Role and Variation of the Amount and Composition of Glomalin in Soil Properties in Farmland and Adjacent Plantations with Reference to a Primary Forest in North-Eastern China

被引:57
|
作者
Wang, Qiong [2 ]
Wang, Wenjie [1 ]
He, Xingyuan [2 ]
Zhang, Wentian [1 ]
Song, Kaishan [2 ]
Han, Shijie [3 ]
机构
[1] Northeast Forestry Univ, Key Lab Forest Plant Ecol, Harbin, Peoples R China
[2] Chinese Acad Sci, Northeast Inst Geog & Agr Ecol, Urban Forests & Wetlands Res Grp, Key Lab Wetland Ecol & Environm, Changchun, Peoples R China
[3] Chinese Acad Sci, Inst Appl Ecol, Res Inst Forest Ecol & Forestry Ecol Engn, Shenyang 110016, Peoples R China
来源
PLOS ONE | 2015年 / 10卷 / 10期
关键词
ARBUSCULAR MYCORRHIZAL FUNGI; DISSOLVED ORGANIC-MATTER; TEMPORAL-CHANGES; PARALLEL FACTOR; PROTEIN FILMS; CARBON; AFFORESTATION; RHIZOSPHERE; SPECTROSCOPY; ORGANIZATION;
D O I
10.1371/journal.pone.0139623
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 glycoprotein known as glomalin-related soil protein (GRSP) is abundantly produced on the hyphae and spores of arbuscular mycorrhizal fungi (AMF) in soil and roots. Few studies have focused on its amount, composition and associations with soil properties and possible land-use influences, although the data hints at soil rehabilitation. By choosing a primary forest soil as a non-degraded reference, it is possible to explore whether afforestation can improve degraded farmland soil by altering GRSP. In this paper, close correlations were found between various soil properties (soil organic carbon, nitrogen, pH, electrical conductivity (EC), and bulk density) and the GRSP amount, between various soil properties and GRSP composition (main functional groups, fluorescent substances, and elements). Afforestation on farmland decreased the EC and bulk density (p < 0.05). The primary forest had a 2.35-2.56-fold higher GRSP amount than those in the plantation forest and farmland, and GRSP composition (tryptophan-like and fulvic acid-like fluorescence; functional groups of C-H, C-O, and O-H; elements of Al, O, Si, C, Ca, and N) in primary forest differed from those in plantation forest and farmland (p < 0.05). However, no evident differences in GRSP amount and composition were observed between the farmland and the plantation forest. Our finding highlights that 30 years poplar afforestation on degraded farmland is not enough to change GRSP-related properties. A longer period of afforestation with close-to-nature managements may favor the AMF-related underground recovery processes.
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页数:19
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