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Progressive nitrogen limitation across the Tibetan alpine permafrost region 期刊论文
NATURE COMMUNICATIONS, 2020, 11 (1)
作者:  Kou, Dan;  Yang, Guibiao;  Li, Fei;  Feng, Xuehui;  Zhang, Dianye;  Mao, Chao;  Zhang, Qiwen;  Peng, Yunfeng;  Ji, Chengjun;  Zhu, Qiuan;  Fang, Yunting;  Liu, Xueyan;  Xu-Ri;  Li, Siqi;  Deng, Jia;  Zheng, Xunhua;  Fang, Jingyun;  Yang, Yuanhe
收藏  |  浏览/下载:21/0  |  提交时间:2020/07/06
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:26/0  |  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.


  
Fast response of cold ice-rich permafrost in northeast Siberia to a warming climate 期刊论文
NATURE COMMUNICATIONS, 2020, 11 (1)
作者:  Nitzbon, Jan;  Westermann, Sebastian;  Langer, Moritz;  Martin, Leo C. P.;  Strauss, Jens;  Laboor, Sebastian;  BOike, Julia
收藏  |  浏览/下载:13/0  |  提交时间:2020/05/13
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:71/0  |  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.


  
Ocean Carbon Storage across the middle Miocene: a new interpretation for the Monterey Event 期刊论文
NATURE COMMUNICATIONS, 2020, 11 (1)
作者:  Sosdian, S. M.;  Babila, T. L.;  Greenop, R.;  Foster, G. L.;  Lear, C. H.
收藏  |  浏览/下载:4/0  |  提交时间:2020/05/13
Biogeographic variation in temperature sensitivity of decomposition in forest soils 期刊论文
GLOBAL CHANGE BIOLOGY, 2019
作者:  Li, Jinquan;  Nie, Ming;  Pendall, Elise;  Reich, Peter B.;  Pei, Junmin;  Noh, Nam Jin;  Zhu, Ting;  Li, Bo;  Fang, Changming
收藏  |  浏览/下载:10/0  |  提交时间:2019/11/27
carbon cycle  carbon cycle modelling  carbon decomposition  climate change  forest  Q(10)  spatial heterogeneity  temperature sensitivity  
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:10/0  |  提交时间:2019/11/27
ecosystem respiration  flooding  gross primary production  hydrology  net ecosystem CO2 exchange  wetland  
Accumulation of soil carbon under elevated CO2 unaffected by warming and drought 期刊论文
GLOBAL CHANGE BIOLOGY, 2019, 25 (9) : 2970-2977
作者:  Dietzen, Christiana A.;  Larsen, Klaus Steenberg;  Ambus, Per L.;  Michelsen, Anders;  Arndal, Marie Frost;  Beier, Claus;  Reinsch, Sabine;  Schmidt, Inger Kappel
收藏  |  浏览/下载:13/0  |  提交时间:2019/11/27
climate driver interactions  drought  elevated CO2  FACE  multifactor climate change experiment  soil carbon  warming  
Anthropogenic N deposition alters soil organic matter biochemistry and microbial communities on decaying fine roots 期刊论文
GLOBAL CHANGE BIOLOGY, 2019
作者:  Argiroff, William A.;  Zak, Donald R.;  Upchurch, Rima A.;  Salley, Sydney O.;  Grandy, A. Stuart
收藏  |  浏览/下载:13/0  |  提交时间:2019/11/27
bacterial community  biogeochemical feedback  fungal community  lignin  microbial decomposition  root decay  soil carbon  
Negative feedback processes following drainage slow down permafrost degradation 期刊论文
GLOBAL CHANGE BIOLOGY, 2019, 25 (10) : 3254-3266
作者:  Goeckede, Mathias;  Kwon, Min Jung;  Kittler, Fanny;  Heimann, Martin;  Zimov, Nikita;  Zimov, Sergey
收藏  |  浏览/下载:9/0  |  提交时间:2019/11/27
Arctic climate change  drainage disturbance  energy redistribution  long-term effects  permafrost carbon