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南极海冰区是气溶胶中生物成因有机氮的来源。

Antarctic sea ice region as a source of biogenic organic nitrogen in aerosols.

机构信息

Institut de Ciències del Mar, CSIC, Pg. Marítim de la Barceloneta 37-49, 08003, Barcelona, Catalonia, Spain.

School of Physics and Centre for Climate and Air Pollution Studies, Ryan Institute, National University of Ireland Galway, University Road, Galway, Ireland.

出版信息

Sci Rep. 2017 Jul 20;7(1):6047. doi: 10.1038/s41598-017-06188-x.

Abstract

Climate warming affects the development and distribution of sea ice, but at present the evidence of polar ecosystem feedbacks on climate through changes in the atmosphere is sparse. By means of synergistic atmospheric and oceanic measurements in the Southern Ocean near Antarctica, we present evidence that the microbiota of sea ice and sea ice-influenced ocean are a previously unknown significant source of atmospheric organic nitrogen, including low molecular weight alkyl-amines. Given the keystone role of nitrogen compounds in aerosol formation, growth and neutralization, our findings call for greater chemical and source diversity in the modelling efforts linking the marine ecosystem to aerosol-mediated climate effects in the Southern Ocean.

摘要

气候变暖影响海冰的形成和分布,但目前有关极地生态系统通过大气变化对气候产生反馈的证据还很稀少。通过在南极洲附近的南大洋进行协同的大气和海洋测量,我们提供的证据表明,海冰和受海冰影响的海洋中的微生物群落是以前未知的大气有机氮的一个重要来源,包括低分子量的烷基胺。鉴于氮化合物在气溶胶形成、生长和中和过程中的关键作用,我们的发现呼吁在将海洋生态系统与南大洋气溶胶介导的气候影响联系起来的建模工作中,增加化学物质和源的多样性。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b0f9/5519629/0c983aa39829/41598_2017_6188_Fig1_HTML.jpg

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