Phosphorus Fractions and Arbuscular Mycorrhizal Fungi Communities in a Tropical Coarse-Textured Soil under Natural Forest and Para Rubber Ecosystems 10.32526/ennrj/20/202100188
Article Sidebar
Main Article Content
Abstract
Soil phosphorus (P) plays an essential role in rubber tree plantations that are rapidly and extensively being established in Southeast Asia. However, available information is quite limited on soil P fractions and arbuscular mycorrhizal fungi (AMF) in the tropical region. Herein, we investigated P fractions and AMF community under natural forest and rubber plantations at different ages of 5 years, 11 years, and 22 years in tropical coarse-textured soils from Thailand. The studied loamy sand soils were acidic (pH=5.0-5.7) with low available P concentrations (1.73-6.48 mg/kg). Data on the P fractions data revealed that the labile P (water-extractable Pi and NaHCO3-extractable Pi) and moderately labile P (NaOH0.1-extractable Po and HCl-extractable Pi) pools in rubber-growing soils were higher than those in the natural forest soil. Elevated values of these properties were substantial with increasing stand ages. The rubber monocropping systems declined in the density and diversity of AMF spores compared to the natural forest site. Glomus badium, Rhizophagus fasciculatus, Acaulospora Laevis, and Ambispora appendiculata were the most dominant and tolerant AMF species across the rubber stands (>50% of the total species). The P fractions and AMF were correlated with soil labile-P forms. Soil labile and moderately P fractions were the important factors affecting the difference in AMF community. This study highlighted that long-term rubber plantations in tropical ecosystems promoted labile P fraction but demoted AMF density and diversity.
Article Details
This work is licensed under a Creative Commons Attribution-NonCommercial 4.0 International License.
Published articles are under the copyright of the Environment and Natural Resources Journal effective when the article is accepted for publication thus granting Environment and Natural Resources Journal all rights for the work so that both parties may be protected from the consequences of unauthorized use. Partially or totally publication of an article elsewhere is possible only after the consent from the editors.
References
Arai Y, Sparks DL. ATR-FTIR Spectroscopic investigation on phosphate adsorption mechanisms at the ferrihydrite-water interface. Journal of Colloid and Interface Science 2001; 241:317-26.
Bhadalung NN, Suwanarit A, Dell B, Nopamornbodi O, Thamchaipenet A, Rungchuang J. Effects of long-term NP-fertilization on abundance and diversity of arbuscular mycorrhizal fungi under a maize cropping system. Plant and Soil 2005;270(1):371-82.
Blake GR, Hartge KH. Bulk density. In: Klute A, editor. Methods of Soil Analysis. Madison, WI, USA: American Society of Agronomy; 1986. p. 363-82.
Bray RH, Kurtz LT. Determination of total, organic, and available forms of phosphorus in soils. Soil Science 1945;59:39-46
Bremner JM. Total nitrogen. In: Black CA, editor. Methods of Soil Analysis. Madison, WI, USA: American Society of Agronomy; 1965. p. 1049-178.
Brookes PC, Powlson DS, Jenkinson DS. Measurement of microbial biomass phosphorus in soil. Soil Biology and Biochemistry 1982;14:319-29.
Cardoso I, Boddington C, Janssen B, Oenema O, Kuyper T. Differential access to phosphorus pools of an oxisol by mycorrhizal and nonmycorrhizal maize. Communications in Soil Science and Plant Analysis 2006;37:1537-51.
Cervantes-Gámez R, Bueno-Ibarra MA, Cruz-Mendívil A, Calderón-Vázquez CL, Ramírez-Douriet CM, Maldonado-Mendoza IE, et al. Arbuscular mycorrhizal symbiosis-induced expression changes in Solanum lycopersicum leaves revealed by RNA-seq analysis. Plant Molecular Biology Reporter 2016;34:89-102.
Chambon B, Ruf F, Kongmanee C, Angthong S. Can the cocoa cycle model explain the continuous growth of the rubber (Hevea brasiliensis) sector for more than a century in Thailand? Journal of Rural Studies 2016;44,187-97.
Chapman HD. Cation‐exchange capacity. In: Norman AG, editor. Methods of Soil Analysis. Madison, WI, USA: American Society of Agronomy; 1965. p. 891-901.
Chen CR, Condron LM, Xu ZH. Impacts of grassland afforestation with coniferous trees on soil phosphorus dynamics and associated microbial processes: A review. Forest Ecology and Management 2008;255:396-409.
Chen CR, Hou EQ, Condron LM, Bacon G, Esfandbod M, Olley J, et al. Soil phosphorus fractionation and nutrient dynamics along the Cooloola coastal dune chronosequence, Southern Queensland Australia. Geoderma 2015;(257-258):4-13.
Cherubin MR, Franco ALC, Cerri CEP, Karlen DL, Pavinato PS, Rodrigues M, et al. Phosphorus pools responses to land-use change for sugarcane expansion in weathered Brazilian soils. Geoderma 2016;265:27-38.
Condron LM, Turner BL, Cade-Menun BJ. Chemistry and dynamics of soil organic phosphorus. In: Sims JT, Sharpley AN, editors. Phosphorus: Agriculture and the Environment. Kimberly, ID, USA: American Society of Agronomy; 2005. p. 87-121.
Costa MG, Gama-Rodrigues AC, Gonçalves JL, de M Gama-Rodrigues EF, Sales MV, et al. Labile and non-labile fractions of phosphorus and its transformations in soil under eucalyptus plantations Brazil. Forests 2016;7:1-15.
Crews TE, Brookes PC. Changes in soil phosphorus forms through time in perennial versus annual agroecosystems. Agriculture, Ecosystems and Environment 2014;184:168-81.
Daniels BA, Skipper HA. Methods for the recovery and quantitative estimation of propagules from soil. In: Schenck, NC, editor. Methods and Principles of Mycorrhizal Research. St. Paul, MN, USA: American Phytopathological Society; 1982; p. 29-35.
Food and Agriculture Organization (FAO). FAOSTAT [Internet]. 2019 [cited 2020 Aug 1]. Available from: http:// www.fao.org /go/to/home/E.
Feldmann F, da Silva Jr JP, Idczak E, Lieberei R. AMF spore community composition at natural and agricultural sites in Central Amazonia-a long term study. Proceedings of German-Brazilian Workshop on Neotropical Ecosystems-Achievements and Prospects of Cooperative Research; 2000 Sep 3-8; Hamburg: Germany; 2000.
Fox J, Castella JC, Ziegler AD, Westley SB. Rubber plantations expand in mountainous Southeast Asia: What are the consequences for the environment? Asia Pacific Issues 2014; 114:1-8.
Gee GW, Bauder JW. Particle-size analysis. In: Klute A, editor. Methods of Soil Analysis. Madison, WI, USA: American Society of Agronomy; 1986. p. 383-411.
Haynes RJ, Swift RS. Effects of soil acidification and subsequent leaching on levels of extractable nutrients in a soil. Plant Soil 1986;95:327-36.
Hedley MJ, Stewart JWB, Chauhan BS. Changes in inorganic and organic soil phosphorus fractions induced by cultivation practices and by laboratory incubations. Soil Science Society of America Journal 1982;46:970-6.
Henriquez C. Assessing Soil Phosphorus Status Under Different Agronomic Land Use [dissertation]. Iowa State University; 2002.
Holford ICR. Soil phosphorus: Its measurement, and its uptake by plants. Australian Journal of Soil Research 1997;35:227-39.
Hu B, Yang B, Pang X, Bao W, Tian G. Responses of soil phosphorus fractions to gap size in a reforested spruce forest. Geoderma 2016;279:61-9.
International Rubber Study Group (IRSG). Rubber statistical bulletin, database [Internet]. 2021 [cited 2021 Aug 1]. Available from: https://www.rubberstudy.org/welcome.
Krailertrattanachai N, Ketrot D, Wisawapipat W. The distribution of trace metals in roadside agricultural soils Thailand. International Journal of Environmental Research and Public Health 2019;16(5):Article No. 714.
Kuo S. Phosphorus. In: Sparks DL, Page AL, Helmke PA, Loeppert RH, Soltanpour PN, Tabatabai MA, Johnston CT, Sumner ME, editors. Methods of Soil Analysis. Madison, Wisconsin, USA: Soil Science Society of America; 1996. p. 869-919.
Li Y, Lan G, Xia Y. Rubber trees demonstrate a clear retranslocation under seasonal drought and cold stresses. Frontiers in Plant Science 2016;7:Article No. 1907.
Liu C, Jin Y, Liu C, Tang J, Wang Q, Xu M. Phosphorous fractions in soils of rubber-based agroforestry systems: Influence of season, management and stand age. Science of the Total Environment 2018;(616-617):1576-88.
Lustosa Filho JF, de Silva Carneiro JS, Barbosa CF, de Lima KP, do Amaral Leite A, Melo LCA. Aging of biochar-based fertilizers in soil: Effects on phosphorus pools and availability to Urochloa brizantha grass. Science of the Total Environment 2020;709:Article No. 136028.
Maranguit D, Guillaume T, Kuzyakov Y. Land-use change affects phosphorus fractions in highly weathered tropical soils. Catena 2017;149:385-93.
Marlairotsiri K, Suchinai A, Hoontakul K. Characterization of Established Soil Series in the Northeast Region of Thailand Reclassified According to Soil Taxonomy 2003. Bangkok, Thailand: Land Development Department; 2004. p. 6-7.
Moreira A, Moraes LAC, Zaninetti RA, Canizella BT. Phosphorus dynamics in the conversion of a secondary forest into a rubber tree plantation in the amazon rainforest. Soil Science 2013; 178:618-25.
Nash DA, Friedman JW, Mathu-Muju KR, Robinson PG, Satur J,Moffat S, et al. A review of the global literature on dental therapists. Community Dentistry and Oral Epidemiology 2014;42:1-10.
Negassa W, Leinweber P. How does the Hedley sequential phosphorus fractionation reflect impacts of land use and management on soil phosphorus: A review. Journal of Plant Nutrition and Soil Science 2009;172:305-25.
Neufeldt H, da Silva JE, Ayarza MA, Zech W. Land-use effects on phosphorus fractions in Cerrado oxisols. Biology and Fertility of Soils 2000;31:30-7.
Rausch C, Bucher M. Molecular mechanisms of phosphate transport in plants. Planta 2002;216:23-37.
Schweiger R, Müller C. Leaf metabolome in arbuscular mycorrhizal symbiosis. Current Opinion in Plant Biology 2015;26:120-6.
Steidinger BS, Turner BL, Corrales A, Dalling JW. Variability in potential to exploit different soil organic phosphorus compounds among tropical montane tree species. Functional Ecology 2015;29:121-30.
Stutter MI, Shand CA, George TS, Blackwell MSA, Dixon L, Bol R, et al. Land use and soil factors affecting accumulation of phosphorus species in temperate soils. Geoderma 2015;(257-258):29-39.
Thai Meteorological Department. Climate data [Internet]. 2018 [cited 2021 Dec 7]. Available from: https://www.tmd.go.th/ programs/uploads/tempstat/max_stat_latest_en.pdf.
Tiessen H, Moir JO. Characterization of available P by sequential extraction. In: Carter MR, editor. Soil Sampling and Methods of Analysis. Canadian Society of Soil Science; 1993. p. 75-86.
van der Heijden MGA, Klironomos JN, Ursic M, Moutoglis P, Strietwolf Engel R, Boller T, et al. Mycorrhizal fungal diversity determines plant biodiversity, ecosystem variability and productivity. Nature 1998;74:69-72.
Wagg C, Bender SF, Widmer F, van der Heijden MGA. Soil biodiversity and soil community composition determine ecosystem multifunctionality. Proceedings of the National Academy of Sciences of the United States of America 2014;111:5266-70.
Walkley A, Black IA. An examination of the Degtjareff method for determining soil organic matter, and a proposed modification of the chromic acid titration method. Soil Science 1934;37:29-38.
Wang J, Wang GG, Zhang B, Yuan Z, Fu Z, Yuan Y, et al. Arbuscular mycorrhizal fungi associated with tree species in a planted forest of Eastern China. Forests 2019;10:1-14.
World Rubber Summit (WRS). Facing the future: Inclusiveness, sustainability and growth for the next normal [Internet]. 2021 [cited 2021 Aug 1]. Available from: https://www.wrs 2021. rubberstudy.org/.
Yang X, Post WM. Phosphorus transformations as a function of pedogenesis: A synthesis of soil phosphorus data using Hedley fractionation method. Biogeosciences 2011;8:2907-16.
Zak JC, Willig MR, Moorhead DL, Wildman HG. Functional diversity of microbial communities: A quantitative approach. Soil Biology and Biochemistry 1994;26:1101-8.
Zhang H, Kovar JL. Fractionation of soil phosphorus. In: Kovar JL, Pierzynski GM, editors. Methods for Phosphorus Analysis for Soils, Sediments, Residuals, and Waters. Southern Cooperative Series Bulletin; 2009. p. 50-60.