[1]蔡苗,卢杰.树轮密度的测量方法及其对气候变化的响应研究进展[J].黑龙江农业科学,2023,(05):107-112.[doi:10.11942/j.issn1002-2767.2023.05.0107]
 CAI Miao,LU Jie.Research Progress on Measurement Methods of Tree-Ring Density and Its Response to Climate Change[J].HEILONGJIANG AGRICULTURAL SCIENCES,2023,(05):107-112.[doi:10.11942/j.issn1002-2767.2023.05.0107]
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树轮密度的测量方法及其对气候变化的响应研究进展

参考文献/References:

[1]柴正礼,姚孟春,张小全,等.树木年轮对气候变化响应研究进展[J].安徽农业科学,2010,38(2):959-961.[2]NATH C D,MUNOZ F,PLISSIER R,et al.Growth rings in tropical trees:role of functional traits,environment,and phylogeny[J].Trees,2016,30(6):2153-2175.[3]BNTGEN U,MYGLAN V S,LJUNGQVIST F C,et al.Cooling and societal change during the Late Antique Little Ice Age from 536 to around 660 AD[J].Nature Geoscience,2016,9(3):231-236.[4]陈兰,李书恒,侯丽,等.基于Vaganov-Shashkin模型的太白红杉径向生长对气候要素的响应[J].应用生态学报,2017,28(8):2470-2480.[5]BABST F,BODESHEIM P,CHARNEY N,et al.When tree rings go global:challenges and opportunities for retro- and prospective insight[J].Quaternary Science Reviews,2018,197:1-20.[6]FRITTS H C,BLASING T J,HAYDEN B P,etal.Multivariate techniques for specifying tree-growth and climate relationships and for reconstructing anomalies in paleoclimate[J].Journal of Applied Meteorology and Climatology,1971:845-864.[7]张志华,李骥.用树轮密度及宽度资料重建新疆吉木萨尔县的季节降水和最高温度[J].气象学报,1998(1):78-87.[8]刘禹,吴祥定,安芷生,等.树轮密度、稳定C同位素对过去近100 a陕西黄陵季节气温与降水的恢复[J].中国科学(D辑:地球科学),1997(3):271-276.[9]KIRDYANOV A V,TREYDTE K S,NIKOLAEV A,et al.Climate signals in tree-ring width,density and δ 13C from larches in Eastern Siberia(Russia)[J].Chemical Geology,2008,252(1-2):31-41.[10]WIMMER R,GRABNER M.A comparison of tree-ring features in Picea abies as correlated with climate[J].Iawa Journal,2000,21(4):403-416.[11]YINH,LIU H,LINDERHOLM H W,et al.Treering density-based warm-season temperature reconstruction since AD 1610 in the eastern Tibetan Plateau[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2015,426:112-120.[12]CAMARERO J J,FERNNDEZ-PEREZ L,KIRDYANOV A V,et al.Minimum wood density of conifers portrays changes in early season precipitation at dry and cold Eurasian regions[J].Trees,2017,31(5):1423-1437.[13]魏本勇,方修琦.树轮气候学中树木年轮密度分析方法的研究进展[J].古地理学报,2008(2):193-202.[14]POLGE H.tablissement des courbes de variation de la densité du bois par exploration densitométrique de radiographies d′échantillons prélevés à la tarière sur des arbres vivants:applications dans les domaines Technologique et Physiologique[C]//Annales des sciences forestières.EDP Sciences,1966,23(1):I-206.[15]MANNES D,LEHMANN E,CHERUBINI P,et al.Neutron imaging versus standard X-ray densitometry as method to measure tree-ring wood density[J].Trees,2007,21(6):605-612.[16]KIRDYANOV A V,VAGANOV E A,HUGHES M K.Separating the climatic signal from tree-ring width and maximum latewood density records[J].Trees,2007,21(1):37-44.[17]BERGSERGS L,NEPVEU G,FRANC A.Effects of ecological factors on radial growth and wood density components of sessile oak(Quercus petraea Liebl.)in Northern France[J].Forest Ecology and Management,2008,255(3-4):567-579.[18]陈峰,袁玉江,王丽丽,等.塔城西伯利亚落叶松树轮密度的气候响应研究[J].干旱区资源与环境,2011,25(6):182-187.[19]杨柳,秦春,李刚.中国祁连山西段青海云杉树轮密度记录的气候信号[J].应用生态学报,2021,32(10):3636-3642.[20]张辉,张芸,胡亚楠,等.气候变暖背景下杉木年轮密度对气候因子的响应[J].生态学报,2021,41(4):1551-1563.[21]喻树龙.新疆伊犁巩乃斯地区树木年轮密度对气候的响应及气候重建[D].乌鲁木齐:新疆师范大学,2011.[22]SONG H,MEI R,LIU Y,et al.Maximum July-September temperatures derived from tree-ring densities on the western Loess Plateau,China[J].International Journal of Climatology,2021,41(2):779-790.[23]SCHINKER M G,HANSEN N,SPIECKER H.High-frequency densitometry-a new method for the rapid evaluation of wood density variations[J].IAWA Journal,2003,24(3):231-239.[24]侯迎,王乃昂,张学敏,等.高频光密度测量法在崆峒山树轮年表建立中的应用[J].干旱区地理,2010,33(2):236-242.[25]DIERICK M,VAN LOO D,MASSCHAELE B,et al.Recent micro-CT scanner developments at UGCT[J].Nuclear Instruments and Methods in Physics Research Section B:Beam Interactions with Materials and Atoms,2014,324:35-40.[26]BJRKLUND J,VON ARX G,NIEVERGELT D,et al.Scientific merits and analytical challenges of tree-ring densitometry[J].Reviews of Geophysics,2019,57(4):1224-1264.[27]de GROOTE S R E,VANHELLEMONT M,BAETEN L,et al.Competition,tree age and size drive the productivity of mixed forests of pedunculate oak,beech and red oak[J].Forest Ecology and Management,2018,430:609-617.[28]VANHELLEMONT M,SOUSA-SILVA R,MAES S L,et al.Distinct growth responses to drought for oak and beech in temperate mixed forests[J].Science ofthe Total Environment,2019,650:3017-3026.[29]姚建峰,符利勇,宋新宇,等.微钻阻力法测量早晚材密度的可行性试验[J].林业工程学报,2022,7(5):66-73.[30]陈峰,袁玉江,魏文寿,等.用于气候分析的树木年轮密度资料获取方法与质量控制[J].沙漠与绿洲气象,2012,6(1):62-67.[31]孙毓,王丽丽,陈津,等.利用兴安落叶松树轮最大晚材密度重建大兴安岭北部5-8月气温变化[J].科学通报,2012,57(19):1791-1799.[32]杨银科,黄强,刘禹,等.以树木年轮密度资料重建鄂尔多斯中部地区6至10月降水量的变化[J].西北农林科技大学学报(自然科学版),2013,41(8):96-102,109.[33]杨银科,黄强,刘禹,等.云杉树轮生长密度对气候要素的响应分析[J].西安理工大学学报,2012,28(4):432-438.[34]HOUSSET J M,NADEAU S,ISABEL N,et al.Tree rings provide a new class of phenotypes for genetic associations that foster insights into adaptation of conifers to climate change[J].New Phytologist,2018,218(2):630-645.[35]陈峰,王慧琴,袁玉江,等.树轮最大密度记录的吉尔吉斯斯坦天山山区公元1650年以来的7-8月温度变化[J].沙漠与绿洲气象,2014,8(4):1-7.[36]SHEN Y,TAKATA K,KUDO K,et al.Effects of climate on the tree ring density and weight of Betula ermanii in a cool temperate forest in central Japan[J].Trees,2022:1-9.[37]石仁娜·加汗.喀什河流域不同海拔雪岭云杉树轮气候响应特征研究[D].乌鲁木齐:新疆大学,2021.[38]王丽丽,邵雪梅,黄磊,等.黑龙江漠河兴安落叶松与樟子松树轮生长特性及其对气候的响应[J].植物生态学报,2005(3):280-285.[39]徐金梅,吕建雄,鲍甫成,等.祁连山青海云杉木材密度对气候变化的响应[J].北京林业大学学报,2011,33(5):115-121.[40]喻树龙,袁玉江,陈峰,等.巩乃斯河源树木年轮密度年表特征分析[J].沙漠与绿洲气象,2010,4(4):6-11.[41]WU P,WANG L,SHAO X.Reconstruction of)summer temperature variation from maximum density of alpine pine during 1917-2002 for west Sichuan Plateau,China[J].Journal of Geographical Sciences,2008,18(2):201-210.[42]邓国富,李明启.树轮密度对气候的响应及重建研究进展[J].地理科学进展,2021,40(2):343-356.[43]RITA A,CHERUBINI P,LEONARDI S,et al.Functional adjustments of xylem anatomy to climatic variability:insights from long-term Ilex aquifolium tree-ring series[J].Tree Physiology,2015,35(8):817-828.[44]BOURIAUD O,BRDA N,DUPOUEY J L,et al.Is ring width a reliable proxy for stem-biomass increment? A case study in European beech[J].Canadian Journal of Forest Research,2005,35(12):2920-2933.[45]刘可祥,张同文,张瑞波,等.不同树高处树轮密度变化特征及其对气候的响应[J].应用生态学报,2021,32(2):503-512.[46]孙毓,王丽丽,陈津.长白落叶松树轮生长对气候变化的响应以及对夏季气温的重建[J].地球环境学报,2012,3(3):889-899.[47]HARTL C,SCHNEIDER L,RIECHELMANN D F C,et al.The temperature sensitivity along elevational gradients is more stable in maximum latewood density than tree-ring width[J].Dendrochronologia,2022,73:125958.[48]KLIPPEL〖KG(0.3mm L,BNTGEN U,KONTER O,et al.〖KG)Climate sensitivity of high- and low-elevation Larix decidua MXD 〖JP4chronologies from the Tatra Mountains[J].Dendrochronologia,2020,60:125674.[49]KONTER O,BNTGEN U,CARRER M,et al.Climate signal age effects in boreal tree-rings:Lessons to be learned for paleoclimatic reconstructions[J].Quaternary Science Reviews,2016,142:164-172.[50]DAY M E,GREENWOOD M S,DIAZ-SALA C.Age- and size-related trends in woody plant shoot development:regulatory pathways and evidence for genetic control[J].Tree Physiology,2002,22(8):507-513.[51]ROSSI(0.7mmS,DESLAURIERS A,ANFODILLO T,et)al.Age-dependent xylogenesis in timberline conifers[J].New Phytologist,2008,177(1):199-208.[52]CARRER〖KG(0.7mm M,URNINATI C.Age-dependent)tree-ring growth responses to climate in Larix decidua and Pinus cembra[J].Ecology,2004,85(3):730-740.[53]LEONELLI(0.5mmG,PELFINI M,BATTIPAGLIA G,et)al.Site-aspect influence on climate sensitivity over time of a high-altitude Pinus cembra tree-ring network[J].Climatic Change,2009,96(1):185-201.[54]ZALLONI(0.2mmE,BATTIPAGLIA G,CHERUBINI P,et)al.Site conditions influence the climate signal of intra-annual density fluctuations in tree rings of Q.ilex L[J].Annals of Forest Science,2018,75(3):1-12.

备注/Memo

收稿日期:2022-12-15

基金项目:科技部国家野外科学研究观测站(生态系统)运行补助项目(2021-2025)。
第一作者:蔡苗(1998-),女,硕士研究生,从事森林生态学研究。E-mail:c187811411612@163.com。
通信作者:卢杰(1973-),男,博士,教授,博导,从事森林生态学的研究与教学工作。E-mail:tibetlj@163.com。

更新日期/Last Update: 2023-05-10