树干甲烷的研究进展

doi:10.12302/j.issn.1000-2006.202003006

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南京林业大学学报（自然科学版） ›› 2021, Vol. 45 ›› Issue (5): 235-241.doi: 10.12302/j.issn.1000-2006.202003006

树干甲烷的研究进展

郭亮(), 丁九敏, 徐侠^*()

南京林业大学生物与环境学院,南方现代林业协同创新中心,江苏南京 210037

收稿日期:2020-03-03 接受日期:2021-02-25 出版日期:2021-09-30 发布日期:2021-09-30
通讯作者: 徐侠
基金资助:
国家自然科学基金青年科学基金项目(31700376);江苏省高等学校自然科学研究重大项目(17KJA180006);江苏省“六大人才高峰”项目(JY-041&TD-XYDXX-006);江苏高校优势学科建设工程资助项目(PAPD);南京林业大学“5151”人才计划项目

Advances in research on methane from tree stems

GUO Liang(), DING Jiuming, XU Xia^*()

College of Biology and the Environment, Co-Innovation Center for the Sustainable Forestry in Southern China, Nanjing Forestry University, Nanjing 210037, China

Received:2020-03-03 Accepted:2021-02-25 Online:2021-09-30 Published:2021-09-30
Contact: XU Xia

摘要/Abstract

摘要：

在全球变暖背景下,甲烷 (CH₄) 作为陆地生态系统中仅次于CO₂的重要温室气体受到了广泛关注,其在百年时间尺度上的温室效应潜力是CO₂的28~34倍,对全球变暖的贡献占20%~30%。现有对森林生态系统CH₄的研究主要集中在土壤,但基于热带森林地表排放估算和卫星CH₄通量之间的差异报告,以及近年的研究证明了树木是森林CH₄预算的重要来源和汇。笔者综合分析了树干CH₄的来源、通量大小、影响因素及其对陆地碳预算的影响,结果发现:①树干释放出的CH₄是来自土壤或者树木心材,然后主要通过树干扩散释放到空气中;②树干CH₄的通量范围为(-37.5±18.75)~(16 937.50±6 812.50) μmol/(m²·h);③树干表面CH₄通量具有较大的时空差异性,这些差异主要来自树种、年龄、组织类型、立地特征和环境条件等;④在不考虑树干CH₄通量的前提下,森林湿地 (或木本沼泽) 生态系统的CH₄释放量部分可能被低估,而旱地或者高山森林中CH₄的吸收量部分可能被高估。树干甲烷作为陆地碳循环的“新成员”,应该被充分重视,这对于预测未来全球气候变化具有重要意义。

关键词: 树干甲烷, 温室气体, 碳循环, 陆地生态系统

Abstract:

Methane (CH₄) as the second most important greenhouse gas in terrestrial ecosystems after carbon dioxide (CO₂) has received extensive attention in the context of global warming. With the same quantity (number of moles) of greenhouse gas, the greenhouse effect of CH₄ in 100 years is 28 to 34 times that of CO₂, and atmospheric CH₄ is responsible for approximately 20% to 30% of global warming. Reports of a discrepancy between emissions-based estimates and satellite-based estimates of CH₄ sources in tropical forests have generated interest in tree surfaces as a neglected source. Numerous studies in recent years have also proved that trees are an important source and sink of forest CH₄ budget. By review in published literatures, this paper comprehensively analyzed the source, flux size, influencing factors of CH₄ in tree stems and its impact on terrestrial carbon budget. We found that: ① CH₄ released by the stems was produced in the soil or in the heartwood of the tree, and then diffused through the stems into the air.② The flux range of stems CH₄ was from(-37.5±18.75) to (16 937.50±6 812.50) μmol/(m²·h).③ The CH₄ flux on the surface of the stems had a large spatiotemporal difference, which mainly comes from the species, age, tissue type, site characteristics and environmental conditions. ④ The CH₄ released from forest wetland (or woody swamp) might be underestimated, while the CH₄ absorption from dryland or alpine forests might be overestimated, without considering the CH₄ flux from the stems. As a new member of the terrestrial carbon cycle, tree-stems methane should be given sufficient attention, which was of great significance for predicting future global climate change.

Key words: stems methane, greenhouse gases, carbon cycle, terrestrial ecosystem

中图分类号:

S718

郭亮,丁九敏,徐侠. 树干甲烷的研究进展[J]. 南京林业大学学报（自然科学版）, 2021, 45(5): 235-241.

GUO Liang, DING Jiuming, XU Xia. Advances in research on methane from tree stems[J].Journal of Nanjing Forestry University (Natural Science Edition), 2021, 45(5): 235-241.DOI: 10.12302/j.issn.1000-2006.202003006.

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链接本文: http://nldxb.njfu.edu.cn/CN/10.12302/j.issn.1000-2006.202003006

http://nldxb.njfu.edu.cn/CN/Y2021/V45/I5/235

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参考文献 58

[1]	IPCC. Global warming of 1.5 ℃[R/OL]. Cambridge: Cambridge University Press, 2018.https://www.ipcc.ch/site/assets/uploads/sites/2/2019/06/SR15_Full_Report_High_Res.pdf.
[2]	HOEGH-GULDBERG O, JACOB D, TAYLOR M, et al. The human imperative of stabilizing global climate change at 1.5 degrees C[J]. Science, 2019, 365(6459):eaaw6974. DOI: 10.1126/science.aaw6974. doi: 10.1126/science.aaw6974
[3]	IPCC. Climate change 2013-the physical science basis: working group I contribution to the fifth assessment report of the intergovernmental panel on climate change[R/OL]. Cambridge: Cambridge University Press, 2014. https://www.cambridge.org/core/books.
[4]	WU J, LI Q, CHEN J W, et al. Afforestation enhanced soil CH₄ uptake rate in subtropical China: evidence from carbon stable isotope experiments[J]. Soil Biology and Biochemistry, 2018, 118:199-206. DOI: 10.1016/j.soilbio.2017.12.017. doi: 10.1016/j.soilbio.2017.12.017
[5]	FLETCHER S E M, SCHAEFER H. Rising methane: a new climate challenge[J]. Science, 2019, 364(6444):932-933. DOI: 10.1126/science.aax1828. doi: 10.1126/science.aax1828
[6]	何姗, 刘娟, 姜培坤, 等. 全球变化对森林土壤甲烷吸收的影响及其机制研究进展[J]. 应用生态学报, 2019, 30(2):677-684.
	HE S, LIU J, JIANG P K, et al. Effects of global change on methane uptake in forest soils and its mechanisms:a review[J]. Chin J Appl Ecol, 2019, 30(2):677-684.DOI: 10.13287/j.1001-9332.201902.028. doi: 10.13287/j.1001-9332.201902.028
[7]	LE MER J, ROGER A P. Production, oxidation, emission and consumption of methane by soils: a review[J]. European Journal of Soil Biology, 2001, 37(1):25-50. DOI: 10.1016/S1164-5563(01)01067-6. doi: 10.1016/S1164-5563(01)01067-6
[8]	ALLEN G. Biogeochemistry: rebalancing the global methane budget[J]. Nature, 2016, 538(7623):46-48. DOI: 10.1038/538046a. doi: 10.1038/538046a
[9]	SAUNOIS M, BOUSQUET P, POULTER B, et al. Variability and quasi-decadal changes in the methane budget over the period 2000-2012[J]. Atmospheric Chemistry and Physics, 2017, 17(18):11135-11161. DOI: 10.5194/acp-17-11135-2017. doi: 10.5194/acp-17-11135-2017
[10]	GAUCI V, GOWING D J G, HORNIBROOK E R C, et al. Woody stem methane emission in mature wetland alder trees[J]. Atmospheric Environment, 2010, 44(17):2157-2160. DOI: 10.1016/j.atmosenv.2010.02.034. doi: 10.1016/j.atmosenv.2010.02.034
[11]	WANG Z P, HAN S J, LI H L, et al. Methane production explained largely by water content in the heartwood of living trees in upland forests[J]. Journal of Geophysical Research: Biogeosciences, 2017, 122(10):2479-2489. DOI: 10.1002/2017JG003991. doi: 10.1002/2017JG003991
[12]	PANGALA S R, ENRICH-PRAST A, BASSO L S, et al. Large emissions from floodplain trees close the Amazon methane budget[J]. Nature, 2017, 552(7684):230-234. DOI: 10.1038/nature24639. doi: 10.1038/nature24639
[13]	PANGALA S R, MOORE S, HORNIBROOK E R, et al. Trees are major conduits for methane egress from tropical forested wetlands[J]. New Phytologist, 2013, 197:524-531. DOI: 10.1111/nph.12031. doi: 10.1111/nph.12031
[14]	FENG H L, GUO J H, HAN M H, et al. A review of the mechanisms and controlling factors of methane dynamics in forest ecosystems[J]. Forest Ecology and Management, 2020, 455:117702. DOI: 10.1016/j.foreco.2019.117702. doi: 10.1016/j.foreco.2019.117702
[15]	ZHANG T, ZHU W, MO J, et al. Increased phosphorus availability mitigates the inhibition of nitrogen deposition on CH₄ uptake in an old-growth tropical forest, southern China[J]. Biogeosciences, 2011, 8(9):2805-2813. DOI: 10.5194/bg-8-2805-2011. doi: 10.5194/bg-8-2805-2011
[16]	CARMICHAEL M J, BERNHARDT E S, BRÄUER S L, et al. The role of vegetation in methane flux to the atmosphere: should vegetation be included as a distinct category in the global methane budget?[J]. Biogeochemistry, 2014, 119(1/3):1-24. DOI: 10.1007/s10533-014-9974-1. doi: 10.1007/s10533-014-9974-1
[17]	BRUHN D, MOLLER I M, MIKKELSEN T N, et al. Terrestrial plant methane production and emission[J]. Physiol Plant, 2012, 144(3):201-209. DOI: 10.1111/j.1399-3054.2011.01551.x. doi: 10.1111/j.1399-3054.2011.01551.x
[18]	COVEY K R, MEGONIGAL J P. Methane production and emissions in trees and forests[J]. New Phytol, 2019, 22(1):35-51. DOI: 10.1111/nph.15624. doi: 10.1111/nph.15624
[19]	WANG Z P, GU Q, DENG F D, et al. Methane emissions from the trunks of living trees on upland soils[J]. New Phytol, 2016, 211(2):429-439. DOI: 10.1111/nph.13909. doi: 10.1111/nph.13909
[20]	PITZ S L, MEGONIGAL J P, CHANG C H, et al. Methane fluxes from tree stems and soils along a habitat gradient[J]. Biogeochemistry, 2018, 137(3):307-320. DOI: 10.1007/s10533-017-0400-3. doi: 10.1007/s10533-017-0400-3
[21]	MACHACOVA K, BACK J, VANHATALO A, et al. Pinus sylvestris as a missing source of nitrous oxide and methane in boreal forest[J]. Sci Rep, 2016, 6:23410. DOI: 10.1038/srep23410. doi: 10.1038/srep23410
[22]	PITZ S, MEGONIGAL J P. Temperate forest methane sink diminished by tree emissions[J]. New Phytol, 2017, 214(4):1432-1439. DOI: 10.1111/nph.14559. doi: 10.1111/nph.14559
[23]	MAIER M, MACHACOVA K, LANG F, et al. Combining soil and tree-stem flux measurements and soil gas profiles to understand CH₄ pathways in Fagus sylvatica forests[J]. J Plant Nutr Soil Sci, 2018, 181(1):31-35. DOI: 10.1002/jpln.201600405. doi: 10.1002/jpln.201600405
[24]	YIP D Z, VEACH A M, YANG Z K, et al. Methanogenic archaea dominate mature heartwood habitats of eastern Cottonwood (Populus deltoides)[J]. New Phytologist, 2018, 222(1):115-121. DOI: 10.1111/nph.15346. doi: 10.1111/nph.15346
[25]	BARBA J, BRADFORD M A, BREWER P E, et al. Methane emissions from tree stems: a new frontier in the global carbon cycle[J]. New Phytol, 2018, 2019(222):18-28. DOI: 10.1111/nph.15582. doi: 10.1111/nph.15582
[26]	SCHINK B, WARD J C. Microaerobic and anaerobic bacterial activities involved in formation of wetwood and discoloured wood[J]. International Association of Wood Anatomist Bulletin, 1984, 5(5):105-109. DOI: 10.1163/22941932-90000872. doi: 10.1163/22941932-90000872
[27]	COVEY K R, WOOD S R, WARREN R J, et al. Elevated methane concentrations in trees of an upland forest[J]. Geophy Resea Lett, 2012, 39(15):L15705. DOI: 10.1029/2012gl052361. doi: 10.1029/2012gl052361
[28]	GARTNER B L, MOORE J R, GARDINER B A. Gas in stems: abundance and potential consequences for tree biomechanics[J]. Tree Physiology, 2004, 24(11):1239-1250. DOI: 10.1093/treephys/24.11.1239 doi: 10.1093/treephys/24.11.1239
[29]	DREW M C, HE C J, MORGAN P W. Programmed cell death and aerenchyma formation in roots[J]. Trends Plant Sci, 2000, 5(3):123-127. DOI: 10.1016/S1360-1385(00)01570-3. doi: 10.1016/S1360-1385(00)01570-3
[30]	EVANS D E. Aerenchyma formation[J]. New Phytologist, 2004, 161(1):35-49. DOI: 10.1046/j.1469-8137.2003.00907.x. doi: 10.1046/j.1469-8137.2003.00907.x
[31]	JACKSON M, ARMSTRONG W. Formation of aerenchyma and the processes of plant ventilation in relation to soil flooding and submergence[J]. Plant Biology, 1999, 1(3):274-287. DOI: 10.1111/j.1438-8677.1999.t600253x. doi: 10.1111/j.1438-8677.1999.t600253x
[32]	RICE A L, BUTENHOFF C L, SHEARER M J, et al. Emissions of anaerobically produced methane by trees[J]. Geophy Resea Lett, 2010, 37(3):L03807. DOI: 10.1029/2009gl041565. doi: 10.1029/2009gl041565
[33]	PANGALA S R, HORNIBROOK E R C, GOWING D J, et al. The contribution of trees to ecosystem methane emissions in a temperate forested wetland[J]. Global Change Biology, 2015, 21(7):2642-2654. DOI: 10.1111/gcb.12891. doi: 10.1111/gcb.12891
[34]	ARMSTRONG W. Aeration in higher plants[J]. Advances in botanical research, 1980, 7:225-332. DOI: 10.1016/s0065-2296(08)60089-0. doi: 10.1016/s0065-2296(08)60089-0
[35]	MEGONIGAL J P, GUENTHER A B. Methane emissions from upland forest soils and vegetation[J]. Tree Physiology, 2008, 28(4):491-498. DOI: 10.1093/treephys/28.4.491. doi: 10.1093/treephys/28.4.491
[36]	IKEDA S, KANEKO T, OKUBO T, et al. Development of a bacterial cell enrichment method and its application to the community analysis in soybean stems[J]. Microb Ecol, 2009, 58(4):703-714. DOI: 10.1007/s00248-009-9566-0. doi: 10.1007/s00248-009-9566-0
[37]	CONRAD R. Quantification of methanogenic pathways using stable carbon isotopic signatures: a review and a proposal[J]. Organic Geochemistry, 2005, 36(5):739-752. DOI: 10.1016/j.orggeochem.2004.09.006. doi: 10.1016/j.orggeochem.2004.09.006
[38]	张雨雪, 黄佳芳, 罗敏, 等. 漳江口不同潮滩秋茄树干CH₄传输速率与呼吸速率[J]. 环境科学研究, 2019, 32(5):840-847.
	ZHANG Y X, HUANG J F, LUO M, et al. Rate of methane transport and respiration from the stem of mangrove Kandelia obovata at different part of intertidal zone in Zhangjiang River estuary[J]. Research of Environmental Sciences, 2019, 32(5):840-847. DOI: 10.13198/j.issn.1001-6929.2018.09.14. doi: 10.13198/j.issn.1001-6929.2018.09.14
[39]	WELCH B, GAUCI V, SAYER E J. Tree stem bases are sources of CH₄ and N₂O in a tropical forest on upland soil during the dry to wet season transition[J]. Glob Change Biol, 2019, 25(1):361-372. DOI: 10.1111/gcb.14498. doi: 10.1111/gcb.14498
[40]	SIEGENTHALER A, WELCH B, PANGALA S R, et al. Technical note: semi-rigid chambers for methane gas flux measurements on tree stems[J]. Biogeosciences, 2016, 13(4):1197-1207. DOI: 10.5194/bg-13-1197-2016. doi: 10.5194/bg-13-1197-2016
[41]	TERAZAWA K, YAMADA K, OHNO Y, et al. Spatial and temporal variability in methane emissions from tree stems of Fraxinus mandshurica in a cool-temperate floodplain forest[J]. Biogeochemistry, 2015, 123(3):349-362. DOI: 10.1007/s10533-015-0070-y. doi: 10.1007/s10533-015-0070-y
[42]	TERAZAWA K, ISHIZUKA S, SAKATA T, et al. Methane emissions from stems of Fraxinus mandshurica var. japonica trees in a floodplain forest[J]. Soil Biology and Biochemistry, 2007, 39(10):2689-2692. DOI: 10.1016/j.soilbio.2007.05.013. doi: 10.1016/j.soilbio.2007.05.013
[43]	WARNER D L, VILLARREAL S, MCWILLIAMS K, et al. Carbon dioxide and methane fluxes from tree stems, coarse woody debris, and soils in an upland temperate forest[J]. Ecosystems, 2017, 20(6):1205-1216. DOI: 10.1007/s10021-016-0106-8. doi: 10.1007/s10021-016-0106-8
[44]	BARBA J, POYATOS R, VARGAS R. Automated measurements of greenhouse gases fluxes from tree stems and soils: magnitudes, patterns and drivers[J]. Sci Rep, 2019, 9(1):4005. DOI: 10.1038/s41598-019-39663-8. doi: 10.1038/s41598-019-39663-8
[45]	PLAIN C, NDIAYE F K, BONNAUD P, et al. Impact of vegetation on the methane budget of a temperate forest[J]. New Phytol, 2019, 221(3):1447-1456. DOI: 10.1111/nph.15452. doi: 10.1111/nph.15452
[46]	PULLIAM W. Methane emissions from cypress knees in a southeastern floodplain swamp[J]. Oecologia, 1992, 91(1):126-128. DOI: 10.1007/BF00317250. doi: 10.1007/BF00317250
[47]	JEFFREY L C, REITHMAIER G, SIPPO J Z, et al. Are methane emissions from mangrove stems a cryptic carbon loss pathway? Insights from a catastrophic forest mortality[J]. New Phytol, 2019, 224(1):146-154 DOI: 10.1111/nph.15995. doi: 10.1111/nph.15995
[48]	ZUCCARINI P, ASENSIO D, OGAYA R, et al. Effects of seasonal and decadal warming on soil enzymatic activity in a P-deficient Mediterranean shrubland[J]. Glob Change Biol, 2020, 26(6):3968-3714. DOI: 10.1111/gcb.15077. doi: 10.1111/gcb.15077
[49]	KALACHANIS D, PSARAS G K, Structural changes in primary lenticels of Olea europaea and Cercis siliquastrum during the year[J]. IAWA Journal, 2007, 28(4):445-456. DOI: 10.1163/22941932-90001654. doi: 10.1163/22941932-90001654
[50]	PANGALA S R, GOWING D J, HORNIBROOK E R C, et al. Controls on methane emissions from Alnus glutinosa saplings[J]. New Phytol, 2014, 201(3):887-896. DOI: 10.1111/nph.12561. doi: 10.1111/nph.12561
[51]	CONRAD R, KLOSE M. Anaerobic conversion of carbon dioxide to methane, acetate and propionate on washed rice roots[J]. FEMS Microbiology Ecology, 1999, 30(2):147-155. DOI: 10.1016/S0168-6496(99)00048-3. doi: 10.1016/S0168-6496(99)00048-3
[52]	OBERLE B, COVEY K R, DUNHAM K M, et al. Dissecting the effects of diameter on wood decay emphasizes the importance of cross-stem conductivity in Fraxinus americana[J]. Ecosystems, 2018, 21(1):85-97. DOI: 10.1007/s10021-017-0136-x. doi: 10.1007/s10021-017-0136-x
[53]	GARNET K N, MEGONIGAL J P, LITCHFIEL D C, et al. Physiological control of leaf methane emission from wetland plants[J]. Aquatic Botany, 2005, 81(2):141-155. DOI: 10.1016/j.aquabot.2004.10.003. doi: 10.1016/j.aquabot.2004.10.003
[54]	MEGONIGAL J P, PATRICK W H Jr, FAULKNER S P. Wetland identification in seasonally flooded forest soils: soil morphology and redox dynamics[J]. Soil Science Society of America Journal, 1993, 57(1):140-149. DOI: 10.2136/sssaj1993.03615995005700010027x. doi: 10.2136/sssaj1993.03615995005700010027x
[55]	TOPP E, PATTEY E. Soils as sources and sinks for atmospheric methane[J]. Canadian Journal of Soil Science, 1997, 77(2):167-177. DOI: 10.4141/S96-107. doi: 10.4141/S96-107
[56]	KIRSCHKE S, BOUSQUET P, CIAIS P, et al. Three decades of global methane sources and sinks[J]. Nature Geoscience, 2013, 6(10):813-823. DOI: 10.1038/ngeo1955. doi: 10.1038/ngeo1955
[57]	KEPPLER F, HAMILTON J T, BRASS M, et al. Methane emissions from terrestrial plants under aerobic conditions[J]. Nature, 2006, 439(7073):187-191. DOI: 10.1038/nature04420. doi: 10.1038/nature04420
[58]	SAUNOIS M, BOUSQUET P, POULTER B, et al. The global methane budget 2000-2012[J]. Earth System Science Data, 2016, 8(2):697-751. DOI: 10.5194/essd-8-697-2016. doi: 10.5194/essd-8-697-2016

森林类型 forest type	植物群落 plant community	地理位置 geographical position	树干测量位置/cm emission surface	通量/ (μmol·m^-2·h^-1) flux	文献 Reference
亚热带红树林	秋茄 Kandelia obovata	23°53'N, 117°30'E	20~50	(0.71±0.24)~(91.19 ±16.63)	[38]
温带落叶林	水曲柳 Fraxinus mandshurica	43°22'N, 141°36'E	15 15 70	5.06~81.56 11.00 6.06	[41] [42]
温带落叶林	北美鹅掌楸 Liriodendron tulipifera等	38°51'N, 78°32'W	30~60	(4.3±0.81) ~(35.49±10.91) 1.59±0.88	[20,22]
温带落叶林	欧洲桤木 Alnus glutinosa	52°0'N, 0°28'W	20~50	(6.71±0.83)~ (9.79 ±1.29)	[33]
热带雨林	8种被子植物	2°20'S, 113°55'E	20~130	(1.06±0.9)~(11.56 ±0.44)	[13]
热带雨林	多种被子植物	2°20'S~3°20'S, 54°55'~61°0'E	15~140	(1.00±2.50)~(16 937.50± 6 812.50)	[12]
温带落叶林	北美鹅掌楸 L. tulipifera等	39°42'N, 75°50'W	130	0.40±0.18	[43]
暖温带森林	山杨 Populus davidiana等	39°58'N, 115°26'E	130	12.63~20.73, 5.33~6.44	[11,19]
温带森林	欧洲水青冈 Fagus sylvatica	48°1'N,7°57'E	120	1.87±3.31	[23]
寒温带森林	欧洲赤松 Pinus sylvestris	61°51'N, 24°17'E	20	0.000 31~0.006 3	[21]
温带森林	欧洲桤木 Alnus glutinosa	52°00'N, 00°28'W	30	0.26~6.31	[10]
温带森林	苦味山核桃 Carya cordiformis	39°5'N, 75°26'W	75 150	0.46±0.03 0.28±0.02	[44]
温带森林	无梗花栎 Quercus petraea	48°29'N, 6°41'E	25~45	0.032±0.022	[45]
亚热带森林	落羽杉 Taxodium distichum	32°08'N, 81°25'W	<30, >300	2.34±0.78	[46]
热带红树林	白骨壤 Avicenna marina	17°27'S, 140°48'E	10~170	0.013~ 21.00, -3.77 ~168.15(死亡株)	[47]
温带森林湿地	多种被子植物(死亡株)	35°54'N, 76°09'W	10-100	吸收-37.5±18.75,25.0±6.25	[48]

树干甲烷的研究进展

Advances in research on methane from tree stems

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