminifera from Storfjordrenna. There was no clear evidence that methane significantly affected the delta C-13 signature of the calcite of living specimens.
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