Calcium Oxalate Crystals in Eucalypt Ectomycorrhizae: Morphochemical Characterization
et al. (2013) Calcium Oxalate Crystals in Eucalypt Ectomycorrhizae: Morphochemical
Characterization. PLoS ONE 8(7): e67685. doi:10.1371/journal.pone.0067685
Calcium Oxalate Crystals in Eucalypt Ectomycorrhizae: Morphochemical Characterization
Victor Satler Pylro 0 1
Andre Luiz Moreira de Freitas 0 1
Wagner Campos Otoni 0 1
Ivo Ribeiro da Silva 0 1
Arnaldo Chaer Borges 0 1
Maurcio Dutra Costa 0 1
Agustin Guerrero-Hernandez, Cinvestav-IPN, Mexico
0 The experiments were performed at Mycorrhizal Associations Laboratory/BIOAGRO, Microbiology Department of Federal
1 1 Departamento de Microbiologia, Universidade Federal de Vic osa, Vic osa, Minas Gerais, Brazil, 2 Departamento de Biologia Vegetal, Universidade Federal de Vic osa, Vic osa, Minas Gerais, Brazil, 3 Departamento de Solos, Universidade Federal de Vic osa , Vic osa, Minas Gerais , Brazil
Ectomycorrhizal fungi are ubiquitous in forest ecosystems, benefitting plants principally by increasing the uptake of water and nutrients such as calcium from the soil. Previous work has demonstrated accumulation of crystallites in eucalypt ectomycorrhizas, but detailed morphological and chemical characterization of these crystals has not been performed. In this work, cross sections of acetic acid-treated and cleared ectomycorrhizal fragments were visualized by polarized light microscopy to evaluate the location of crystals within cortical root cells. Ectomycorrhizal sections were also observed by scanning electron microscopy (SEM) coupled with energy dispersive x-ray (EDS) microprobe analysis. The predominant forms of crystals were crystal sand (granules) and concretions. Calcium, carbon and oxygen were detected by EDS as constituent elements and similar elemental profiles were observed between both crystal morphologies. All analyzed crystalline structures were characterized as calcium oxalate crystals. This is the first report of the stoichiometry and morphology of crystals occurring in eucalypt ectomycorrhizas in tropical soils. The data corroborates the role of ectomycorrhizae in the uptake and accumulation of calcium in the form of calcium oxalate crystals in hybrid eucalypt plants.
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Funding: This work was funded by FAPEMIG (www.fapemig.br) grant APQ-00403-09, CNPq (www.cnpq.br), and CAPES (www.capes.gov.br). The funders had no
role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.
Competing Interests: The authors have declared that no competing interests exist.
The occurrence of calcium oxalate crystals (CaC2O4 or CaOx)
has been observed in plants of several botanical families [1], and
they contribute a large portion of the total calcium of these plants.
CaOx deposits have been described in most tissues and organs as
either intracellular (usually associated with vacuoles of specialized
cells; idioblasts) or extracellular [14] deposits. The biological
function of CaOx crystals in plants is neither completely
understood nor characterized. Several functions have been
attributed to them, largely based upon the amount, distribution
and morphology of the crystals as well as the inherent
characteristics of the cells where they are produced [1]. Some
studies imply that CaOx may serve different biological functions
such as a calcium reservoir, deposit of secondary metabolites and
sequestration of potentially toxic metal ions [5,6], formation of
aerenchyma in aquatic plants [7], providing structural support [8],
or protection against herbivory by association with stinging
substances or proteolytic toxins [911].
Eucalyptus is the most important genus of exotic plants in
Brazilian planted forests, with great economic and environmental
significance [12]. Generally, the soils under eucalypt cultivation in
Brazil are highly weathered, with pH values below 5.5, an
Aluminum saturation of 90%, and a low content of organic matter
and limiting concentrations of Phosphorus, Nitrogen and Calcium
(Ca2+) [1316]. Soil exchangeable calcium is often at or below
8 kg ha21 and insufficient to fulfil the plant demand [17]. Soil
microorganisms play an essential role in biochemical cycles and
contribute to edaphic homeostasis. In the current understanding
that biological and functional diversity is a crucial factor in
maintaining ecosystems [18] are included ectomycorrhizal fungi
associated with the roots, that benefit plants by increasing the
volume of the soil explored by roots, and thus the amount of
absorbed nutrients and water [19].
The presence of CaOx crystals in ectomycorrhizal hyphae is
limited to temperate soils containing high concentrations of
calcium [2022]. In Brazil, the number of studies aiming at
evaluating the accumulation of calcium crystals in eucalypt
ectomycorrhizae is scarce [23]. However, the existing report has
suggested a paramount role of ectomycorrhizal fungi in supplying
Ca to eucalyptus in Brazilian soils poor in Ca, since putative CaOx
crystals have been shown to be predominantly present in
ectomycorrhizae rather than in non-mycorrhizal fine roots.
Understanding the morphochemical patterns of crystalline
structures in Eucalyptus ectomycorrhizae can help generate new
information regarding the role of ectomycorrhizal fungi in Ca2+
uptake by plants. Therefore, the aim of this study was to evaluate
the location, morphology and chemical composition of crystals
present in eucalypt ectomycorrhizae.
Materials and Methods
University of Vicosa (UFV). Analyses of Scanning Electron
Microscopy (SEM) and Energy Dispersive X-ray (EDS) were
performed at the Microscopy Center of the Federal University of
Minas Gerais. All samples were processed at the Center of
Microscopy and Microanalysis at UFV.
Characterization of Sampling Site
Samples were taken from within a 2.5 year old planted stand of
clonal E. grandis X E. urophylla hybrids located in the experimental
field of UFV (20u 469 27.399 S and 42u 519 36.299 W; elevation:
697 m). Ten soil cores (2.0 cm diameter, 20 cm depth) were
collected at random points within the study area, and the cores
were combined to form a composite sample. Physicochemical
analyses (Table 1) were performed according to routine methods.
Fine lateral roots colonized by ectomycorrhizal fungi were
collected from the 010 cm layer of soil around randomly selected
trees within the plantation. The soil was excavated and the roots
were collected with fine-tipped forceps and razor blades. Samples
were placed in a moist chamber and transported to the laboratory,
for analysis.
Ectomycorrhizal Eucalypt Preparation, Acid Digestion
and Image Processing
Ectomycorrhizal samples were washed in phosphate buffer,
pH 7.0, to remove soil particles adhered to the surface, and then
dehydrated in an ethanol series [10, 30, 50, 70 and 90% ethanol
(vol/vol)] for 10 min in each solution and finally kept in 95%
ethanol (vol/vol) for 12 h. Subsequently, part of the samples was
cleared in a 1.8% (vol/vol) sodium hypochlorite solution for 1 h.
The cleared samples containing cry (...truncated)