[1] Pan Y, Birdsey RA, Fang J, et al. A large and persistent carbon sink in the world’s forests. Science, 2011, 333: 988-993 [2] IPCC. Climate Change 2013: The Physical Science Basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge: Cambridge University Press, 2013 [3] Yuan X, Si Y, Lin W, et al. Effects of short-term warming and nitrogen addition on the quantity and quality of dissolved organic matter in a subtropical Cunninghamia lanceolata plantation. PLoS One, 2018, 13: e0191403 [4] Liu F, Kou D, Abbott BW, et al. Disentangling the effects of climate, vegetation, soil and related substrate properties on the biodegradability of permafrost-derived dissolved organic carbon. Journal of Geophysical Research: Biogeosciences, 2019, 124: 3377-3389 [5] Nguyen HVM, Choi JH. Changes in the dissolved organic matter leaching from soil under severe temperature and N-deposition. Environmental Monitoring and Assessment, 2015, 187: 323 [6] Urbanek E. Why are aggregates destroyed in low intensity fire? Plant and Soil, 2013, 362: 33-36 [7] Yin H, Li Y, Xiao J, et al. Enhanced root exudation stimulates soil nitrogen transformations in a subalpine coniferous forest under experimental warming. Global Change Biology, 2013, 19: 2158-2167 [8] Meng C, Tian D, Zeng H, et al. Global meta-analysis on the responses of soil extracellular enzyme activities to warming. Science of the Total Environment, 2020, 705: 135992 [9] Rehschuh R, Rehschuh S, Gast A, et al. Tree allocation dynamics beyond heat and hot drought stress reveal changes in carbon storage, belowground translocation and growth. New Phytologist, 2022, 233: 687-704 [10] Wang HC, Chou CY, Chiou CR, et al. Humic acid composition and characteristics of soil organic matter in relation to the elevation gradient of Moso bamboo plantations. PLoS One, 2016, 11: e0162193 [11] Loomis SE, Russell JM, Verschuren D, et al. The tropical lapse rate steepened during the Last Glacial Maximum. Science Advances, 2017, 3: e1600815 [12] Keller AB, Phillips RP. Leaf litter decay rates differ between mycorrhizal groups in temperate, but not tropical, forests. New Phytologist, 2019, 222: 556-564 [13] Guo J, Yang Z, Lin C, et al. Conversion of a natural evergreen broadleaved forest into coniferous plantations in a subtropical area: Effects on composition of soil microbial communities and soil respiration. Biology and Fertility of Soils, 2016, 52: 799-809 [14] Ohno T. Fluorescence inner-filtering correction for determining the humification index of dissolved organic matter. Environmental Science & Technology, 2002, 36: 742-746 [15] McKnight DM, Boyer EW, Westerhoff PK, et al. Spectrofluorometric characterization of dissolved organic matter for indication of precursor organic material and aromaticity. Limnology and Oceanography, 2001, 46: 38-48 [16] Birdwell JE, Engel AS. Characterization of dissolved organic matter in cave and spring waters using UV-Vis absorbance and fluorescence spectroscopy. Organic Geochemistry, 2010, 41: 270-280 [17] 丁一汇, 司东, 柳艳菊, 等. 论东亚夏季风的特征、驱动力与年代际变化. 大气科学, 2018, 42(3): 533-558 [18] 林捷, 叶功富, 黄石德, 等. 武夷山中亚热带常绿阔叶林凋落物量动态研究. 防护林科技, 2019(10): 1-5 [19] Liu J, Liu S, Li Y, et al. Warming effects on the decomposition of two litter species in model subtropical forests. Plant and Soil, 2017, 420: 277-287 [20] Lu M, Zhou X, Yang Q, et al. Responses of ecosystem carbon cycle to experimental warming: A meta-analysis. Ecology, 2013, 94: 726-738 [21] Kermavnar J, Vilhar U. Canopy precipitation interception in urban forests in relation to stand structure. Urban Ecosystems, 2017, 20: 1373-1387 [22] Querejeta JI, Ren W, Prieto I. Vertical decoupling of soil nutrients and water under climate warming reduces plant cumulative nutrient uptake, water-use efficiency and productivity. New Phytologist, 2021, 230: 1378-1393 [23] 杨成邦, 张丽, 高艳丽, 等. 增温对湿润亚热带杉木幼林和成熟林土壤无机氮的影响. 应用生态学报, 2020, 31(9): 2849-2856 [24] Migliorini GH, Romero GQ. Warming and leaf litter functional diversity, not litter quality, drive decomposition in a freshwater ecosystem. Scientific Reports, 2020, 10: 20333 [25] Li A, Fan Y, Chen S, et al. Soil warming did not enhance leaf litter decomposition in two subtropical forests. Soil Biology and Biochemistry, 2022, 170: 108716 [26] Liu X, Chen S, Yang Z, et al. Will heterotrophic soil respiration be more sensitive to warming than autotrophic respiration in subtropical forests? European Journal of Soil Science, 2019, 70: 655-663 [27] Eusterhues K, Rumpel C, Kleber M, et al. Stabilisation of soil organic matter by interactions with minerals as revealed by mineral dissolution and oxidative degradation. Organic Geochemistry, 2003, 34: 1591-1600 [28] Roth VN, Lange M, Simon C, et al. Persistence of dissolved organic matter explained by molecular changes during its passage through soil. Nature Geoscience, 2019, 12: 755-761 [29] Leinemann T, Preusser S, Mikutta R, et al. Multiple exchange processes on mineral surfaces control the transport of dissolved organic matter through soil profiles. Soil Biology and Biochemistry, 2018, 118: 79-90 [30] Avneri-Katz S, Young RB, McKenna AM, et al. Adsorptive fractionation of dissolved organic matter (DOM) by mineral soil: Macroscale approach and molecular insight. Organic Geochemistry, 2017, 103: 113-124 [31] Suseela V, Tharayil N, Xing B, et al. Labile compounds in plant litter reduce the sensitivity of decomposition to warming and altered precipitation. New Phytologist, 2013, 200: 122-133 [32] Ohno T, Parr TB, Gruselle MCI, et al. Molecular composition and biodegradability of soil organic matter: A case study comparing two New England forest types. Environmental Science & Technology, 2014, 48: 7229-7236 [33] Liu W, Jiang Y, Su Y, et al. Warming affects soil nitrogen mineralization via changes in root exudation and associated soil microbial communities in a subalpine tree species Abies fabri. Journal of Soil Science and Plant Nutrition, 2022, 22: 406-415 |