Shinde Suhas, Behpouri Ali, McElwain Jennifer C, Ng Carl K-Y
School of Biology and Environmental Science, University College Dublin, Belfield, Dublin 4, Ireland
School of Biology and Environmental Science, University College Dublin, Belfield, Dublin 4, Ireland.
J Exp Bot. 2015 Jul;66(13):4001-12. doi: 10.1093/jxb/erv197. Epub 2015 May 6.
It is widely accepted that atmospheric O2 has played a key role in the development of life on Earth, as evident from the coincidence between the rise of atmospheric O2 concentrations in the Precambrian and biological evolution. Additionally, it has also been suggested that low atmospheric O2 is one of the major drivers for at least two of the five mass-extinction events in the Phanerozoic. At the molecular level, our understanding of the responses of plants to sub-ambient O2 concentrations is largely confined to studies of the responses of underground organs, e.g. roots to hypoxic conditions. Oxygen deprivation often results in elevated CO2 levels, particularly under waterlogged conditions, due to slower gas diffusion in water compared to air. In this study, changes in the transcriptome of gametophytes of the moss Physcomitrella patens arising from exposure to sub-ambient O2 of 13% (oxygen deprivation) and elevated CO2 (1500 ppmV) were examined to further our understanding of the responses of lower plants to changes in atmospheric gaseous composition. Microarray analyses revealed that the expression of a large number of genes was affected under elevated CO2 (814 genes) and sub-ambient O2 conditions (576 genes). Intriguingly, the expression of comparatively fewer numbers of genes (411 genes) was affected under a combination of both sub-ambient O2 and elevated CO2 condition (low O2-high CO2). Overall, the results point towards the effects of atmospheric changes in CO2 and O2 on transcriptional reprogramming, photosynthetic regulation, carbon metabolism, and stress responses.
大气中的氧气在地球生命发展过程中发挥了关键作用,这一点已被广泛接受,从前寒武纪大气氧气浓度的上升与生物进化的巧合中可见一斑。此外,也有人提出,低大气氧含量是显生宙五次大灭绝事件中至少两次的主要驱动因素之一。在分子水平上,我们对植物对低于环境氧浓度的反应的理解主要局限于对地下器官(如根对缺氧条件)反应的研究。由于与空气相比,水中的气体扩散较慢,缺氧通常会导致二氧化碳水平升高,特别是在涝渍条件下。在本研究中,研究了苔藓小立碗藓配子体暴露于13%的低于环境氧浓度(缺氧)和升高的二氧化碳(1500 ppmV)后转录组的变化,以进一步了解低等植物对大气气体成分变化的反应。微阵列分析显示,大量基因的表达在二氧化碳升高(814个基因)和低于环境氧浓度条件下(576个基因)受到影响。有趣的是,在低于环境氧浓度和二氧化碳升高的组合条件下(低氧-高二氧化碳),受影响的基因数量相对较少(411个基因)。总体而言,结果表明大气中二氧化碳和氧气的变化对转录重编程、光合调节、碳代谢和应激反应有影响。