| Literature DB >> 29868044 |
Abstract
Systems studies of drought stress in resurrection plants and other xerophytes are rapidly identifying a large number of genes, proteins and metabolites that respond to severe drought stress or desiccation. This has provided insight into drought resistance mechanisms, which allow xerophytes to persist under such extreme environmental conditions. Some of the mechanisms that ensure cellular protection during severe dehydration appear to be unique to desert species, while many other stress signaling pathways are in common with well-studied model and crop species. However, despite the identification of many desiccation inducible genes, there are few "gene-to-field" examples that have led to improved drought tolerance and yield stability derived from resurrection plants, and only few examples have emerged from model species. This has led to many critical reviews on the merit of the experimental approaches and the type of plants used to study drought resistance mechanisms. This article discusses the long-standing arguments between the ecophysiology and molecular biology communities, on how to "drought-proof" future crop varieties. It concludes that a more positive and inclusive dialogue between the different disciplines is needed, to allow us to move forward in a much more constructive way.Entities:
Keywords: Arabidopsis; drought avoidance; drought survival; drought tolerance; extremophiles
Year: 2018 PMID: 29868044 PMCID: PMC5962824 DOI: 10.3389/fpls.2018.00543
Source DB: PubMed Journal: Front Plant Sci ISSN: 1664-462X Impact factor: 5.753
Comparison of growth conditions in transcriptome, proteome, metabolome, and physiological studies of extremophiles.
| Negev Desert: temperature range−3.6 to 46.8°C, arid | 16 h day; 150 μmol m−2 s−1; 22°C, RH not specified | Growth cabinet | Metabolic profiling/salt and heat stress (MS agar medium) | Eshel et al., | |
| Accession: Yukon | Yukon territory: temperature range 15–24°C, light 1,500 μmol m−2 s−1, semi-arid | 21 h day, 250 μmol m−2 s−1, 22/10°C, RH not specified | Growth cabinet and native habitat | Transcriptome/control vs. native habitat (soil grown) | Champigny et al., |
| Accession: Shangdon | 21 h day, 250 μmol m−2 s−1, 22/10°C, RH not specified | Growth cabinet | Transcriptome/of natural variation (soil grown) | Champigny et al., | |
| Accession: Yukon | Yukon territory: temperature range 15–24°C, light 1,500 μmol m−2 s−1, semi-arid | 21 h day, 250 μmol m−2 s−1, 22/10°C, RH not specified | Growth cabinet and native habitat | Transcriptome and metabolome/ control vs. native habitats (soil grown) | Guevara et al., |
| Bahrah (Saudi Arabia): day temperature 36–43°C, light >1,000 μmol m−2 s−1, arid | Not applicable | Native habitat | Diurnal transcriptome | Yates et al., | |
| Bahrah (Saudi Arabia): day temperature 36–43°C, light >1,000 μmol m−2 s−1, arid | Not applicable | Native habitat | Diurnal changes in photosynthesis leaf physiology | Lawson et al., | |
| Salt flats in Tuz (Central Anatolia, Turkey) | 12 h day, 22/20°C, 60%RH, light not specified | Growth cabinet | Chloroplast physiology, salt stress (soil mixture) | Uzilday et al., | |
| South Africa (conditions not specified) | 16 h day, 4,000 lux, 23/19°C RH not specified | Growth cabinet | Transcriptome/different dehydration levels (artificial clay) | Rodriguez et al., | |
| South Africa (conditions not specified) | 14 h day, 24/20°C, 60,000 lx, 60% RH | Growth cabinet | Expression profile of GRP1/desiccation (clay) | Giarola et al., | |
| South Africa (conditions not specified) | Growth cabinet | Expression profile of EDR1 and CRP1/dehydration and rehydration (clay) | Giarola et al., | ||
| Verena, Transvaal, South Africa | 16 h day, 28/19°C, light and RH not specified | Growth cabinet | Transcriptome and metabolome/dehydration and rehydration (soil) | Yobi et al., | |
| 16 h day, 28/19°C, light and RH not specified | Growth cabinet | Proteome/dehydration (soil) | Oliver et al., | ||
| 16 h day, 28/19°C, light and RH not specified | Growth cabinet | Metabolome/during dehydration (soil) Comparison with | Oliver et al., | ||
| Yinchuan City, Ningxia, China | 16 h day, 28/16°C, natural light (intensity not specified) | Growth cabinet | Transcriptome/drought stress (soil and vermiculite) | Ma et al., | |
| Rhodope Mountains, Bulgaria, light at harvesting side 20 μE m−2 s−1 | 16 h day, 21°C, 20 μE m−2 s−1, RH 65% | Growth cabinet | Transcriptome and metabolomics (soil) | Gechev et al., | |
| Desert areas in China and Mongolia | 16 h day, 28/23°C, 800 μmol m−2 s−1, RH 65–70% | Growth cabinet | Transcriptome/ salt and osmotic stress (sand) | Ma et al., | |
| Shapotou Desert Experiment and Research, Ningxia, China | 12 h day, 25°C, 70 μmol m−2 s−1, RH not specified | Growth cabinet | Transcriptome / salt stress (MS agar medium) | Qiu et al., | |
| Saudi Arabia, field site near Jeddah: day temperature 36–43°C, light >1,000 μmol m−2 s−1, arid | 16 h day, 25–28°C, 8,000lx, RH not specified | Growth cabinet | Transcriptome and metabolome/salt and drought stress (growth medium not specified) | Mutwakil et al., | |
| Vargas State, Venezuela: light 100–1,500 μmol m−2 s−1, temperature 25–32°C, RH 65–85% | Not applicable | Native habitat | Photosynthetic physiology | Tezara et al., | |
RH, relative humidity.