Microbes in nature are limited by carbon and energy: the starving-survival lifestyle in soil and consequences for estimating microbial rates

被引:151
作者
Hobbie, John E. [1 ]
Hobbie, Erik A. [2 ]
机构
[1] Marine Biol Lab, Ctr Ecosyst, Woods Hole, MA 02543 USA
[2] Univ New Hampshire, Earth Syst Res Ctr, Durham, NH 03824 USA
基金
美国国家科学基金会;
关键词
microbes; soil; water; activity; labeled substrate; amino acids; sugars; FREE AMINO-ACIDS; DISSOLVED ORGANIC NITROGEN; SURFACE WATERS; FOREST SOILS; GLUCOSE; MINERALIZATION; PLANTS; GROWTH; DYNAMICS; ASSIMILATION;
D O I
10.3389/fmicb.2013.00324
中图分类号
Q93 [微生物学];
学科分类号
071005 ; 100705 ;
摘要
Understanding microbial transformations in soils is important for predicting future carbon sequestration and nutrient cycling. This review questions some methods of assessing one key microbial process, the uptake of labile organic compounds. First, soil microbes have a starving-survival life style of dormancy, arrested activity, and low activity. Yet they are very abundant and remain poised to completely take up all substrates that become available. As a result, dilution assays with the addition of labeled substrates cannot be used. When labeled substrates are transformed into (CO2)-C-14, the first part of the biphasic release follows metabolic rules and is not affected by the environment. As a consequence, when identical amounts of isotopically substrates are added to soils from different climate zones, the same percentage of the substrate is respired and the same half-life of the respired 14CO2 from the labeled substrate is estimated. Second, when soils are sampled by a variety of methods from taking 10 cm diameter cores to millimeter-scale dialysis chambers, amino acids (and other organic compounds) appear to be released by the severing of fine roots and mycorrhizal networks as well as from pressing or centrifuging treatments. As a result of disturbance as well as of natural root release, concentrations of individual amino acids of 10 M are measured. This contrasts with concentrations of a few nanomolar found in aquatic systems and raises questions about possible differences in the bacterial strategy between aquatic and soil ecosystems. The small size of the hyphae (2-10 rim diameter) and of the fine roots (0.2-2 mm diameter), make it very difficult to sample any volume of soil without introducing artifacts. Third, when micromolar amounts of labeled amino acids are added to soil, some of the isotope enters plant roots. This may be an artifact of the high micromolar concentrations applied.
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页数:11
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共 77 条
  • [61] Growth of saprotrophic fungi and bacteria in soil
    Rousk, Johannes
    Baath, Erland
    [J]. FEMS MICROBIOLOGY ECOLOGY, 2011, 78 (01) : 17 - 30
  • [62] Lack of Correlation between Turnover of Low-Molecular-Weight Dissolved Organic Carbon and Differences in Microbial Community Composition or Growth across a Soil pH Gradient
    Rousk, Johannes
    Brookes, Philip C.
    Glanville, Helen C.
    Jones, David L.
    [J]. APPLIED AND ENVIRONMENTAL MICROBIOLOGY, 2011, 77 (08) : 2791 - 2795
  • [63] Loss of low molecular weight dissolved organic carbon (DOC) and nitrogen (DON) in H2O and 0.5 M K2SO4 soil extracts
    Rousk, Johannes
    Jones, Davey L.
    [J]. SOIL BIOLOGY & BIOCHEMISTRY, 2010, 42 (12) : 2331 - 2335
  • [64] Carbon use efficiency of microbial communities: stoichiometry, methodology and modelling
    Sinsabaugh, Robert L.
    Manzoni, Stefano
    Moorhead, Daryl L.
    Richter, Andreas
    [J]. ECOLOGY LETTERS, 2013, 16 (07) : 930 - 939
  • [65] Bacterial utilization of dissolved glucose in the upper water column of the Gulf of Mexico
    Skoog, A
    Biddanda, B
    Benner, R
    [J]. LIMNOLOGY AND OCEANOGRAPHY, 1999, 44 (07) : 1625 - 1633
  • [66] Ecosystem partitioning of 15N-glycine after long-term climate and nutrient manipulations, plant clipping and addition of labile carbon in a subarctic heath tundra
    Sorensen, Pernille Laerkedal
    Michelsen, Anders
    Jonasson, Sven
    [J]. SOIL BIOLOGY & BIOCHEMISTRY, 2008, 40 (09) : 2344 - 2350
  • [67] EPIDERMAL AMINO-ACID TRANSPORT IN MARINE-INVERTEBRATES
    STEPHENS, GC
    [J]. BIOCHIMICA ET BIOPHYSICA ACTA, 1988, 947 (01) : 113 - 138
  • [68] Dynamics of simple carbon compounds in two forest soils as revealed by soil solution concentrations and biodegradation kinetics
    van Hees, P. A. W.
    Johansson, E.
    Jones, D. L.
    [J]. PLANT AND SOIL, 2008, 310 (1-2) : 11 - 23
  • [69] Control of amino acid mineralization and microbial metabolism by temperature
    Vinolas, LC
    Vallejo, VR
    Jones, DL
    [J]. SOIL BIOLOGY & BIOCHEMISTRY, 2001, 33 (7-8) : 1137 - 1140
  • [70] Soil amino acid composition across a boreal forest successional sequence
    Werdin-Pfisterer, Nancy R.
    Kielland, Knut
    Boone, Richard D.
    [J]. SOIL BIOLOGY & BIOCHEMISTRY, 2009, 41 (06) : 1210 - 1220