GSTDTAP

浏览/检索结果: 共8条,第1-8条 帮助

已选(0)清除 条数/页:   排序方式:
Millennial-scale hydroclimate control of tropical soil carbon storage 期刊论文
NATURE, 2020, 581 (7806) : 63-+
作者:  Lam, Tommy Tsan-Yuk;  Jia, Na;  Zhang, Ya-Wei;  Shum, Marcus Ho-Hin;  Jiang, Jia-Fu;  Zhu, Hua-Chen;  Tong, Yi-Gang;  Shi, Yong-Xia;  Ni, Xue-Bing;  Liao, Yun-Shi;  Li, Wen-Juan;  Jiang, Bao-Gui;  Wei, Wei;  Yuan, Ting-Ting;  Zheng, Kui;  Cui, Xiao-Ming;  Li, Jie;  Pei, Guang-Qian
收藏  |  浏览/下载:61/0  |  提交时间:2020/05/13

Over the past 18,000 years, the residence time and amount of soil carbon stored in the Ganges-Brahmaputra basin have been controlled by the intensity of Indian Summer Monsoon rainfall, with greater carbon destabilization during wetter, warmer conditions.


The storage of organic carbon in the terrestrial biosphere directly affects atmospheric concentrations of carbon dioxide over a wide range of timescales. Within the terrestrial biosphere, the magnitude of carbon storage can vary in response to environmental perturbations such as changing temperature or hydroclimate(1), potentially generating feedback on the atmospheric inventory of carbon dioxide. Although temperature controls the storage of soil organic carbon at mid and high latitudes(2,3), hydroclimate may be the dominant driver of soil carbon persistence in the tropics(4,5)  however, the sensitivity of tropical soil carbon turnover to large-scale hydroclimate variability remains poorly understood. Here we show that changes in Indian Summer Monsoon rainfall have controlled the residence time of soil carbon in the Ganges-Brahmaputra basin over the past 18,000 years. Comparison of radiocarbon ages of bulk organic carbon and terrestrial higher-plant biomarkers with co-located palaeohydrological records(6) reveals a negative relationship between monsoon rainfall and soil organic carbon stocks on a millennial timescale. Across the deglaciation period, a depletion of basin-wide soil carbon stocks was triggered by increasing rainfall and associated enhanced soil respiration rates. Our results suggest that future hydroclimate changes in tropical regions are likely to accelerate soil carbon destabilization, further increasing atmospheric carbon dioxide concentrations.


  
Plant 22-nt siRNAs mediate translational repression and stress adaptation 期刊论文
NATURE, 2020, 581 (7806) : 89-+
作者:  Roulis, Manolis;  Kaklamanos, Aimilios;  Schernthanner, Marina;  Bielecki, Piotr;  Zhao, Jun;  Kaffe, Eleanna;  Frommelt, Laura-Sophie;  Qu, Rihao;  Knapp, Marlene S.;  Henriques, Ana;  Chalkidi, Niki;  Koliaraki, Vasiliki;  Jiao, Jing;  Brewer, J. Richard;  Bacher, Maren;  Blackburn, Holly N.;  Zhao, Xiaoyun;  Breyer, Richard M.;  Aidinis, Vassilis;  Jain, Dhanpat;  Su, Bing;  Herschman, Harvey R.;  Kluger, Yuval;  Kollias, George;  Flavell, Richard A.
收藏  |  浏览/下载:54/0  |  提交时间:2020/07/03

Characterization of 22-nucleotide short interfering RNAs in plants finds that they accumulate in response to environmental stress, causing translational repression, inhibition of plant growth and enhanced stress responses.


Small interfering RNAs (siRNAs) are essential for proper development and immunity in eukaryotes(1). Plants produce siRNAs with lengths of 21, 22 or 24 nucleotides. The 21- and 24-nucleotide species mediate cleavage of messenger RNAs and DNA methylation(2,3), respectively, but the biological functions of the 22-nucleotide siRNAs remain unknown. Here we report the identification and characterization of a group of endogenous 22-nucleotide siRNAs that are generated by the DICER-LIKE 2 (DCL2) protein in plants. When cytoplasmic RNA decay and DCL4 are deficient, the resulting massive accumulation of 22-nucleotide siRNAs causes pleiotropic growth disorders, including severe dwarfism, meristem defects and pigmentation. Notably, two genes that encode nitrate reductases-NIA1 and NIA2-produce nearly half of the 22-nucleotide siRNAs. Production of 22-nucleotide siRNAs triggers the amplification of gene silencing and induces translational repression both gene specifically and globally. Moreover, these 22-nucleotide siRNAs preferentially accumulate upon environmental stress, especially those siRNAs derived from NIA1/2, which act to restrain translation, inhibit plant growth and enhance stress responses. Thus, our research uncovers the unique properties of 22-nucleotide siRNAs, and reveals their importance in plant adaptation to environmental stresses.


  
The fate of carbon in a mature forest under carbon dioxide enrichment 期刊论文
NATURE, 2020, 580 (7802) : 227-+
作者:  Sun, P. Z.;  Yang, Q.;  Kuang, W. J.;  Stebunov, Y. V.;  Xiong, W. Q.;  Yu, J.;  Nair, R. R.;  Katsnelson, M. I.;  Yuan, S. J.;  Grigorieva, I. V.;  Lozada-Hidalgo, M.;  Wang, F. C.;  Geim, A. K.
收藏  |  浏览/下载:89/0  |  提交时间:2020/05/13

Carbon dioxide enrichment of a mature forest resulted in the emission of the excess carbon back into the atmosphere via enhanced ecosystem respiration, suggesting that mature forests may be limited in their capacity to mitigate climate change.


Atmospheric carbon dioxide enrichment (eCO(2)) can enhance plant carbon uptake and growth(1-5), thereby providing an important negative feedback to climate change by slowing the rate of increase of the atmospheric CO2 concentration(6). Although evidence gathered from young aggrading forests has generally indicated a strong CO2 fertilization effect on biomass growth(3-5), it is unclear whether mature forests respond to eCO(2) in a similar way. In mature trees and forest stands(7-10), photosynthetic uptake has been found to increase under eCO(2) without any apparent accompanying growth response, leaving the fate of additional carbon fixed under eCO(2) unclear(4,5,7-11). Here using data from the first ecosystem-scale Free-Air CO2 Enrichment (FACE) experiment in a mature forest, we constructed a comprehensive ecosystem carbon budget to track the fate of carbon as the forest responded to four years of eCO(2) exposure. We show that, although the eCO(2) treatment of +150 parts per million (+38 per cent) above ambient levels induced a 12 per cent (+247 grams of carbon per square metre per year) increase in carbon uptake through gross primary production, this additional carbon uptake did not lead to increased carbon sequestration at the ecosystem level. Instead, the majority of the extra carbon was emitted back into the atmosphere via several respiratory fluxes, with increased soil respiration alone accounting for half of the total uptake surplus. Our results call into question the predominant thinking that the capacity of forests to act as carbon sinks will be generally enhanced under eCO(2), and challenge the efficacy of climate mitigation strategies that rely on ubiquitous CO2 fertilization as a driver of increased carbon sinks in global forests.


  
Hydrogen peroxide sensor HPCA1 is an LRR receptor kinase in Arabidopsis 期刊论文
NATURE, 2020, 578 (7796) : 577-+
作者:  Bogomilov, M.;  Tsenov, R.;  Vankova-Kirilova, G.;  Song, Y. P.;  Tang, J. Y.;  Li, Z. H.;  Bertoni, R.;  Bonesini, M.;  Chignoli, F.;  Mazza, R.;  Palladino, V;  de Bari, A.;  Orestano, D.;  Tortora, L.;  Kuno, Y.;  Sakamoto, H.;  Sato, A.;  Ishimoto, S.;  Chung, M.;  Sung, C. K.;  Filthaut, F.;  Jokovic, D.;  Maletic, D.;  Savic, M.;  Jovancevic, N.;  Nikolov, J.;  Vretenar, M.;  Ramberger, S.;  Asfandiyarov, R.;  Blondel, A.;  Drielsma, F.;  Karadzhov, Y.;  Boyd, S.;  Greis, J. R.;  Lord, T.;  Pidcott, C.;  Taylor, I;  Charnley, G.;  Collomb, N.;  Dumbell, K.;  Gallagher, A.;  Grant, A.;  Griffiths, S.;  Hartnett, T.;  Martlew, B.;  Moss, A.;  Muir, A.;  Mullacrane, I;  Oates, A.;  Owens, P.;  Stokes, G.;  Warburton, P.;  White, C.;  Adams, D.;  Bayliss, V;  Boehm, J.;  Bradshaw, T. W.;  Brown, C.;  Courthold, M.;  Govans, J.;  Hills, M.;  Lagrange, J-B;  Macwaters, C.;  Nichols, A.;  Preece, R.;  Ricciardi, S.;  Rogers, C.;  Stanley, T.;  Tarrant, J.;  Tucker, M.;  Watson, S.;  Wilson, A.;  Bayes, R.;  Nugent, J. C.;  Soler, F. J. P.;  Chatzitheodoridis, G. T.;  Dick, A. J.;  Ronald, K.;  Whyte, C. G.;  Young, A. R.;  Gamet, R.;  Cooke, P.;  Blackmore, V. J.;  Colling, D.;  Dobbs, A.;  Dornan, P.;  Franchini, P.;  Hunt, C.;  Jurj, P. B.;  Kurup, A.;  Long, K.;  Martyniak, J.;  Middleton, S.;  Pasternak, J.;  Uchida, M. A.;  Cobb, J. H.;  Booth, C. N.;  Hodgson, P.;  Langlands, J.;  Overton, E.;  Pec, V;  Smith, P. J.;  Wilbur, S.;  Ellis, M.;  Gardener, R. B. S.;  Kyberd, P.;  Nebrensky, J. J.;  DeMello, A.;  Gourlay, S.;  Lambert, A.;  Li, D.;  Luo, T.;  Prestemon, S.;  Virostek, S.;  Palmer, M.;  Witte, H.;  Adey, D.;  Bross, A. D.;  Bowring, D.;  Liu, A.;  Neuffer, D.;  Popovic, M.;  Rubinov, P.;  Freemire, B.;  Hanlet, P.;  Kaplan, D. M.;  Mohayai, T. A.;  Rajaram, D.;  Snopok, P.;  Torun, Y.;  Cremaldi, L. M.;  Sanders, D. A.;  Summers, D. J.;  Coney, L. R.;  Hanson, G. G.;  Heidt, C.
收藏  |  浏览/下载:78/0  |  提交时间:2020/07/03

Hydrogen peroxide (H2O2) is a major reactive oxygen species in unicellular and multicellular organisms, and is produced extracellularly in response to external stresses and internal cues(1-4). H2O2 enters cells through aquaporin membrane proteins and covalently modifies cytoplasmic proteins to regulate signalling and cellular processes. However, whether sensors for H2O2 also exist on the cell surface remains unknown. In plant cells, H2O2 triggers an influx of Ca2+ ions, which is thought to be involved in H2O2 sensing and signalling. Here, by using forward genetic screens based on Ca2+ imaging, we isolated hydrogen-peroxide-induced Ca(2+)increases (hpca) mutants in Arabidopsis, and identified HPCA1 as a leucine-rich-repeat receptor kinase belonging to a previously uncharacterized subfamily that features two extra pairs of cysteine residues in the extracellular domain. HPCA1 is localized to the plasma membrane and is activated by H2O2 via covalent modification of extracellular cysteine residues, which leads to autophosphorylation of HPCA1. HPCA1 mediates H2O2-induced activation of Ca2+ channels in guard cells and is required for stomatal closure. Our findings help to identify how the perception of extracellular H2O2 is integrated with responses to various external stresses and internal cues in plants, and have implications for the design of crops with enhanced fitness.


HPCA1, a member of a previously uncharacterized subfamily of leucine-rich-repeat receptor-like kinases, is the hydrogen-peroxide sensor at the plasma membrane in Arabidopsis.


  
Response of maize biomass and soil water fluxes on elevated CO2 and drought-From field experiments to process-based simulations 期刊论文
GLOBAL CHANGE BIOLOGY, 2019, 25 (9) : 2947-2957
作者:  Kellner, Juliane;  Houska, Tobias;  Manderscheid, Remy;  Weigel, Hans-Joachim;  Breuer, Lutz;  Kraft, Philipp
收藏  |  浏览/下载:34/0  |  提交时间:2019/11/27
CO2 response  coupled hydrological-plant growth model  evaporation  free-air carbon dioxide enrichment  transpiration  Zea mays  
FACE facts hold for multiple generations; Evidence from natural CO2 springs 期刊论文
GLOBAL CHANGE BIOLOGY, 2019, 25 (1) : 1-11
作者:  Saban, Jasmine M.;  Chapman, Mark A.;  Taylor, Gail
收藏  |  浏览/下载:22/0  |  提交时间:2019/04/09
atmospheric CO2  climate change  meta-analysis  natural CO2 spring  plant adaptation  plant response  plasticity  
Plant species or flower colour diversity? Identifying the drivers of public and invertebrate response to designed annual meadows 期刊论文
LANDSCAPE AND URBAN PLANNING, 2018, 180: 103-113
作者:  Hoyle, Helen;  Norton, Briony;  Dunnett, Nigel;  Richards, J. Paul;  Russell, Jean M.;  Warren, Philip
收藏  |  浏览/下载:12/0  |  提交时间:2019/04/09
Urban meadows  Green infrastructure  Flower colour diversity  Plant species diversity  Human aesthetic response  Invertebrate response  
Reconciling seasonal hydraulic risk and plant water use through probabilistic soil-plant dynamics 期刊论文
GLOBAL CHANGE BIOLOGY, 2017, 23 (9)
作者:  Feng, Xue;  Dawson, Todd E.;  Ackerly, David D.;  Santiago, Louis S.;  Thompson, Sally E.
收藏  |  浏览/下载:19/0  |  提交时间:2019/04/09
drought response  plant hydraulic risk  rainfall variability  soil-plant feedback  stochastic soil moisture dynamics