Interactive effects of mercuric oxide nanoparticles and future climate CO2 on maize plant

2021 ◽  
Vol 401 ◽  
pp. 123849
Author(s):  
Ahmed M. Saleh ◽  
Yasser M. Hassan ◽  
Talaat H. Habeeb ◽  
Areej A. Alkhalaf ◽  
Wael N. Hozzein ◽  
...  
2020 ◽  
Vol 749 ◽  
pp. 142356
Author(s):  
Hamada AbdElgawad ◽  
Yasser M. Hassan ◽  
Modhi O. Alotaibi ◽  
Afrah E. Mohammed ◽  
Ahmed M. Saleh

2009 ◽  
Vol 276 (1663) ◽  
pp. 1883-1888 ◽  
Author(s):  
Maria Byrne ◽  
Melanie Ho ◽  
Paulina Selvakumaraswamy ◽  
Hong D. Nguyen ◽  
Symon A. Dworjanyn ◽  
...  

Global warming is causing ocean warming and acidification. The distribution of Heliocidaris erythrogramma coincides with the eastern Australia climate change hot spot, where disproportionate warming makes marine biota particularly vulnerable to climate change. In keeping with near-future climate change scenarios, we determined the interactive effects of warming and acidification on fertilization and development of this echinoid. Experimental treatments (20–26°C, pH 7.6–8.2) were tested in all combinations for the ‘business-as-usual’ scenario, with 20°C/pH 8.2 being ambient. Percentage of fertilization was high (>89%) across all treatments. There was no difference in percentage of normal development in any pH treatment. In elevated temperature conditions, +4°C reduced cleavage by 40 per cent and +6°C by a further 20 per cent. Normal gastrulation fell below 4 per cent at +6°C. At 26°C, development was impaired. As the first study of interactive effects of temperature and pH on sea urchin development, we confirm the thermotolerance and pH resilience of fertilization and embryogenesis within predicted climate change scenarios, with negative effects at upper limits of ocean warming. Our findings place single stressor studies in context and emphasize the need for experiments that address ocean warming and acidification concurrently. Although ocean acidification research has focused on impaired calcification, embryos may not reach the skeletogenic stage in a warm ocean.


2009 ◽  
Vol 9 (2) ◽  
pp. 6147-6206 ◽  
Author(s):  
T. Keenan ◽  
Ü. Niinemets ◽  
S. Sabate ◽  
C. Gracia ◽  
J. Peñuelas

Abstract. Large uncertainties exist in our knowledge of regional emissions of non-methane biogenic volatile organic compounds (BVOC). We address these uncertainties through a two-pronged approach by compiling a state of the art database of the emissions potentials for 80 European forest species, and by a model assessment and inter-comparison, both at the local and regional scale, under present and projected future climatic conditions. We coupled three contrasting isoprenoid models with the ecophysiological forest model GOTILWA+ to explore the interactive effects of climate, vegetation distribution, and productivity, on leaf and ecosystem isoprenoid emissions, and to consider model behaviour in present climate and under projected future climate change conditions. Hourly, daily and annual isoprene emissions as simulated by the models were evaluated against flux measurements. The validation highlighted a general model capacity to capture gross fluxes but inefficiencies in capturing short term variability. A regional inventory of isoprenoid emissions for European forests was created using each of the three modelling approaches. The models agreed on an average European emissions budget of 1.03 TgC a−1 for isoprene and 0.97 TgC a−1 for monoterpenes for the period 1960–1990, which was dominated by a few species with largest aerial coverage. Species contribution to total emissions depended both on species emission potential and geographical distribution. For projected future climate conditions, however, emissions budgets proved highly model dependent, illustrating the current uncertainty associated with isoprenoid emissions responses to potential future conditions. These results suggest that current model estimates of isoprenoid emissions concur well, but future estimates are highly uncertain. We conclude that development of reliable models is highly urgent, but for the time being, future BVOC emission scenario estimates should consider results from an ensemble of available emission models.


2019 ◽  
Vol 15 (3) ◽  
pp. 315-323 ◽  
Author(s):  
Chang-Beom Park ◽  
Jae-Woong Jung ◽  
Dong-Hyuk Yeom ◽  
Jiyi Jang ◽  
Jin-Woo Park ◽  
...  

2019 ◽  
Vol 286 (1896) ◽  
pp. 20181887 ◽  
Author(s):  
Zhiguang Qiu ◽  
Melinda A. Coleman ◽  
Euan Provost ◽  
Alexandra H. Campbell ◽  
Brendan P. Kelaher ◽  
...  

Climate change is driving global declines of marine habitat-forming species through physiological effects and through changes to ecological interactions, with projected trajectories for ocean warming and acidification likely to exacerbate such impacts in coming decades. Interactions between habitat-formers and their microbiomes are fundamental for host functioning and resilience, but how such relationships will change in future conditions is largely unknown. We investigated independent and interactive effects of warming and acidification on a large brown seaweed, the kelp Ecklonia radiata , and its associated microbiome in experimental mesocosms. Microbial communities were affected by warming and, during the first week, by acidification. During the second week, kelp developed disease-like symptoms previously observed in the field. The tissue of some kelp blistered, bleached and eventually degraded, particularly under the acidification treatments, affecting photosynthetic efficiency. Microbial communities differed between blistered and healthy kelp for all treatments, except for those under future conditions of warming and acidification, which after two weeks resembled assemblages associated with healthy hosts. This indicates that changes in the microbiome were not easily predictable as the severity of future climate scenarios increased. Future ocean conditions can change kelp microbiomes and may lead to host disease, with potentially cascading impacts on associated ecosystems.


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