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热融塌陷加剧多年冻土区土壤呼吸对气候变暖的响应 快报文章
资源环境快报,2024年第9期
作者:  董利苹
Microsoft Word(21Kb)  |  收藏  |  浏览/下载:508/0  |  提交时间:2024/05/15
Enhanced Response  Thermokarst  Soil Respiration  
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:25/0  |  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.


  
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:70/0  |  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.


  
Increased high-latitude photosynthetic carbon gain offset by respiration carbon loss during an anomalous warm winter to spring transition 期刊论文
GLOBAL CHANGE BIOLOGY, 2019
作者:  Liu, Zhihua;  Kimball, John S.;  Parazoo, Nicholas C.;  Ballantyne, Ashley P.;  Wang, Wen J.;  Madani, Nima;  Pan, Caleb G.;  Watts, Jennifer D.;  Reichle, Rolf H.;  Sonnentag, Oliver;  Marsh, Philip;  Hurkuck, Miriam;  Helbig, Manuel;  Quinton, William L.;  Zona, Donatella;  Ueyama, Masahito;  Kobayashi, Hideki;  Euskirchen, Eugenie S.
收藏  |  浏览/下载:12/0  |  提交时间:2019/11/27
ABoVE  boreal  carbon cycle  climate change  productivity  respiration  SMAP L4C  soil moisture  tundra  
Plant respiration: Controlled by photosynthesis or biomass? 期刊论文
GLOBAL CHANGE BIOLOGY, 2019
作者:  Collalti, Alessio;  Tjoelker, Mark G.;  Hoch, Guenter;  Makela, Annikki;  Guidolotti, Gabriele;  Heskel, Mary;  Petit, Giai;  Ryan, Michael G.;  Battipaglia, Giovanna;  Matteucci, Giorgio;  Prentice, Iain Colin
收藏  |  浏览/下载:22/0  |  提交时间:2019/11/27
biomass accumulation  carbon use efficiency  gross primary production  maintenance respiration  metabolic scaling theory  net primary production  nonstructural carbohydrates  plant respiration  
Intensified inundation shifts a freshwater wetland from a CO2 sink to a source 期刊论文
GLOBAL CHANGE BIOLOGY, 2019, 25 (10) : 3319-3333
作者:  Zhao, Junbin;  Malone, Sparkle L.;  Oberbauer, Steven F.;  Olivas, Paulo C.;  Schedlbauer, Jessica L.;  Staudhammer, Christina L.;  Starr, Gregory
收藏  |  浏览/下载:9/0  |  提交时间:2019/11/27
ecosystem respiration  flooding  gross primary production  hydrology  net ecosystem CO2 exchange  wetland  
How eddy covariance flux measurements have contributed to our understanding of Global Change Biology 期刊论文
GLOBAL CHANGE BIOLOGY, 2019
作者:  Baldocchi, Dennis D.
收藏  |  浏览/下载:6/0  |  提交时间:2019/11/27
eddy covariance  carbon dioxide  water vapor  evaporation  ecosystem  photosynthesis  ecosystem respiration  
Microbial community responses reduce soil carbon loss in Tibetan alpine grasslands under short-term warming 期刊论文
GLOBAL CHANGE BIOLOGY, 2019, 25 (10) : 3438-3449
作者:  Li, Yaoming;  Lv, Wangwang;  Jiang, Lili;  Zhang, Lirong;  Wang, Shiping;  Wang, Qi;  Xue, Kai;  Li, Bowen;  Liu, Peipei;  Hong, Huan;  Renzen, Wangmu;  Wang, A.;  Luo, Caiyun;  Zhang, Zhenhua;  Dorji, Tsechoe;  Tas, Neslihan;  Wang, Zhezhen;  Zhou, Huakun;  Wang, Yanfen
收藏  |  浏览/下载:11/0  |  提交时间:2019/11/27
labile carbon limitation  microbial community response  soil heterotrophic respiration  soil incubation  soil respiration acclimation  
Increasing microbial carbon use efficiency with warming predicts soil heterotrophic respiration globally 期刊论文
GLOBAL CHANGE BIOLOGY, 2019, 25 (10) : 3354-3364
作者:  Ye, Jian-Sheng;  Bradford, Mark A.;  Dacal, Marina;  Maestre, Fernando T.;  Garcia-Palacios, Pablo
收藏  |  浏览/下载:11/0  |  提交时间:2019/11/27
CO2 efflux  global warming  microbe  soil carbon stock  soil respiration  
Nitrate addition stimulates microbial decomposition of organic matter in salt marsh sediments 期刊论文
GLOBAL CHANGE BIOLOGY, 2019, 25 (10) : 3224-3241
作者:  Bulseco, Ashley N.;  Giblin, Anne E.;  Tucker, Jane;  Murphy, Anna E.;  Sanderman, Jonathan;  Hiller-Bittrolff, Kenly;  Bowen, Jennifer L.
收藏  |  浏览/下载:5/0  |  提交时间:2019/11/27
16S rRNA gene  anaerobic respiration  decomposition  flow-through reactor  microbes  nitrate  organic matter  salt marsh