A review of effects of fire disturbance on understory vegetation in boreal coniferous forest

doi:10.3724/SP.J.1258.2013.00049

Abstract

Abstract:

Understory vegetation in boreal forests is the most diverse and least understood component of boreal plant com- munities. In addition, the aboveground net primary productivity of understory vegetation is almost comparable to that of the trees, and the biomass turns over more rapidly than does that of the trees. Fire disturbance is an important landscape process, driving understory structure and function in boreal forests. We review recent research about how fire, interacting with topography and overstory canopy, affects environmental resources (e.g., light and soil nutrients) and understory vegetation. Recent studies have demonstrated that understory vegetation in boreal forests can also influence post-fire tree seedling regeneration, rate of recovery and successional pathways. It can also affect the quantity and heterogeneity of environmental resources by influencing biogeochemical processes such as decomposition and nutrient flow. Understanding understory vegetation dynamics after fire, especially during early succession, is very important for biodiversity conservation and management of boreal forest.

Key words: boreal coniferous forest, environmental resources, fire disturbance, species diversity, understory vegetation

YANG Jian,KONG Jian-Jian,LIU Bo. A review of effects of fire disturbance on understory vegetation in boreal coniferous forest[J]. Chin J Plant Ecol, 2013, 37(5): 474-480.

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URL: https://www.plant-ecology.com/EN/10.3724/SP.J.1258.2013.00049

https://www.plant-ecology.com/EN/Y2013/V37/I5/474

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References 49

[1]	Alaback PB ( 1982). Dynamics of understory biomass in Sikta spruce-western hemlock forests of southeast Alaska. Ecology, 63, 1932-1948.
[2]	Barbier S, Gosselin F, Balandier P ( 2008). Influence of tree species on understory vegetation diversity and mechanisms involved—A critical review for temperate and boreal forests. Forest Ecology and Management, 254, 1-15.
[3]	Bartels SF, Chen HYH ( 2010). Is understory plant species diversity driven by resource quantity or resource heterogeneity? Ecology, 91, 1931-1938.
[4]	Barton AM ( 1994). Gradient analysis of relationships among fire, environment, and vegetation in a southwestern USA mountain range. Bulletin of the Torrey Botanical Club, 121, 251-265.
[5]	Bergeron Y ( 2000). Species and stand dynamics in the mixed woods of Quebec’s southern boreal forest. Ecology, 81, 1500-1516.
[6]	Bergeron Y, Dubuc M ( 1989). Succession in the southern part of the Canadian boreal forest. Vegetation, 79, 51-63.
[7]	Bohlen PJ, Groffman PM, Driscoll CT, Fahey TJ, Siccama TG ( 2001). Plant-soil-microbial interactions in a northern hardwood forest. Ecology, 82, 965-978.
[8]	Brais S, David P, Ouimet R ( 2000). Impacts of wild fire severity and salvage harvesting on the nutrient balance of jack pine and black spruce boreal stands. Forest Ecology and Management, 137, 231-243.
[9]	Brassard BW, Chen HYH ( 2006). Stand structural dynamics of the North American boreal forests. Critical Review in Plant Sciences, 24, 115-137.
[10]	Brassard BW, Chen HYH, Wang JR, Duinker PN ( 2008). Effects of time since stand-replacing fire and overstory composition on live-tree structural diversity in the boreal forest of central Canada. Canadian Journal of Forest Research, 38, 52-62.
[11]	Breshears DD, Rich PM, Barnes FJ, Campbell K ( 1997). Overstory-imposed heterogeneity in solar radiation and soil moisture in a semiarid woodland. Ecological Applications, 7, 1201-1215.
[12]	Cai WH, Yang J, Liu ZH, Hu YM, Liu SJ, Jing GZ, Zhao ZF ( 2012). Controls of post-fire tree recruitment in Great Xing’an Mountains in Heilongjiang Province. Acta Ecologica Sinica, 32, 3303-3312. (in Chinese with English abstract)
	[ 蔡文华, 杨健, 刘志华, 胡远满, 柳生吉, 荆国志, 赵增福 ( 2012). 黑龙江省大兴安岭林区火烧迹地森林更新及其影响因子. 生态学报, 32, 3303-3312.]
[13]	Cavard X, Bergeron Y, Chen HYH, Pare D ( 2011). Effect of forest canopy composition on soil nutrients and dynamics of the understorey: mixed canopies serve neither vascular nor bryophyte strata. Journal of Vegetation Science, 22, 1105-1119.
[14]	Cote L, Brown S, David P, Fyles JW, Bauhus J ( 2000). Dynamics of carbon and nitrogen mineralization in relation to stand type, stand age and soil texture in the boreal mixedwood. Soil Biology and Biochemistry, 32, 1079-1090.
[15]	Driscoll KG, Arocena JM, Massicotte HB ( 1999). Post-fire soil nitrogen content and vegetation composition in sub-boreal spruce forests of British Columbia’s central interior, Canada. Forest Ecology and Management, 121, 227-237.
[16]	Flanagan LB, Cleve KV ( 1983). Nutrient cycling in relation to decomposition and organic-matter quality in taiga ecosystems. Canadian Journal of Forest Research, 13, 795-817.
[17]	Gillman LN, Wright SD ( 2006). The influence of productivity on the species richness of plants: a critical assessment. Ecology, 87, 1234-1243. URL PMID
[18]	Gower S, Krankina O, Olson R, Apps M, Linder S, Wang C ( 2001). Net primary production and carbon allocation patterns of boreal forest ecosystems. Ecological Applications, 11, 1395-1411.
[19]	Grandpré LD, Gagnon D, Bergeron Y ( 1993). Changes in the understory of Canadian southern boreal forest after fire. Journal of Vegetation Science, 4, 803-810.
[20]	Greene DF, Zasada JC, Sirois L, Kneeshaw D, Morin H, Charron I, Simard MJ ( 1999). A review of the regeneration dynamics of North American boreal forest tree species. Canadian of Journal Forest Research, 29, 824-839.
[21]	Gross KL, Willig MR, Gough L, Inouye R, Cox SB ( 2000). Patterns of species density and productivity at different spatial scales in herbaceous plant communities. Oikos, 89, 417-427.
[22]	Gu HY, Jin JB, Chen XW ( 2010). The long term impacts on chemical properties of Larix gmelini forest on the northern slope of Greater Hinggan Mountains from a forest fire of varying fire intensity. Journal of Natural Resources, 25, 1114-1121. (in Chinese with English abstract)
	[ 谷会岩, 金靖博, 陈祥伟 ( 2010). 不同火烧强度林火对大兴安岭北坡兴安落叶松林土壤化学性质的长期影响. 自然资源学报, 25, 1114-1121.]
[23]	Hart SA, Chen HYH ( 2006). Understory vegetation dynamics of North American boreal forests. Critical Reviews in Plant Sciences, 25, 381-397.
[24]	Hart SA, Chen HYH ( 2008). Fire, logging, and overstory affect understory abundance, diversity, and composition in boreal forest. Ecological Monographs, 78, 123-140.
[25]	Hu HQ, Liu Y, Sun L ( 2008). Effect of fire on soil hydro- physical properties under different types of forest land. Journal of Soil and Water Conservation, 22, 162-165. (in Chinese with English abstract)
	[ 胡海清, 刘洋, 孙龙 ( 2008). 火烧对不同林型下森林土壤水分物理性质的影响. 水土保持学报, 22, 162-165.]
[26]	Huston M ( 1979). A general hypothesis of species diversity. The American Naturalist, 113, 81-101.
[27]	Kassen R, Buckling A, Bell G, Rainey PB ( 2000). Diversity peaks at intermediate productivity in a laboratory microcosm. Nature, 406, 508-512.
[28]	Keeley JE, Lubin D, Fotheringham CJ ( 2003). Fire and grazing impacts on plant diversity and alien plant invasions in the southern Sierra Nevada. Ecological Applications, 13, 1355-1374.
[29]	Liu ZH, Yang J, Chang Y, Weisberg PJ, He HS ( 2012). Spatial patterns and drivers of fire occurrence and its future trend under climate change in a boreal forest of Northeast China. Global Change Biology, 18, 2041-2056.
[30]	Maclean DA, Wein RW ( 1977). Changes in understory vegetation with increasing stand age in new brunswick forests: species composition, cover, biomass, and nutrients. Canadian Journal of Botany, 55, 2818-2831.
[31]	Messier C, Parent S, Bergeron Y ( 1998). Effects of overstory and understory vegetation on the understory light environment in mixed boreal forests. Journal of Vegetable Science, 9, 511-520.
[32]	Neary DG, Klopatek CC, DeBano LF, Ffolliott PF ( 1999). Fire effects on belowground sustainability: a review and synthesis. Forest Ecology and Management, 122, 51-71.
[33]	Nilsson MC, Wardle DA ( 2005). Understory vegetation as a forest ecosystem driver: evidence from the northern Swedish boreal forest. Frontiers in Ecology and the Environment, 3, 421-428.
[34]	Pan Y, Birdsey RA, Fang J, Houghton R, Kauppi PE, Kurz WA, Phillips OL, Shvidenko A, Lewis SL, Canadell JG, Ciais P, Jackson RB, Pacala SW, McGuire AD, Piao S, Rautiainen A, Sitch S, Hayes D ( 2011). A large and persistent carbon sink in the world’s forests. Science, 333, 988-993. DOI URL PMID
[35]	Purdon M, Brais S, Bergeron Y ( 2004). Initial response of understorey vegetation to fire severity and salvage-logging in the southern boreal forest of Quebec. Applied Vegetation Science, 7, 49-60.
[36]	Qian H, Klinka K, Økland RH, Krestov P, Kayahara GJ ( 2003). Understorey vegetation in boreal Picea mariana and Populus tremuloides stands in British Columbia. Journal of Vegetation Science, 14, 173-184.
[37]	Reich PB, Frelich LE, Voldseth RA, Bakken P, Adair EC ( 2012). Understorey diversity in southern boreal forests is regulated by productivity and its indirect impacts on resource availability and heterogeneity. Journal of Ecology, 100, 539-545.
[38]	Roberts MR ( 2004). Response of the herbaceous layer to natural disturbance in North American forests. Canadian Journal of Botany, 82, 1273-1283.
[39]	Running SW ( 2006). Is global warming causing more, larger wildfires? Science, 313, 927-928.
[40]	Shu LF, Wang MY, Li ZQ ( 2004). Dwarf Siberian pine forest fire environment in Daxing’an Mountains. Journal of Mountain Science, 22, 36-39. (in Chinese with English abstract)
	[ 舒立福, 王明玉, 李忠琦 ( 2004). 大兴安岭山地偃松林火环境研究. 山地学报, 22, 36-39.]
[41]	Smithwick EAH, Turner MG, Mack MC, Chapin FSI ( 2005). Postfire soil N cycling in northern conifer forests affected by severe, stand-replacing wildfires. Ecosystems, 8, 163-181.
[42]	Stevens MHH, Carson WP ( 2002). Resource quantity, not resource heterogeneity, maintains plant diversity. Ecology Letters, 5, 420-426.
[43]	Sun JB, Zhang HL, Hu HQ ( 2009). Effect of fire disturbance intensity on species composition and species diversity of Larix gmelinii forest in Daxing’anling Mountains. Forest Engineering, 25, 1-5. (in Chinese with English abstract)
	[ 孙家宝, 张海林, 胡海清 ( 2009). 火干扰强度对兴安落叶松林物种组成及多样性的影响. 森林工程, 25, 1-5.]
[44]	Timoney KP ( 2001). Types and attributes of old-growth forests in Alberta, Canada. Natural Areas Journal, 21, 282-300.
[45]	Waide RB, Willig MR, Steiner CF, Mittelbach GG, Gough L, Dodson SI, Juday GP, Parmenter R ( 1999). The relationship between productivity and species richness. Annual Review of Ecological and Systems, 30, 257-300.
[46]	Wang CK, Gower ST, Wang YH, Zhao HX, Yan P, Lamberty BB ( 2001). The influence of fire on carbon distribution and net primary production of boreal Larix gmelinii forests in northeastern China. Global Change Biology, 7, 719-730.
[47]	Wang XG, Li XZ, He HS ( 2004). Postfire succession of larch forest on the northern slope of Daxinganling. Chinese Journal of Ecology, 23, 35-41. (in Chinese with English abstract)
	[ 王绪高, 李秀珍, 贺红士 ( 2004). 大兴安岭北坡落叶松林火后植被演替过程研究. 生态学杂志, 23, 35-41.]
[48]	Yu B, Wu JSGL, Wang BT ( 2009). Research on characteristics of vegetation change in gaps of Larix gmelinii natural forest in Daxinganling. Forest Research, 22, 213-218. (in Chinese with English abstract)
	[ 玉宝, 乌吉斯古楞, 王百田 ( 2009). 大兴安岭兴安落叶松天然林林隙地被物变化特征研究. 林业科学研究, 22, 213-218.]
[49]	Zhang YH, Qin BX, Sun ML, Zhou ZQ ( 2012). Impact of forest fire on understory vegetation and soil in typical forest types of Daxing’an Mountains, northeastern China. Journal of Beijing Forestry University, 34(2), 7-13. (in Chinese with English abstract)
	[ 张玉红, 覃炳醒, 孙铭隆, 周志强 ( 2012). 林火对大兴安岭典型林型林下植被与土壤的影响. 北京林业大学学报, 34(2), 7-13.]