树木年轮年内高分辨率稳定同位素记录:方法、进展和展望

doi:10.13287/j.1001-9332.202110.024

应用生态学报 ›› 2021, Vol. 32 ›› Issue (10): 3743-3752.doi: 10.13287/j.1001-9332.202110.024

树木年轮年内高分辨率稳定同位素记录:方法、进展和展望

李瑶, 曾小敏^*, 倪萍, 王文超, 刘晓宏

陕西师范大学地理科学与旅游学院, 西安 710119

收稿日期:2021-03-22 修回日期:2021-07-26 出版日期:2021-10-15 发布日期:2022-04-15
通讯作者: * E-mail: zengxm1021@snnu.edu.cn
作者简介:李瑶, 女, 2000年生, 硕士研究生。主要从事高分辨率树轮稳定同位素研究。E-mail: 1095072174@qq.com
基金资助:
国家自然科学基金项目(41807431,41971104)、陕西省自然科学基金项目(2019JQ-325)和中央高校基础研究经费项目(GK202103140,GK202007012)

Intra-annual high resolution stable isotope records of tree ring: Methods, progress and prospects

LI Yao, ZENG Xiao-min^*, NI Ping, WANG Wen-chao, LIU Xiao-hong

School of Geography and Tourism, Shaanxi Normal University, Xi'an 710119, China

Received:2021-03-22 Revised:2021-07-26 Online:2021-10-15 Published:2022-04-15
Contact: * E-mail: zengxm1021@snnu.edu.cn
Supported by:
National Natural Science Foundation of China (41807431, 41971104), the National Science Foundation of Shaanxi Province (2019JQ-325), and the Fundamental Research Funds for the Central Universities (GK202103140, GK202007012).

摘要/Abstract

摘要： 树轮稳定同位素比率能有效地记录树木生长过程中气候环境变化信息及树木的生理响应机制。年内高分辨率树轮稳定同位素比率则能够提供更为详细的气候环境信息,揭示树木对季节尺度气候环境变化的生理生态响应机制,在古气候和全球变化生态学研究方面显示出巨大的潜力。本文收集了1990年以来发表的树轮年内高分辨率稳定同位素比率研究论文,从样品剥离方法、α-纤维素化学提取方法以及应用等方面综述了其研究进展,展望了年内高分辨率树轮稳定同位素记录研究的潜力和未来发展方向。

关键词: 树木年轮, 稳定同位素比率, 年内变化, 气候信号

Abstract: Stable isotope ratios of tree ring can effectively record climate and environmental changes during tree growth and the physiological responses of trees to such changes. Intra-annual high resolution stable isotope ratios of tree ring can provide more detailed climatic and environmental information, reveal the physiological and ecological response mechanism of trees to seasonal climatic variation, and thus with great potential in the study of paleoclimate and global change ecology. Based on the intra-annual high resolution stable isotope ratios related literature since 1990, we reviewed the research progress of intra-annual high resolution tree ring stable isotope records in the aspects of sample stripping method, chemical extraction method of α-cellulose and application, and further proposed the potential and future development direction of intra-annual high resolution tree ring stable isotope records.

Key words: tree ring, stable isotope ratio, intra-annual variation, climatic signal

李瑶, 曾小敏, 倪萍, 王文超, 刘晓宏. 树木年轮年内高分辨率稳定同位素记录:方法、进展和展望[J]. 应用生态学报, 2021, 32(10): 3743-3752.

LI Yao, ZENG Xiao-min, NI Ping, WANG Wen-chao, LIU Xiao-hong. Intra-annual high resolution stable isotope records of tree ring: Methods, progress and prospects[J]. Chinese Journal of Applied Ecology, 2021, 32(10): 3743-3752.

参考文献

[1] 刘晓宏, 徐国保, 曾小敏, 等. 树轮稳定同位素记录: 进展、问题及展望. 第四纪研究, 2015, 35(5): 1245-1260 [Liu X-H, Xu G-B, Zeng X-M, et al. Tree ring stable isotope records: Progress, problems and prospects. Quaternary Research, 2015, 35(5): 1245-1260]
[2] 曾小敏. 亚洲夏季风北边缘带树轮宽度和高分辨率δ¹⁸O和δ¹³C气候意义研究. 博士论文. 兰州: 中国科学院西北生态环境资源研究院, 2017 [Zeng X-M. Study on the Climatic Significance of Tree-ring Width and High-resolution δ¹⁸O and δ¹³C in the Northern Boundary Belt of Asian Summer Monsoon. PhD Thesis. Lanzhou: Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, 2017]
[3] Roden JS, Johnstone JA, Dawson TE. Intra-annual varia-tion in the stable oxygen and carbon isotope ratios of cellulose in tree rings of coast redwood (Sequoia sempervirens). The Holocene, 2009, 19: 189-197
[4] Rinne KT, Saurer M, Kirdyanov AV. The relationship between needle sugar carbon isotope ratios and tree rings of larch in Siberia. Tree Physiology, 2015, 35: 1192-1205
[5] Xu C, Zheng H, Nakatsuka T, et al. Inter- and intra-annual tree-ring cellulose oxygen isotope variability in response to precipitation in Southeast China. Trees, 2016, 30: 785-794
[6] Schubert BA, Jahren AH. Seasonal temperature and precipitation recorded in the intra-annual oxygen isotope pattern of meteoric water and tree-ring cellulose. Quaternary Science Reviews, 2015, 125: 1-14
[7] Managave SR, Sheshshayee MS, Bhattacharyya A, et al. Intra-annual variations of teak cellulose δ¹⁸O in Kerala, India: Implications to the reconstruction of past summer and winter monsoon rains. Climate Dynamics, 2011, 37: 555-567
[8] Szymczak S, Bräuning A, Häusser M, et al. The relationship between climate and the intra-annual oxygen isotope patterns from pine trees: A case study along an elevation gradient on Corsica, France. Annals of Forest Science, 2019, 76, doi: 10.1007/s13595-019-0860-9
[9] Szymczak S, Barth J, Bendix J, et al. First indications of seasonal and spatial variations of water sources in pine trees along an elevation gradient in a Mediterranean ecosystem derived from δ¹⁸O. Chemical Geology, 2020, 549: 119695, doi: 10.1016/j.chemgeo.2020.119695
[10] Managave SR , Sheshshayee MS, Borgaonkar HP, et al. Past break-monsoon conditions detectable by high resolution intra-annual δ¹⁸O analysis of teak rings. Geophysical Research Letters, 2010, 37: L05702, doi:10.1029/2009GL041172
[11] Leavitt SW. Prospects for reconstruction of seasonal environment from tree-ring δ¹³C baseline findings from the Great Lakes area, USA. Chemical Geology, 2002, 192: 47-58
[12] Leavitt SW. Regional expression of the 1988 U.S. Midwest drought in seasonal δ¹³C of tree rings. Journal of Geophysical Research: Atmospheres, 2007, 112: D06107, doi: 10.1029/2006JD007081
[13] Schubert BA, Timmermann A. Reconstruction of seaso-nal precipitation in Hawai'i using high-resolution carbon isotope measurements across tree rings. Chemical Geo-logy, 2015, 417: 273-278
[14] Schubert BA, Jahren AH. Quantifying seasonal precipitation using high-resolution carbon isotope analyses in evergreen wood. Geochimica et Cosmochimica Acta, 2011, 75: 7291-7303
[15] Jahren AH, Sternberg L. Annual patterns within tree rings of the Arctic middle Eocene (ca. 45 Ma): Isotopic signatures of precipitation, relative humidity, and deci-duousness. Geology, 2008, 36: 99-102
[16] Reimchen TE, Arbellay E. Intra-annual variability in isotopic and total nitrogen in tree rings of old growth Sitka spruce from coastal British Columbia. Botany, 2018, 96: 851-857
[17] Ohashi S, Durgante FM, Kagawa A, et al. Seasonal varia-tions in the stable oxygen isotope ratio of wood cellulose reveal annual rings of trees in a Central Amazon terra firme forest. Oecologia, 2016, 180: 685-696
[18] Pons TL, Helle G. Identification of anatomically non-distinct annual rings in tropical trees using stable isotopes. Trees, 2010, 25: 83-93
[19] Evans MN, Schrag DP. A stable isotope-based approach to tropical dendroclimatology. Geochimica et Cosmochimica Acta, 2004, 68: 3295-3305
[20] Helle G, Schleser GH. Beyond CO₂-fixation by Rubisco: An interpretation of ¹³C/¹²C variations in tree rings from novel intra-seasonal studies on broad-leaf trees. Plant, Cell & Environment, 2004, 27: 367-380
[21] Kagawa A, Sugimoto A, Maximov TC. ¹³CO₂ pulse-labelling of photoassimilates reveals carbon allocation within and between tree rings. Plant, Cell & Environment, 2006, 29: 1571-1584
[22] Eglin T, Francois C, Michelot A, et al. Linking intra-seasonal variations in climate and tree-ring δ¹³C: A functional modelling approach. Ecological Modelling, 2010, 221: 1779-1797
[23] He M, Bruning A, Rossi S, et al. No evidence for carryover effect in tree rings based on a pulse-labelling experiment on Juniperus communis in South Germany. Trees, 2020, 35: 493-502
[24] Krepkowski J, Gebrekirstos A, Shibistova O, et al. Stable carbon isotope labeling reveals different carry-over effects between functional types of tropical trees in an Ethiopian mountain forest. New Phytologist, 2013, 199: 431-440
[25] Offermann C, Ferrio JP, Holst J, et al. The long way down: Are carbon and oxygen isotope signals in the tree ring uncoupled from canopy physiological processes? Tree Physiology, 2011, 31: 1088-1102
[26] Treydte K, Boda S, Pannatier EG, et al. Seasonal transfer of oxygen isotopes from precipitation and soil to the tree ring: Source water versus needle water enrichment. New Phytologist, 2014, 202: 772-783
[27] Evans MN. Toward forward modeling for paleoclimatic proxy signal calibration: A case study with oxygen isotopic composition of tropical woods. Geochemistry, Geophysics, Geosystems, 2007, 8: Q07008, doi: 10.1029/2006GC001406
[28] Anchukaitis KJ, Evans MN, Wheelwright NT, et al. Stable isotope chronology and climate signal calibration in neotropical montane cloud forest trees. Journal of Geophysical Research, 2008, 113: G03030, doi:10.1029/2007JG000613
[29] Berkelhammer M, Stott LD. Modeled and observed intra-ring δ¹⁸O cycles within late Holocene Bristlecone Pine tree samples. Chemical Geology, 2009, 264: 13-23
[30] Zeng X, Liu X, Evans MN, et al. Seasonal incursion of Indian Monsoon humidity and precipitation into the southeastern Qinghai-Tibetan Plateau inferred from tree ring δ¹⁸O values with intra-seasonal resolution. Earth & Planetary Science Letters, 2016, 443: 9-19
[31] Ogée J, Barbour MM, Wingate L, et al. A single-substrate model to interpret intra-annual stable isotope signals in tree-ring cellulose. Plant, Cell & Environment, 2010, 32: 1071-1090
[32] Zeng X, Liu X, Treydte K, et al. Climate signals in tree-ring δ¹⁸O and δ¹³C from southeastern Tibet: Insights from observations and forward modelling of intra- to interdecadal variability. New Phytologist, 2017, 216: 1104-1118
[33] Poussart PF, Schrag DP. Seasonally resolved stable isotope chronologies from northern Thailand deciduous trees. Earth and Planetary Science Letters, 2005, 235: 752-765
[34] Zhu M, Stott L, Buckley B, et al. 20th century seasonal moisture balance in Southeast Asian montane forests from tree cellulose δ¹⁸O. Climatic Change, 2012, 115: 505-517
[35] Zhu M, Stott L, Buckley B, et al. Indo-Pacific Warm Pool convection and ENSO since 1867 derived from Cambodian pine tree cellulose oxygen isotopes. Journal of Geophysical Research, 2012, 117: D11307, doi:10.1029/2011JD017198
[36] Ballantyne AP, Baker PA, Chambers JQ, et al. Regional differences in south American monsoon precipitation inferred from the growth and isotopic composition of tropi-cal trees. Earth Interaction, 2011, 15: 1-35
[37] Boysen BMM, Evans MN, Baker PJ. δ¹⁸O in the tropical conifer Agathis robusta records ENSO-related precipitation variations. PLoS ONE, 2014, 9(7): e102336
[38] Sargeant CI, Singer MB. Sub-annual variability in historical water source use by Mediterranean riparian trees. Ecohydrology, 2016, 9: 1328-1345
[39] Xu G, Liu X, Sun W, et al. Seasonal divergence between soil water availability and atmospheric moisture recorded in intra-annual tree-ring δ¹⁸O extremes. Environmental Research Letters, 2020, 15: 094036, doi:10.1088/1748-9326/ab9792
[40] Walcroft AS, Silvester WB, Whitehead D, et al. Seasonal changes in stable carbon isotope ratios within annual rings of Pinus radiata reflect environmental regulation of growth processes. Functional Plant Biology, 1997, 24: 57-68
[41] Barbour M, Walcroft AS, Farquhar GD. Seasonal variation in δ¹³C and δ¹⁸O of cellulose from growth rings of Pinus radiata. Plant, Cell & Environment, 2002, 25: 1483-1499
[42] Poussart PF, Evans MN, Schrag DP, et al. Resolving seasonality in tropical trees: Multi-decade, high-resolution oxygen and carbon isotope records from Indonesia and Thailand. Earth and Planetary Science Letters, 2004, 218: 301-316
[43] Xu C, Sano M, Yoshimura K, et al. Oxygen isotopes as a valuable tool for measuring annual growth in tropical trees that lack distinct annual rings. Geochemical Journal, 2014, 48: 371-378
[44] Verheyden A, Helle G, Schleser GH, et al. Annual cyclicity in high-resolution stable carbon and oxygen isotope ratios in the wood of the mangrove tree Rhizophora mucronata. Plant, Cell & Environment, 2004, 27: 1525-1536
[45] Ogle N, Turney CSM, Kalin RM, et al. Palaeovolcanic forcing of short-term dendroisotopic depletion: The effect of decreased solar intensity on Irish oak. Geophysical Research Letters, 2005, 32: L04708, doi:10.1029/2004GL021623
[46] Weidner K, Helle G, Löffler J, et al. The reaction of δ¹³C, δ¹⁸O and ring width on Larch Budmoth (Zeiraphera diniana Gn.) outbreaks in the European Larch (Larix decidua Mill.): A case study in the Lötschental, Switzerland. TRACE, Switzerland, 2005: 281-286
[47] Anchukaitis KJ, Evans MN. Tropical cloud forest climate variability and the demise of the Monteverde golden toad. Proceedings of the National Academy of Sciences of the United States of America, 2010, 107: 5036-5040
[48] Szejner P, Clute T, Anderson E, et al. Reduction in lumen area is associated with the δ¹⁸O exchange between sugars and source water during cellulose synthesis. New Phytologist, 2020, 226: 1583-1593
[49] Vaganov E, Schulze E, Skomarkova MV, et al. Intra-annual variability of anatomical structure and δ¹³C values within tree rings of spruce and pine in alpine, temperate and boreal Europe. Oecologia, 2009, 161: 729-745
[50] Soudant A, Loader NJ, Back J, et al. Intra-annual varia-bility of wood formation and δ¹³C in tree-rings at Hyytiälä, Finland. Agricultural and Forest Meteorology, 2016, 224: 17-29
[51] Dodd JP, Patterson WP, Holmden C, et al. Robotic micromilling of tree-rings: A new tool for obtaining subseasonal environmental isotope records. Chemical Geology, 2008, 252: 21-30
[52] Schollaen K, Heinrich I, Neuwirth B, et al. Multiple tree-ring chronologies (ring width, δ¹³C and δ¹⁸O) reveal dry and rainy season signals of rainfall in Indonesia. Quaternary Science Reviews, 2013, 73: 170-181
[53] Xu C, Sano M, Nakatsuka T. Tree ring cellulose δ¹⁸O of Fokienia hodginsii in northern Laos: A promising proxy to reconstruct ENSO? Journal of Geophysical Research, 2011, 116: D24109, doi: 10.1029/2011JD016694
[54] Li Z, Labbé N, Driese SG, et al. Micro-scale analysis of tree-ring δ¹⁸O and δ¹³C on α-cellulose spline reveals high-resolution intra-annual climate variability and tropical cyclone activity. Chemical Geology, 2011, 284: 138-147
[55] Gessler A, Brandes E, Keitel C, et al. The oxygen isotope enrichment of leaf-exported assimilates: Does it always reflect lamina leaf water enrichment? New Phyto-logist, 2013, 200: 144-157
[56] Roden JS, Lin G, Ehleringer JR. A mechanistic model for interpretation of hydrogen and oxygen isotope ratios in tree-ring cellulose. Geochimica et Cosmochimica Acta, 2000, 64: 21-35
[57] Berkelhammer M, Still CJ, Ritter F, et al. Persistence and plasticity in conifer water-use strategies. Journal of Geophysical Research: Biogeosciences, 2020, 125, doi: 10.1029/2018JG004845
[58] Barbour MM, Roden JS, Ehleringer FJR, et al. Expressing leaf water and cellulose oxygen isotope ratios as enrichment above source water reveals evidence of a Péclet effect. Oecologia, 2004, 138: 426-435
[59] 张铁钢, 李占斌, 李鹏, 等. 土石山区不同植物土壤水分利用方式对降雨的响应特征. 应用生态学报, 2016, 27(5): 1461-1467 [Zhang T-G, Li Z-B, Li P, et al. Response characteristics of soil water use patterns by different plants to precipitation in rocky mountainous areas. Chinese Journal of Applied Ecology, 2016, 27(5): 1461-1467]
[60] 徐晓梧, 李瀚之, 余新晓, 等. 基于稳定碳同位素的北京西山侧柏林生态系统呼吸区分. 应用生态学报, 2020, 31(6): 1844-1850 [Xu X-W, Li H-Z, Yu X-X, et al. Partitioning ecosystem respiration of a Platycladus orientalis forest in the west mountainous area of Beijing, China using stable carbon isotope. Chinese Journal of Applied Ecology, 2020, 31(6): 1844-1850]

树木年轮年内高分辨率稳定同位素记录:方法、进展和展望

Intra-annual high resolution stable isotope records of tree ring: Methods, progress and prospects

PDF (PC)

可视化

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 15

编辑推荐

Metrics

本文评价

[1]	高欣, 杨立新, 陈振举. 基于树木年轮径切特征的卷积神经网络树种识别 [J]. 应用生态学报, 2023, 34(1): 47-57.
[2]	李颖辉, 齐贵增, 冯荣荣, 刘康. 秦岭北麓油松径向生长对气候变化的响应 [J]. 应用生态学报, 2022, 33(8): 2043-2050.
[3]	韩艳刚, 盖学瑞, 邱思玉, 张月, 王守乐, 周莉, 于大炮. 大兴安岭兴安落叶松径向生长对气候响应的时空变化 [J]. 应用生态学报, 2021, 32(10): 3397-3404.
[4]	杨婧雯, 张秋良, 宋文琦, 张旭, 李宗善, 张远东, 王晓春. 大兴安岭兴安落叶松和樟子松径向生长对气候变化的响应差异 [J]. 应用生态学报, 2021, 32(10): 3415-3427.
[5]	肖健宇, 张文艳, 牟玉梅, 吕利新. 树木年轮揭示的东灵山主要树种间干旱耐受性差异 [J]. 应用生态学报, 2021, 32(10): 3487-3496.
[6]	李静茹, 彭剑峰, 杨柳, 崔佳月, 李轩, 彭猛. 川西高原两种针叶树径向生长对气候因子的响应 [J]. 应用生态学报, 2021, 32(10): 3512-3520.
[7]	刘兰娅, 勾晓华, 张芬, 尹定财, 王学佳, 夏敬清, 李芊, 杜苗苗. 升温对祁连山东部青海云杉径向生长的影响 [J]. 应用生态学报, 2021, 32(10): 3576-3584.
[8]	苟晓霞, 张同文, 袁玉江, 喻树龙, 张瑞波, 姜盛夏, 郭玉琳. 阿尔泰山主要针叶树种树木径向生长及其对气候变化的响应 [J]. 应用生态学报, 2021, 32(10): 3594-3608.
[9]	曹红华, 赵晓恩, 陈峰, 王世杰, 刘兴华. 基于油松树轮重建晋东南地区近296年来1—6月降水变化 [J]. 应用生态学报, 2021, 32(10): 3618-3626.
[10]	袁晴雪, 喻树龙, 姜盛夏, 秦宁生, 张同文. 川西雅江地区过去567年3—8月干旱变化的树轮重建 [J]. 应用生态学报, 2021, 32(10): 3627-3635.
[11]	朱晓龙, 陈庆美, 吕爱锋, 黄茹, 邵雪梅, 梁尔源, 朱海峰. 利用树轮揭示人类活动对柴达木盆地巴音河径流量的影响 [J]. 应用生态学报, 2021, 32(10): 3653-3660.
[12]	白耀玉, 韩宜洁, 王坷坷, 刘波. 秦岭山地针叶树种树木生长对气候变化的响应 [J]. 应用生态学报, 2021, 32(10): 3715-3723.
[13]	康虎虎, 刘晓宏, 张馨予, 郭军明, 吴国菊, 徐国保, 康世昌. 树木年轮汞记录: 进展、问题和展望 [J]. 应用生态学报, 2021, 32(10): 3733-3742.
[14]	于健, 陈佳佳, 孟盛旺, 周华, 周光, 高露双, 王永平, 刘琪璟. 长白山群落交错带长白松和鱼鳞云杉径向生长对气候变暖的响应 [J]. 应用生态学报, 2021, 32(1): 46-56.
[15]	华亚伟, 张红娟, 刘康. 基于油松树轮重建陕西省镇安县165年以来3—4月平均最高气温 [J]. 应用生态学报, 2020, 31(2): 381-387.