IsoLife – Stable Isotope Labelled Plant Products for the Life Sciences

Applications  |  Ecology: Forest Burnings and Cellulose Decomposers

RNA-SIP of cellulose decomposers after forest burnings

Introduction

Regular burning as a forest management tool to improve short-term benefits may strongly affect below-ground micro-organisms and soil carbon cycling in ecosystems. Although analysis of soil microbial communities by direct soil DNA extraction from the treated forest plots and subsequent DGGE demonstrated that basidiomycete communities altered significantly (Bastias et al, 2006), no information is obtained about the fungal species involved and about the functional significance of these changes. This requires knowledge about how major functional groups like cellulose decomposers are affected. However, identification of the relevant members of these groups is not easy and only recently feasible (Bastias, 2009).

Stable Isotope Solution : 13C-cellulose

Stable Isotope Probing offers a more direct means to identify cellulolytic fungi than cultivation-based methods. Furthermore, RNA-SIP seems a more sensitive method then DNA-SIP because of the higher rates of RNA-synthesis (Manefield et al, 2002). Bastias et al (2009) has used 13C-cellulose (IsoLife BV) to study the effects of prescribed burning of forests on the occurrence of cellulose decomposers. The authors have added 13C-cellulose to soils of forests plots with a prescribed biennial burning since 1972 and compared these plots with unburned plots. The soils were incubated for more than a month and subsequently RNA-SIP was applied followed by DGGE to determine the effect of burning on cellulolytic fungi to be identified by the incorporation of 13C. DGGE bands were subsequently analyzed with Canonical Analysis of Principle coordinates (CAP). The sequences of several DGGE-bands were obtained and analysed with FastA, a program that compared the input DNA sequence to all of the sequences in the EMBL-database and reported the best matched sequences.

Results

The DGGE showed that all 12C and 13C fractions in the unburned plots had complex profiles (Figure 1a), but in the 2-yr-burn plots the 13C-fraction contained only 5 discrete bands (Figure 1b).

Figure 1. DGGE patterns from soil RNA extracts following incubation with 13C-cellulose (A unburned plots, B 2-yr burn plots) (Bastias et al, 2009).

Ordination by CAP indicated that DGGE profiles for both 12C and 13C fractions from the 2-yr burn plot differed significantly (P=0.04) from those of the unburned plot (Figure 2).

Figure 2. Canonical analysis of the DGGE-patterns (unburned: triangles; 2-yr burn: squares; closed symbols: 12C; open symbols: 13C) (Bastias et al, 2009).

Sequencing some of the DGGE-bands and analysis with FastA yielded several matches (Table 1).

Table 1. Closest FastA matches of sequenced DGGE bands from 2-yr burn plots with sequence in the EMBL database (band numbers correspond to numbers in Figure 1b).
Band no
Size (bp)
FastA closest match
Sequence similarity (%)
Overlap (bp)
1
173
Metarhizium anisopliae
93
162
2
150
Cryptococcus podzolicus
99
138
3
177
Monacrosporium sichuanense
83
179
4
220
Monacrosporium sichuanense
92
220
5
152
Cryptococcus sp
93
145
6
145
Cryptococcus humicolus
99
134
7
219
Monacrosporium ellipsosporum
75
167

The fewer bands in the DDGE-profiles for the 13C fractions suggest that fewer active fungi incorporated 13C from the labelled cellulose and indicate a reduced diversity of cellulolytic soil fungi. Some fungi that were able to use the 13C-cellulose or its 13C-degradation products were identified as Cryptococcus podzolicus, Crypotococcus humicolus and Metarhizium anisopliae. Bastias et al (2009) therefore concluded that repeated burning since 1972 significantly altered the soil fungal community. This conclusion is in line with Waldrop and Harden’s (2008) conclusion that wildfires affect fungal abundance and subsequent lignin decomposition rates.

References

Bastias BA, ZQ Huang, T Blumfeld, ZH Xu, JWG Cairney. 2006.
Influence of repeated prescribed burning on the soil fungal community in an eastern Australian wet sclerophyll forest.
Soil Biology & Biochemistry 38: 3492-3501.

Manefield M, AS Whiteley, RI Griffiths, MR Bailey. 2002.
RNA stable isotope probing, a novel means of linking microbial community function to phylogeny.
Environmental Microbiology 68: 5367-5373.

Bastias BA, IA Anderson, J Ignacio-Castro, PI Parkin, JI Prosser, JWG Cairney. 2009.
Influence of repeated prescribed burning on incorporation of 13C from cellulose by forest soil fungi as determined by RNA stable isotope probing.
Soil Biology & Biochemistry 41: 467-472. doi:10.1016/j.soilbio.2008.11.018

Waldrop MP, JW Harden. 2008.
Interactive effects of wildfire and permafrost on microbial communities and soil processes in an Alaskan black spruce forest.
Global Change Biology 14: 1-12.