Distribution of microbial biomass and phospholipid fatty acids in Podzol profiles under coniferous forest

Citation
H. Fritze et al., Distribution of microbial biomass and phospholipid fatty acids in Podzol profiles under coniferous forest, EUR J SO SC, 51(4), 2000, pp. 565-573
Citations number
21
Categorie Soggetti
Agriculture/Agronomy
Journal title
EUROPEAN JOURNAL OF SOIL SCIENCE
ISSN journal
13510754 → ACNP
Volume
51
Issue
4
Year of publication
2000
Pages
565 - 573
Database
ISI
SICI code
1351-0754(200012)51:4<565:DOMBAP>2.0.ZU;2-Z
Abstract
Microbial-derived phospholipid fatty acids (PLFAs) can be used to character ize the microbial communities in soil without the need to isolate individua l fungi and bacteria. They have been used to assess microbial communities o f humus layers under coniferous forest, but nothing is known of their distr ibution in the deeper soil. To investigate the vertical distribution we sam pled nine Podzol profiles on a 100-m-long transect in a coniferous forest a nd analysed for their microbial biomass and PLFA pattern to a depth of 0.4 m. The transect covered a fertility gradient from Vaccinium vitis-idaea for est site type to Vaccinium myrtillus forest site type. The cores were divid ed into humus (O) and eluvial (E) layers and below that into 10-cm sections and designated as either illuvial (B) or parent material (C), or as a comb ination (BC). Two measures of microbial biomass analyses were applied: subs trate-induced respiration (SIR) to determine microbial biomass C (C-mic), a nd the sum of the extracted microbial-derived phospholipid fatty acids (tot PLFA). The soil fertility had no effect on the results. The C-mic correlate d well with totPLFA (r = 0.86). The microbial biomass decreased with increa sing depth. In addition the PLFA pattern changed with increased depth as as sessed with principal component analysis, indicating a change in the microb ial community structure. The composition of the PLFAs in the O layer differ ed from that in the E layer and both differed from the upper part of the B layer and from the rest of the BC layers. The deeper parts of the B layer ( BC1, BC2 and BC3) were similar to one other. The O layer had more 18:2 omeg a6, a PLFA indicator of fungi, whereas the E layer contained relatively mor e of the PLFAs 16:1 omega9, 18:1 omega7 and cy19:0 common in gram-negative bacteria. With increased depth the relative amount of 10Me18:0, the PLFA in dicator for actinomycetes, increased. We conclude that the PLFA method is a promising discriminator between the microbial community structures of the horizons in Podzols.