油松（ Pinus tabulaeformis ）径向生长对气候响应的区域分异特征

苏靖茸; 肖生春; 彭小梅; 车存伟; 赵鹏

doi:10.7522/j.issn.1000-694X.2024.00034

中国沙漠 >

2024 , Vol. 44 >Issue 5: 60 - 72

DOI: https://doi.org/10.7522/j.issn.1000-694X.2024.00034

油松（ Pinus tabulaeformis ）径向生长对气候响应的区域分异特征

苏靖茸 ,
肖生春 ,
彭小梅 ,
车存伟 ,
赵鹏

展开

^1.中国科学院西北生态环境资源研究院干旱区生态安全与可持续发展全国重点实验室，甘肃兰州 730000
^2.中国科学院大学，北京 100049
^3.西北师范大学地理与环境科学学院，甘肃兰州 730070
^4.淮南师范学院计算机学院，安徽淮南 232038

肖生春（E-mail： xiaosc@lzb.ac.cn）
苏靖茸（1989—），女，甘肃白银人，博士研究生，主要从事树轮生态学研究。E-mail： sujingrong@nieer.ac.cn

收稿日期: 2023-10-20

修回日期: 2024-02-17

网络出版日期: 2024-10-15

基金资助

国家自然科学基金项目(41977419);内蒙古自治区科技成果转化专项(2021CG0046);阿拉善盟科技计划项目(AMYY 2021-19)

收起

Regional differentiation of radial growth to climate response of Chinese pine （ Pinus tabulaeformis ）

Jingrong Su ,
Shengchun Xiao ,
Xiaomei Peng ,
Cunwei Che ,
Peng Zhao

Expand

^1.Key Laboratory of Ecological Safety and Sustainable Development in Arid Lands，Northwest Institute of Eco-Environment and Resources，Chinese Academy of Sciences，Lanzhou 730000，China
^2.University of Chinese Academy of Sciences，Beijing 100049，China
^3.Geography and Environmental Science，Northwest Normal University，Lanzhou 730070，China
^4.School of Computer Science，Huainan Normal University，Huainan 232038，Anhui，China

Received date: 2023-10-20

Revised date: 2024-02-17

Online published: 2024-10-15

Fold

摘要

油松（Pinus tabulaeformis）是中国特有且广泛分布的针叶树种，也是中国北方地区的主要造林树种。气候变化对油松生长的影响是种群生态学研究的热点。基于油松树木年轮学文献成果，系统梳理分析了不同降水、气温等因素影响下中国北方地区油松径向生长特征，试图明晰其区域分异特征，以期为油松天然林和人工林管理提供理论和决策依据。结果表明：（1）在年降水量低于400 mm的区域，限制油松径向生长的主要因素是生长季降水；在年降水量400~600 mm的区域，生长季的水热因素共同影响油松的径向生长；在年降水量高于600 mm区域，油松的径向生长主要受5月降水与平均气温及其共同作用的干旱胁迫影响。（2）上年降水对油松径向生长的“滞后效应”主要体现在年降水量低于600 mm和年均气温低于9 ℃的区域。（3）冬季气温对年降水量高于600 mm和年均气温高于9 ℃区域油松的生长起促进作用，对年降水量低于600 mm和年均气温低于9 ℃的区域起抑制作用。在全球气候变暖背景下，油松分布区将面临从干旱半干旱区向相对湿润区、从低海拔向高海拔移动的趋势。

关键词： 油松; 径向生长; 气候响应; 区域分异特征

本文引用格式

苏靖茸 , 肖生春 , 彭小梅 , 车存伟 , 赵鹏 . 油松（ Pinus tabulaeformis ）径向生长对气候响应的区域分异特征[J]. 中国沙漠, 2024 , 44(5) : 60 -72 . DOI: 10.7522/j.issn.1000-694X.2024.00034

Abstract

Pinus tabulaeformis，an endemic and widely distributed conifer in China， is widely distributed conifer species in China， and it is also the main afforestation species in the northern region of China. The impact of climate change on the growth of P. tabuliformis has become a hot research topic of genecology. In this study， based on the results of research on the chronology of P. tabuliformis， we systematically sorted out and analyzed the characteristics of the response of its radial growth to climatic factors under the influence of different precipitation， temperature， and other factors in the northern region of China. Our aim was to clarify the regional differentiation characteristics and provide a theoretical and decision-making basis for the management of natural and planted forests of P. tabuliformis. The results showed the following：（1） The main factor limiting the radial growth of P. tabuliformis is precipitation during the growing season. In regions with annual precipitation lower than 400 mm， hydrothermal factors in the growing season mainly influence the radial growth. In regions with annual precipitation of 400-600 mm， the radial growth of P. tabuliformis is mainly limited by temperature and precipitation. In regions with annual precipitation higher than 600 mm， the radial growth of P. tabuliformis is mainly affected by May precipitation and temperature and their combined effect of drought stress （2） The “lagging effect” of precipitation （e.g.， the previous precipitation of September） on the radial growth of P. tabuliformis is a significant factor， and it is mainly observed in regions with annual precipitation lower than 600 mm and annual mean temperatures below 9 ℃. （3） Winter temperature promotes the growth of P. tabuliformis in regions with annual precipitation higher than 600 mm and annual mean temperatures higher than 9 ℃. However， it inhibits the growth in regions with annual precipitation lower than 600 mm and annual mean temperatures lower than 9 ℃. Under the climatic background of global warming， the distribution of P. tabuliformis is likely to shift from arid and semi-arid regions to relatively humid regions and from low to high altitudes.

Key words： Pinus tabulaeformis; radial growth; climate response; regional differentiation

参考文献

1	Brubaker L B.Tree rings and climate［J］.Ecology，1977，58（6）：1400-1401.
2	方克艳，勾晓华，陈发虎，等.树轮生态学研究进展［J］.冰川冻土，2008，30（5）：825-834.
3	Guo H， Wang B， Ma X Q，et al.Evaluation of ecosystem services of Chinese pine forests in China［J］.Science in China Series C：Life Sciences，2008，51：662-670.
4	王生军，韩丽华，李春红，等.樟子松、赤松、油松在形态结构及生态生物学特性的比较研究［J］.干旱区资源与研究，2008，22（10）：179-182.
5	韩超，肖生春，丁爱军，等.腾格里沙漠南缘青海云杉（Picea crassifolia）和油松（Pinus tabulaeformis）年轮记录的气候变化［J］.中国沙漠，2020，40（3）：50-58.
6	Chen F， Yuan Y J， Chen F H，et al.Reconstruction of spring temperature on the southern edge of the Gobi Desert，Asia，reveals recent climatic warming［J］.Palaeogeography Palaeoclimatology Palaeoecology，2014，409：145-52.
7	Fang K Y， Gou X H， Chen F，et al.Tree-ring based reconstruction of drought variability （1615-2009） in the Kongtong Mountain area，northern China［J］.Global and Planetary Change，2012，80：190-197.
8	Sun J Y， Liu Y， Wang Y C，et al.Tree-ring based runoff reconstruction of the upper Fenhe River basin，North China，since 1799 AD［J］.Quaternary International，2013，283：117-124.
9	Chen F， Yuan Y J， Wei W S，et al.Reconstructed precipitation for the north-central China over the past 380 years and its linkages to East Asian summer monsoon variability［J］.Quaternary International，2013，283：36-45.
10	陈智平，张涛，赵万奎，等.黄土高原子午岭林区油松林种子雨强度及时空动态特征［J］.中国沙漠，2020，40（3）：85-93.
11	刘淑明，董立民.油松地理分布区质量等级的划分［J］.西北林学院学报，1995，10（3）：35-39.
12	徐文铎，邹春静.中国沙地森林生态系统［M］.北京：中国森林出版社，1998.
13	Li G Q， Xu G H， Guo K，et al.Geographical boundary and climatic analysis of Pinus tabulaeformis in China：insights on its afforestation［J］.Ecological Engineering，2016，86：75-84.
14	Wang X F， Yang B.Divergent tree radial growth at alpine coniferous forest ecotone and corresponding responses to climate change in northwestern China［J］.Ecological Indicators，2020，121：107052.
15	Chen K， Jiao L， Liu X P，et al.Evaluation of the response stability of two dominant conifer species to climate change in the southern margin of the Tengger Desert［J］.Global Ecology and Conservation，2021，25：e01439.
16	郭树杰，徐华，宋建昌，等.油松种质资源调查收集初报［J］.陕西林业科技，2013（4）：28-30.
17	赵莹，蔡立新，靳雨婷，等.暖干化加剧东北半干旱地区油松人工林径向生长的水分限制［J］.应用生态学报，2021，32（10）：3459-3467.
18	Cai L X， Li J X， Bai X P，et al.Variations in the growth response of Pinus tabulaeformis to a warming climate at the northern limits of its natural range［J］.Trees，2020，34：707-719.
19	刘鸣.系统评价Meta分析与评价方法［M］.北京：人民卫生出版社，2011.
20	郑景云，尹云鹤，李炳元.中国气候区划新方案［J］.地理学报，2010，65（1）：2-12.
21	高艳红，许建伟，张萌.中国 400 mm 等降水量变迁与干湿变化研究进展［J］.地球科学进展，2020，35（11）：1101-1112.
22	Gong C， Tand Q U， Xua M X，et al.Mixed-species plantations can alleviate water stress on the Loess Plateau［J］.Forest Ecology and Management，2020，458：117767.
23	Liu Y， Song H M， Sun C F，et al.The 600-mm precipitation isoline distinguishes tree-ring-width responses to climate in China［J］.National Science Review，2019，6：359-368.
24	Van Mantgem P J， Stephenson N L， Byrne J C，et al.Widespread increase of tree mortality rates in the western United States［J］.Science，2009，323：521-524.
25	李颖辉，齐贵增，冯荣荣，等.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.
26	Liu Y， Linderholm H W， Song H M，et al.Temperature variations recorded in Pinus tabulaeformis tree rings from the southern and northern slopes of the central Qinling Mountains，central China［J］.Journal of Quaternary Science，2008，38：285-291.
27	Van D， Barichivich J， Briffa K R，et al.A scPDSI-based global data set of dry and wet spells for 1901-2009［J］.Journal of Geophysical Research Atmospheres，2013，118（10）：4025-4048.
28	Gou X H， Chen F， Jacoby G，et al.Rapid tree growth with respect to the last 400 years in response to climate warming，northeastern Tibetan Plateau［J］.International Journal of Climatology，2007，27（11）：1497-1503.
29	Cai Q F， Liu Y.Climatic response of three tree species growing at different elevations in the Lüliang Mountains of northern China［J］.Dendrochronologia，2013，31（4）：311-317.
30	Zhang X， Liu Y， Song H，et al.Interannual variability of PDSI from tree-ring widths for the past 278 years in Baotou，China［J］.Trees，2017，31：1531-1541.
31	M?kinen H， N?jd P， Kahle H P，et al.Large-scale climatic variability and radial increment variation of Picea abies （L.） in central and northern Europe［J］.Trees，2003，17：173-184.
32	Camarero J J， Rubio-Cuadrado A.Relating climate，drought and radial growth in broadleaf mediterranean tree and shrub species：a new approach to quantify climate-growth relationships［J］.Forest，2020，11（12）：1250.
33	Bai M W， Dong Z P， Chen D，et al.Different responses of the radial growth of the planted and natural forests to climate change in humid subtropical China［J］.Geografiska Annaler Series：A，Physical Geography，2020，102（1）：1-12.
34	Domec J， King J S， Ward E，et al.Conversion of natural forests to managed forest plantations decreases tree resistance to prolonged droughts［J］.Forest Ecology and Management，2015 355：58-71.
35	Che C W， Xiao S C， Ding A J，et al.Growth response of plantations Hippophae rhamnoides Linn.on different slope aspects and natural Caragana opulens Kom.to climate and implications for plantations management［J］.Ecological Indicators，2022，138：108833.
36	Che C W， Xiao S C， Peng X M，et al.Radial growth of Korshinsk peashrub and its response to drought in different sub-arid climate regions of northwest China［J］.Journal of Environmental Management，2023，326：116708.
37	IPCC.Climate Change 2021：the Physical Science Basis［M］.Cambridge，UK：Cambridge University Press，2021.
38	Marcott S A， Shakun J， Clark P U，et al.A reconstruction of areasal and global temperature for the past 11，300 years［J］.Science，2013，339（6124）：1198-1201.
39	Liu H， Cui H， Yu P，et al.The origin of remnant forest stands of Pinus tabulaeformis in southeastern Inner Mongolia［J］.Plant Ecology，2002，158：139-151.
40	刘慎谔.东北木本植物图志［M］.北京：科学出版社，1955
41	韦红红.北京松山不同地形条件下油松径向生长与气候的关系［D］.北京：北京林业大学，2017.
42	Du H， Liu J， Li M H，et al.Warming-induced upward migration of the alpine treeline in the Changbai Mountains，northeast China［J］.Global Change Biology，2018，24：1256-1266.

Options

文章导航

模态框（Modal）标题

摘要

本文引用格式

Abstract

参考文献