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从温带盐沼到干燥和再湿润,底栖生物膜群落的抗逆性和恢复力。

Resistance and resilience of benthic biofilm communities from a temperate saltmarsh to desiccation and rewetting.

机构信息

Department of Biological Sciences, University of Essex, Wivenhoe Park, Colchester, UK.

出版信息

ISME J. 2011 Jan;5(1):30-41. doi: 10.1038/ismej.2010.91. Epub 2010 Jul 1.

Abstract

Periods of desiccation and rewetting are regular, yet stressful events encountered by saltmarsh microbial communities. To examine the resistance and resilience of microbial biofilms to such stresses, sediments from saltmarsh creeks were allowed to desiccate for 23 days, followed by rewetting for 4 days, whereas control sediments were maintained under a natural tidal cycle. In the top 2 mm of the dry sediments, salinity increased steadily from 36 to 231 over 23 days, and returned to seawater salinity on rewetting. After 3 days, desiccated sediments had a lower chlorophyll a (Chl a) fluorescence signal as benthic diatoms ceased to migrate to the surface, with a recovery in cell migration and Chl a fluorescence on rewetting. Extracellular β-glucosidase and aminopeptidase activities decreased within the first week of drying, but increased sharply on rewetting. The bacterial community in the desiccating sediment changed significantly from the controls after 14 days of desiccation (salinity 144). Rewetting did not cause a return to the original community composition, but led to a further change. Pyrosequencing analysis of 16S rRNA genes amplified from the sediment revealed diverse microbial responses, for example desiccation enabled haloversatile Marinobacter species to increase their relative abundance, and thus take advantage of rewetting to grow rapidly and dominate the community. A temporal sequence of effects of desiccation and rewetting were thus observed, but the most notable feature was the overall resistance and resilience of the microbial community.

摘要

盐沼微生物群落经常会遇到干燥和再湿润的周期性胁迫事件。为了研究微生物生物膜对这些胁迫的抵抗力和恢复力,我们让盐沼小溪的沉积物干燥 23 天,然后再湿润 4 天,而对照沉积物则保持在自然潮汐循环下。在干燥沉积物的前 2 毫米中,盐分从 36 逐渐增加到 231,再湿润时恢复到海水盐度。干燥 3 天后,由于底栖硅藻停止向表面迁移,干燥沉积物的叶绿素 a(Chl a)荧光信号降低,随着再湿润,细胞迁移和 Chl a 荧光恢复。干燥过程中,胞外β-葡萄糖苷酶和氨肽酶活性在前一周内下降,但再湿润时急剧增加。干燥 14 天后,干燥沉积物中的细菌群落与对照相比发生了显著变化(盐度为 144)。再湿润不会导致群落组成恢复原状,而是进一步发生变化。从沉积物中扩增的 16S rRNA 基因的焦磷酸测序分析显示,微生物有多种响应方式,例如干燥使耐盐性更强的 Marinobacter 物种增加了相对丰度,从而在再湿润时迅速生长并占据主导地位。因此,我们观察到了干燥和再湿润的时间序列效应,但最显著的特征是微生物群落的整体抵抗力和恢复力。

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