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大型底栖动物会增强沿海沉积物的甲烷通量。

Methane fluxes from coastal sediments are enhanced by macrofauna.

作者信息

Bonaglia Stefano, Brüchert Volker, Callac Nolwenn, Vicenzi Alessandra, Chi Fru Ernest, Nascimento Francisco J A

机构信息

Department of Ecology, Environment and Plant Sciences, Stockholm University, Stockholm, Sweden.

Bolin Centre for Climate Research, Stockholm University, Stockholm, Sweden.

出版信息

Sci Rep. 2017 Oct 13;7(1):13145. doi: 10.1038/s41598-017-13263-w.

DOI:10.1038/s41598-017-13263-w
PMID:29030563
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC5640653/
Abstract

Methane and nitrous oxide are potent greenhouse gases (GHGs) that contribute to climate change. Coastal sediments are important GHG producers, but the contribution of macrofauna (benthic invertebrates larger than 1 mm) inhabiting them is currently unknown. Through a combination of trace gas, isotope, and molecular analyses, we studied the direct and indirect contribution of two macrofaunal groups, polychaetes and bivalves, to methane and nitrous oxide fluxes from coastal sediments. Our results indicate that macrofauna increases benthic methane efflux by a factor of up to eight, potentially accounting for an estimated 9.5% of total emissions from the Baltic Sea. Polychaetes indirectly enhance methane efflux through bioturbation, while bivalves have a direct effect on methane release. Bivalves host archaeal methanogenic symbionts carrying out preferentially hydrogenotrophic methanogenesis, as suggested by analysis of methane isotopes. Low temperatures (8 °C) also stimulate production of nitrous oxide, which is consumed by benthic denitrifying bacteria before it reaches the water column. We show that macrofauna contributes to GHG production and that the extent is dependent on lineage. Thus, macrofauna may play an important, but overlooked role in regulating GHG production and exchange in coastal sediment ecosystems.

摘要

甲烷和一氧化二氮是导致气候变化的强效温室气体。沿海沉积物是重要的温室气体排放源,但栖息其中的大型动物(大于1毫米的底栖无脊椎动物)的作用目前尚不清楚。通过痕量气体、同位素和分子分析相结合的方法,我们研究了多毛类和双壳类这两类大型动物对沿海沉积物甲烷和一氧化二氮通量的直接和间接贡献。我们的结果表明,大型动物可使底栖甲烷排放通量增加多达8倍,这可能占波罗的海总排放量的9.5%。多毛类通过生物扰动间接增强甲烷排放,而双壳类则对甲烷释放有直接影响。甲烷同位素分析表明,双壳类体内携带进行优先氢营养型甲烷生成的古菌产甲烷共生体。低温(8°C)也会刺激一氧化二氮的产生,在其到达水柱之前会被底栖反硝化细菌消耗。我们表明大型动物对温室气体产生有贡献,且其程度取决于种类。因此,大型动物可能在调节沿海沉积物生态系统中温室气体的产生和交换方面发挥重要但被忽视的作用。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ab62/5640653/8174dd4a4590/41598_2017_13263_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ab62/5640653/0e6de8cd05a0/41598_2017_13263_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ab62/5640653/710a03b9e085/41598_2017_13263_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ab62/5640653/8174dd4a4590/41598_2017_13263_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ab62/5640653/0e6de8cd05a0/41598_2017_13263_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ab62/5640653/710a03b9e085/41598_2017_13263_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ab62/5640653/8174dd4a4590/41598_2017_13263_Fig3_HTML.jpg

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