Characteristics of soil organic carbon fractions and influencing factors in different understory mosses in karst urban parks

被引:0
作者
Zhang, Yinfang [1 ]
Wang, Xiurong [1 ]
Zheng, Yingying [1 ]
Duan, Lixin [1 ]
机构
[1] Guizhou Univ, Coll Forestry, Guiyang, Peoples R China
来源
SCIENTIFIC REPORTS | 2024年 / 14卷 / 01期
基金
中国国家自然科学基金;
关键词
Soil organic carbon; Organic carbon fractions; Karst region; Urban parks; Moss; BRYOPHYTES; EXCHANGE; POOLS;
D O I
10.1038/s41598-024-77735-6
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
The impact of different vegetation types on soil organic carbon (SOC) is a key focus in global warming research. Bryophytes, commonly found in karst urban forests, significantly contribute to carbon accumulation in surface soil. However, the changes in soil organic carbon fractions under moss and the influencing factors remain unclear. To address this knowledge gap, the study examined the organic carbon content, soil physicochemical properties, and associated environmental factors in both moss-covered soil and bare soil under six different forest species within an urban park. The results showed that the SOC contents under moss cover in evergreen coniferous forest (127.28 g/kg), bamboo forest (144.70 g/kg), deciduous broad-leaved forest (87.63 g/kg), and evergreen shrub (109.28 g/kg) were significantly higher compared to bare soil. Moss cover also had a significant impact on soil readily oxidizable carbon (ROC), particulate organic carbon (POC), mineral-associated organic carbon (MOC), and heavy fraction organic carbon (HFOC) (P < 0.01). The soil under moss had a higher content of stable organic carbon fraction, which is conducive to the stability of the soil organic carbon pool. The interaction between moss cover and stand type had the most significant effect on soil organic carbon, especially in bamboo forests. Canopy density, moss biomass, and soil moisture were the main environmental factors affecting the content of soil organic carbon and its fractions, while soil organic carbon content was mainly affected by soil nitrogen and phosphorus. This study establishes a theoretical framework for investigating the carbon cycle in karst urban underforest ecosystems, offering a scientific basis for the management and preservation of urban green space ecosystems. Future studies should include bryophytes in the assessment of dynamic factors affecting the soil carbon pool under forest cover and further explore the function and ecological significance of bryophytes in understory ecosystems.
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页数:10
相关论文
共 62 条
  • [11] Dai L., 2021, Farm. Cultivation, V41, P47, DOI [10.13605/j.cnki.52-1065/s.2021.05.013, DOI 10.13605/J.CNKI.52-1065/S.2021.05.013]
  • [12] Dang K., 2016, Chin. J. Ecol, V36, P1030, DOI [10.5846/stxb201406271326, DOI 10.5846/STXB201406271326]
  • [13] The contribution of bryophytes to the carbon exchange for a temperate rainforest
    DeLucia, EH
    Turnbull, MH
    Walcroft, AS
    Griffin, KL
    Tissue, DT
    Glenny, D
    McSeveny, TM
    Whitehead, D
    [J]. GLOBAL CHANGE BIOLOGY, 2003, 9 (08) : 1158 - 1170
  • [14] [丁咸庆 Ding Xianqing], 2015, [水土保持学报, Journal of Soil and Water Conservation], V29, P258
  • [15] Species richness correlations among primary producers in boreal forests
    Dynesius, Mats
    Zinko, Ursula
    [J]. DIVERSITY AND DISTRIBUTIONS, 2006, 12 (06) : 703 - 713
  • [16] Contribution of cryptogamic covers to the global cycles of carbon and nitrogen
    Elbert, Wolfgang
    Weber, Bettina
    Burrows, Susannah
    Steinkamp, Joerg
    Buedel, Burkhard
    Andreae, Meinrat O.
    Poeschl, Ulrich
    [J]. NATURE GEOSCIENCE, 2012, 5 (07) : 459 - 462
  • [17] Recalcitrance of lichen and moss litters increases soil carbon storage on permafrost
    Fujii, Kazumichi
    Hayakawa, Chie
    [J]. PLANT AND SOIL, 2022, 472 (1-2) : 595 - 608
  • [18] Substrate concentration and enzyme allocation can affect rates of microbial decomposition
    German, Donovan P.
    Chacon, Stephany S.
    Allison, Steven D.
    [J]. ECOLOGY, 2011, 92 (07) : 1471 - 1480
  • [19] Golubiewski NE, 2006, ECOL APPL, V16, P555, DOI 10.1890/1051-0761(2006)016[0555:UIGCPE]2.0.CO
  • [20] 2