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本文引用的文献

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Microbial Mat Communities along an Oxygen Gradient in a Perennially Ice-Covered Antarctic Lake.常年冰封的南极湖泊中沿氧梯度分布的微生物席群落
Appl Environ Microbiol. 2015 Nov 13;82(2):620-30. doi: 10.1128/AEM.02699-15. Print 2016 Jan 15.
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The changing form of Antarctic biodiversity.南极生物多样性的变化形式。
Nature. 2015 Jun 25;522(7557):431-8. doi: 10.1038/nature14505.
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Quantifying community assembly processes and identifying features that impose them.量化群落组装过程并确定施加这些过程的特征。
ISME J. 2013 Nov;7(11):2069-79. doi: 10.1038/ismej.2013.93. Epub 2013 Jun 6.
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Fundamentals of microbial community resistance and resilience.微生物群落抗逆性和恢复力基础。
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The Pyramid Trough Wetland: environmental and biological diversity in a newly created Antarctic protected area.金字塔潟湖湿地:新创建的南极保护区中的环境和生物多样性。
FEMS Microbiol Ecol. 2012 Nov;82(2):356-66. doi: 10.1111/j.1574-6941.2012.01380.x. Epub 2012 Apr 30.
6
Continent-wide risk assessment for the establishment of nonindigenous species in Antarctica.南极洲非本地物种建立的全大陆风险评估。
Proc Natl Acad Sci U S A. 2012 Mar 27;109(13):4938-43. doi: 10.1073/pnas.1119787109. Epub 2012 Mar 5.
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Ancient origins determine global biogeography of hot and cold desert cyanobacteria.古老起源决定了炎热和寒冷沙漠蓝细菌的全球生物地理学。
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Ozone depletion and climate change: impacts on UV radiation.臭氧消耗和气候变化:对紫外线辐射的影响。
Photochem Photobiol Sci. 2011 Feb;10(2):182-98. doi: 10.1039/c0pp90034f. Epub 2011 Jan 20.
9
QIIME allows analysis of high-throughput community sequencing data.QIIME可用于分析高通量群落测序数据。
Nat Methods. 2010 May;7(5):335-6. doi: 10.1038/nmeth.f.303. Epub 2010 Apr 11.
10
Global distribution of cyanobacterial ecotypes in the cold biosphere.全球冷生环境中蓝藻的生态型分布。
ISME J. 2010 Feb;4(2):191-202. doi: 10.1038/ismej.2009.113. Epub 2009 Nov 5.

利用斯科特船长“发现号”采集的标本探寻过往:南极蓝藻细菌的多样性在过去100年里发生变化了吗?

Using Captain Scott's Discovery specimens to unlock the past: has Antarctic cyanobacterial diversity changed over the last 100 years?

作者信息

Jungblut Anne D, Hawes Ian

机构信息

Life Sciences Department, Natural History Museum, Cromwell Road, London SW7 5BD, UK

University of Waikato, 58 Cross Road, Tauranga 3110, New Zealand.

出版信息

Proc Biol Sci. 2017 Jun 28;284(1857). doi: 10.1098/rspb.2017.0833.

DOI:10.1098/rspb.2017.0833
PMID:28637848
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC5489731/
Abstract

Evidence of climate-driven environmental change is increasing in Antarctica, and with it comes concern that this will propagate to impacts on biological communities. Recognition and prediction of change needs to incorporate the extent and timescales over which communities vary under extant conditions. However, few observations of Antarctic microbial communities, which dominate inland habitats, allow this. We therefore carried out the first molecular comparison of Cyanobacteria in historic herbarium microbial mats from freshwater ecosystems on Ross Island and the McMurdo Ice Shelf, collected by Captain R.F. Scott's 'Discovery' Expedition (1902-1903), with modern samples from those areas. Using 16S rRNA gene surveys, we found that modern and historic cyanobacteria assemblages showed some variation in community structure but were dominated by the same genotypes. Modern communities had a higher richness, including genotypes not found in historic samples, but they had the highest similarity to other cyanobacteria sequences from Antarctica. The results imply slow cyanobacterial 16S rRNA gene genotype turnover and considerable community stability within Antarctic microbial mats. We suggest that this relates to Antarctic freshwater 'organisms requiring a capacity to withstand diverse stresses, and that this could also provide a degree of resistance and resilience to future climatic-driven environmental change in Antarctica.

摘要

南极地区受气候驱动的环境变化证据日益增多,随之而来的是人们担心这将蔓延至对生物群落的影响。对变化的认识和预测需要考虑到在现有条件下群落变化的程度和时间尺度。然而,对于在内陆栖息地占主导地位的南极微生物群落,几乎没有观测数据能做到这一点。因此,我们首次对罗斯岛和麦克默多冰架淡水生态系统中具有历史意义的植物标本微生物垫中的蓝细菌进行了分子比较,这些标本是由R.F. 斯科特船长的“发现”号探险队(1902 - 1903年)采集的,并与来自这些地区的现代样本进行了对比。通过16S rRNA基因调查,我们发现现代和历史蓝细菌组合在群落结构上存在一些差异,但都由相同的基因型主导。现代群落的丰富度更高,包括一些在历史样本中未发现的基因型,但它们与来自南极的其他蓝细菌序列相似度最高。结果表明南极微生物垫中蓝细菌16S rRNA基因基因型更替缓慢,群落具有相当的稳定性。我们认为这与南极淡水“生物需要具备承受多种压力的能力有关,并且这也可能为南极未来受气候驱动的环境变化提供一定程度的抵抗力和恢复力。