多指标记录的1962—2008年长白山园池泥炭地地表湿度变化

doi:10.13287/j.1001-9332.202102.008

应用生态学报 ›› 2021, Vol. 32 ›› Issue (2): 477-485.doi: 10.13287/j.1001-9332.202102.008

多指标记录的1962—2008年长白山园池泥炭地地表湿度变化

刘玉芳^1,2,3, 李鸿凯^1,2,3, 赵红艳^1,2,3*, 卜兆君^1,2,3, 王升忠^1,2,3

¹东北师范大学地理科学学院, 长白山地理过程与生态安全教育部重点实验室, 长春 130024;
²东北师范大学泥炭沼泽研究所, 国家环境保护湿地生态与植被恢复重点实验室, 长春 130024;
³吉林省长白山湿地生态过程与环境变化重点实验室, 长春 130024

收稿日期:2020-07-01 接受日期:2020-11-09 出版日期:2021-02-15 发布日期:2021-08-15
通讯作者: ^*E-mail: hyzhao@nenu.edu.cn
作者简介:刘玉芳, 女, 1996年生, 硕士研究生。主要从事自然地理学与湿地生态学研究。E-mail: liuyf873@nenu.edu.cn
基金资助:
国家自然科学基金项目(41471165,41771217)和国家级大学生创新创业训练计划创新训练项目(202010200111402)资助

The variations of surface wetness recorded by multi-proxies in Yuanchi peatland of the Changbai Mountains from 1962 to 2008

LIU Yu-fang^1,2,3, LI Hong-kai^1,2,3, ZHAO Hong-yan^1,2,3*, BU Zhao-jun^1,2,3, WANG Sheng-zhong^1,2,3

¹Ministry of Education Key Laboratory of Geographical Processes and Ecological Security in Changbai Mountains, School of Geographical Science, Northeast Normal University, Changchun 130024, China;
²State Environmental Protection Key Laboratory of Wetland Ecology and Vegetation Restoration, Institute for Peat and Mire Research, Northeast Normal University, Changchun 130024, China;
³Jilin Provincial Key Laboratory for Wetland Ecological Processes and Environmental Change in the Changbai Mountains, Changchun 130024, China

Received:2020-07-01 Accepted:2020-11-09 Online:2021-02-15 Published:2021-08-15
Contact: ^*E-mail: hyzhao@nenu.edu.cn
Supported by:
National Natural Science Foundation of China (41471165, 41771217) and the National Training Program of Innovation and the Entrepreneurship for Undergraduates (202010200111402)

摘要/Abstract

摘要： 使用AMS ¹⁴C和¹³⁷Cs方法建立年代序列,通过植物残体、有壳变形虫和腐殖化度3个指标的综合分析,重建了长白山园池泥炭地地表的湿度变化,并探讨其对气候的响应。结果表明: 园池泥炭地地表50 cm泥炭植物残体以藓类为主,利用去趋势对应分析(DCA)发现,第一轴得分代表沼泽表面湿度变化,将植物残体揭示的1962—2008 A.D.间泥炭地地表湿度与有壳变形虫-水位间转换函数得到的水位埋深以及腐殖化度进行对比,发现植物残体、有壳变形虫和腐殖化度揭示的沼泽表面湿度变化总体趋势一致,即40～50 cm层(1962—1975 A.D.)湿度较大;27～40 cm层(1975—1987 A.D.)湿度变小,处于干湿交替期;0～27 cm层(1987—2008 A.D.)湿度较小。将3种指标重建的地表湿度与二道气象站数据对比发现,气候代用指标揭示的沼泽地表湿度变化与温度的变化趋势基本吻合,沼泽地地表湿度降低发生在夏季温度和年均温偏高的年份。由此推测,近46年来沼泽地地表湿度变化主要是对温度升高引起的有效降水减弱的响应。

关键词: 植物残体, 有壳变形虫, 腐殖化度, 水文气候, 长白山

Abstract: Surface wetness of Yuanchi peatland in the Changbai Mountains were reconstructed by comprehensive analysis on plant residue, testate amoeba and humification, using the age-depth model established with AMS ¹⁴C and ¹³⁷Cs dating methods. The response of surface wetness to climate change was addressed. Results showed that plant residues in the top 50 cm of peat sequence were dominated by mosses. Detrended correspondence analysis (DCA) of plant residue revealed that axis 1 of DCA biplot might represent mire surface wetness (MSW). MSW from 1962 to 2008 as indicated by axis 1 scores of DCA on plant residue were compared with depths to water table derived by testate amoebae-DWT transfer function and humification measurements, and the results showed that the trends of MSW reconstructed by three proxies were largely consistent. They were wetter MSW from 40-50 cm (1962 to 1975), 27-40 cm (fluctuating from wet to dry from 1975 to 1987), and 0-27 cm (drier from 1987 to 2008). Compared with instrumental data from nearby Erdao weather station, the reconstructed MSW was basically consistent with temperature change in this period. The decreases of MSW occurred when mean summer temperature and mean annual temperature were higher than long-term mean value. Our results suggest that the variability in MSW in the recent 46 years predominantly responded weakening of effective precipitation induced by increasing temperature.

Key words: plant residue, testate amoebae, humification, hydrological climate, Changbai Mountains

刘玉芳, 李鸿凯, 赵红艳, 卜兆君, 王升忠. 多指标记录的1962—2008年长白山园池泥炭地地表湿度变化[J]. 应用生态学报, 2021, 32(2): 477-485.

LIU Yu-fang, LI Hong-kai, ZHAO Hong-yan, BU Zhao-jun, WANG Sheng-zhong. The variations of surface wetness recorded by multi-proxies in Yuanchi peatland of the Changbai Mountains from 1962 to 2008[J]. Chinese Journal of Applied Ecology, 2021, 32(2): 477-485.

参考文献

[1] Daley TJ, Barber KE. Multi-proxy Holocene palaeoclimate records from Walton Moss, northern England and Dosenmoor, northern Germany, assessed using three statistical approaches. Quaternary International, 2012, 268: 111-127
[2] Booth RK. Testate amoebae as proxies for mean annual water-table depth in Sphagnum-dominated peatlands of North America. Journal of Quaternary Science, 2008, 23: 43-57
[3] Blackford JJ, Chambers FM. Proxy climate record for the last 1000 years from Irish blanket peat and a possible link to solar variability. Earth and Planetary Science Letters, 1995, 133: 145-150
[4] De Klerk P, Haberl A, Kaffke A, et al. Vegetation history and environmental development since ca 6000 cal yr BP in and around Ispani 2 (Kolkheti lowlands, Georgia). Quaternary Science Reviews, 2009, 28: 890-910
[5] Hughes P, Mauquoy D, Barber K, et al. Mire-development pathways and palaeoclimatic records from a full Holocene peat archive at Walton Moss, Cumbria, England. The Holocene, 2000, 10: 465-479
[6] Charman DJ, Barber KE, Blaauw M, et al. Climate drivers for peatland palaeoclimate records. Quaternary Science Reviews, 2009, 28: 1811-1819
[7] Chambers FM, Charman DJ. Holocene environmental change: Contributions from the peatland archive. Holo-cene, 2004, 14: 1-6
[8] Blundell A, Charman D, Barber K. Multiproxy late Holo-cene peat records from Ireland: Towards a regional palaeoclimate curve. Journal of Quaternary Science, 2008, 23: 59-71
[9] Payne R, Ratcliffe J, Andersen R, et al. A meta-database of peatland palaeoecology in Great Britain. Palaeogeography, Palaeoclimatology, Palaeoecology, 2016, 457: 389-395
[10] 赵红艳, 李鸿凯, 韩毅, 等. 长白山西侧哈泥沼泽表面湿度的多指标记录及其可能的驱动因素. 第四纪研究, 2014, 34(2): 434-442 [Zhao H-Y, Li H-K, Han Y, et al. A multi-proxy record of surface wetness in Hani mire of west Changbaishan Mountain and possible drivers. Quaternary Sciences, 2014, 34(2): 434-442]
[11] Lamentowicz M, Galka M, Milecka K, et al. A 1300-year multi-proxy, high-resolution record from a rich fen in northern Poland: Reconstructing hydrology, land use and climate change. Journal of Quaternary Science, 2013, 28: 582-594
[12] 邵雪梅, 吴祥定. 利用树轮资料重建长白山区过去气候变化. 第四纪研究, 1997, 17(1): 76-85 [Shao X-M, Wu X-D. Reconstruction of climate on Changbai Mountain, northeast China using tree-ring data. Quaternary Sciences, 1997, 17(1): 76-85]
[13] 张彦, 史彩奎, 王健, 等. 长白山圆池泥炭沼泽演变及环境信息记录. 湿地科学, 2012, 10(3): 271-277 [Zhang Y, Shi C-K, Wang J, et al. The evolution and environment archives of Yuanchi peat mires in Changbai Mountains. Wetland Science, 2012, 10(3): 271-277]
[14] Hong YT, Hong B, Lin QH, et al. Synchronous climate anomalies in the western North Pacific and North Atlantic regions during the last 14000 years. Quaternary Science Reviews, 2009, 28: 840-849
[15] Hong B, Liu C, Lin Q, et al. Temperature evolution from the δ¹⁸O record of Hani peat, Northeast China, in the last 14000 years. Science in China Series D: Earth Sciences, 2009, 52: 952-964
[16] Zheng YH, Zhou WJ, Liu Z, et al. Compositions of aliphatic des-A-triterpenes in the Hani peat deposit, Northeast China and its biological significance. Chinese Science Bulletin, 2010, 21: 2275-2281
[17] Zhou W, Zheng Y, Meyers PA, et al. Postglacial climate-change record in biomarker lipid compositions of the Hani peat sequence, Northeastern China. Earth & Planetary Science Letters, 2010, 294: 37-46
[18] 喻春霞, 罗运利, 孙湘君. 吉林柳河哈尼湖13.1—4.5 cal.ka B.P.古气候演化的高分辨率孢粉记录. 第四纪研究, 2008, 28(5): 929-938 [Yu C-X, Luo Y-L, Sun X-J. A high-resolution pollen records from Ha’ni lake, Jilin, northeast China showing climate changes between 13.1 cal.ka B.P. and 4.5 cal.ka B.P. Quaternary Sciences, 2008, 28(5): 929-938]
[19] 卜兆君, 杨允菲, 代丹, 等. 长白山泥炭沼泽桧叶金发藓种群的年龄结构与生长分析. 应用生态学报, 2005, 16(1): 44-48 [Bu Z-J, Yang Y-F, Dai D, et al. Age structure and growth pattern of Polytrichum juniperum populations in a mire of Changbai Mountains. Chinese Journal of Applied Ecology, 2005, 16(1): 44-48]
[20] 贾琳, 王国平, 刘景双. 长白山圆池泥炭常量和微量元素分布特征及其环境意义. 山地学报, 2006, 24(6): 662-666 [Jia L, Wang G-P, Liu J-S. Distribution and implications of major and trace elements in peat profiles of Yuanchi, Changbai Mountain. Mountain Research, 2006, 24(6): 662-666]
[21] 苏莹, 赵明宪, 王国平. 长白山圆池泥炭氮元素分布特征及其影响因素分析. 湿地科学, 2006, 4(4): 292-297 [Su Y, Zhao M-X, Wang G-P. Characteristics of nitrogen distribution and their affecting factors in the peat profiles of the Yuanchi in the Changbaishan Mountains. Wetland Science, 2006, 4(4): 292-297]
[22] Van Der Plicht J, Yeloff D, Van Der Linden M, et al. Dating recent peat accumulation in European Ombrotrophic Bogs. Radiocarbon, 2013, 55: 1763-1778
[23] Nilsson M, Klarqvist M, Bohlin E, et al. Variation in ¹⁴C age of macrofossils and different fractions of minute peat samples dated by AMS. The Holocene, 2001, 11: 579-586
[24] Goslar T, Van Der Knaap WO, Hicks S, et al. Radiocarbon dating of modern peat profiles: Pre- and post-bomb ¹⁴C variations in the construction of age-depth models. Radiocarbon, 2005, 47: 115-134
[25] Clarke LJ, Robinson SA, Hua Q, et al. Radiocarbon bomb spike reveals biological effects of Antarctic climate change. Global Change Biology, 2012, 18: 301-310
[26] Aaby B. Cyclic climatic variations in climate over the past 5500 yr reflected in raised bogs. Nature, 1976, 263: 281-284
[27] Payne R, Blackford J. Peat humification and climate change: A multi-site comparison from mires in south-east Alaska. Mires and Peat, 2008, 3: 1-11
[28] Chambers FM, Beilman DW, Yu Z. Methods for determining peat humification and for quantifying peat bulk density, organic matter and carbon content for palaeo-studies of climate and peatland carbon dynamics. Mires & Peat, 2011, 7: 1-10
[29] Barber K, Chambers F, Maddy D, et al. A sensitive high-resolution record of Late-Holocene climatic change from a raised bog in Northern England. The Holocene, 1994, 4: 198-205
[30] Mauquoy D, Hughes PDM, Geel VB. A protocol for plant macrofossil analysis of peat deposits. Mires & Peat, 2010, 7: 1-5
[31] Booth RK, Lamentowicz M, Charman DJ. Preparation and analysis of testate amoebae in peatland palaeoenvi-ronmental studies. Mires & Peat, 2010, 7: 1-7
[32] Charman DJ, Hendon D, Woodland WA. The identification of testate amoebae (Protozoa: Rhizopoda) in peats, technical guide No. 9. Quaternary Science Reviews, 2004, 23: 1869
[33] Davis RB, Hess CT, Norton SA, et al. ¹³⁷Cs and ²¹⁰Pb dating of sediments from soft-water lakes in New England (U.S.A.) and Scandinavia, a failure of ¹³⁷Cs dating. Chemical Geology, 1984, 44: 151-185
[34] Li HC, Wang J, Sun J, et al. Study of Jinchuan Mire in NE China. Ⅰ. AMS ¹⁴C, ²¹⁰Pb and ¹³⁷Cs dating on peat cores. Quaternary International, 2019, 528: 9-17
[35] Mauquoy D, Barber K. Testing the sensitivity of the palaeoclimatic signal from ombrotrophic peat bogs in northern England and the Scottish Borders. Review of Palaeobotany & Palynology, 2002, 119: 219-240
[36] 秦养民, 顾延生, 周修高, 等. 第四纪环境重建的良好代用指标——有壳变形虫记录与古生态学研究进展. 地球科学进展, 2008, 23(8): 803-812 [Qin Y-M, Gu Y-S, Zhou X-G, et al. An excellent indicator for quaternary paleoenvironmental reconstructions—Advances in the study of testate amoebae (Thecamoe-bians, Arcellacean). Advances in Earth Science, 2008, 23(8): 803-812]
[37] Charman DJ. Biostratigraphic and palaeoenvironmental applications of testate amoebae. Quaternary Science Reviews, 2001, 20: 1753-1764
[38] Warner BG, Charman DJ. Holocene changes on a peatland in northwestern Ontario interpreted from testate amoebae (Protozoa) analysis. Boreas, 1994, 23: 270-279
[39] Yang QN, Li HC, Zhao HY, et al. Hydroclimate controls of the distribution and abundance of mosses in Hani mire, Northeast China: Modern vegetation survey and peat-core analysis. Quaternary International, 2019, 528: 30-40
[40] Charman DJ, Hendon D, Packman S. Multiproxy surface wetness records from replicate cores on an ombrotrophic mire: Implications for Holocene palaeoclimate records. Journal of Quaternary Science, 1999, 14: 451-463
[41] Barber KE, Maddy D, Rose N, et al. Replicated proxy-climate signals over the last 2000 yr from two distant UK peat bogs: New evidence for regional palaeoclimate teleconnections. Quaternary Science Reviews, 2000, 19: 481-487
[42] Charman DJ, Brown A, Hendon D, et al. Testing the relationship between Holocene peatland palaeoclimate reconstructions and instrumental data at two European sites. Quaternary Science Reviews, 2004, 23: 137-143
[43] Hendon D, Charman DJ. High-resolution peatland water-table changes for the past 200 years: The influence of climate and implications for management. Holocene, 2004, 14: 125-134

多指标记录的1962—2008年长白山园池泥炭地地表湿度变化

The variations of surface wetness recorded by multi-proxies in Yuanchi peatland of the Changbai Mountains from 1962 to 2008

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