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Global biogeography of fungal and bacterial biomass carbon in topsoil

He, Liyuan ; Mazza Rodrigues, Jorge L. ; Soudzilovskaia, Nadejda A. ; Barceló, Milagros ; Olsson, Pål Axel LU ; Song, Changchun ; Tedersoo, Leho ; Yuan, Fenghui ; Yuan, Fengming and Lipson, David A. , et al. (2020) In Soil Biology and Biochemistry 151.
Abstract

Bacteria and fungi, representing two major soil microorganism groups, play an important role in global nutrient biogeochemistry. Biogeographic patterns of bacterial and fungal biomass are of fundamental importance for mechanistically understanding nutrient cycling. We synthesized 1323 data points of phospholipid fatty acid-derived fungal biomass C (FBC), bacterial biomass C (BBC), and fungi:bacteria (F:B) ratio in topsoil, spanning 11 major biomes. The FBC, BBC, and F:B ratio display clear biogeographic patterns along latitude and environmental gradients including mean annual temperature, mean annual precipitation, net primary productivity, root C density, soil temperature, soil moisture, and edaphic factors. At the biome level, tundra... (More)

Bacteria and fungi, representing two major soil microorganism groups, play an important role in global nutrient biogeochemistry. Biogeographic patterns of bacterial and fungal biomass are of fundamental importance for mechanistically understanding nutrient cycling. We synthesized 1323 data points of phospholipid fatty acid-derived fungal biomass C (FBC), bacterial biomass C (BBC), and fungi:bacteria (F:B) ratio in topsoil, spanning 11 major biomes. The FBC, BBC, and F:B ratio display clear biogeographic patterns along latitude and environmental gradients including mean annual temperature, mean annual precipitation, net primary productivity, root C density, soil temperature, soil moisture, and edaphic factors. At the biome level, tundra has the highest FBC and BBC densities at 3684 (95% confidence interval: 1678–8084) mg kg−1 and 428 (237–774) mg kg−1, respectively; desert has the lowest FBC and BBC densities at 16.92 (14.4–19.89) mg kg−1 and 6.83 (6.1–7.65) mg kg−1, respectively. The F:B ratio varies dramatically, ranging from 1.8 (1.6–2.1) in savanna to 8.6 (6.7–11.0) in tundra. An empirical model was developed for the F:B ratio and it is combined with a global dataset of soil microbial biomass C to produce global maps for FBC and BBC in 0–30 cm topsoil. Across the globe, the highest FBC is found in boreal forest and tundra while the highest BBC is in boreal forest and tropical/subtropical forest, the lowest FBC and BBC are in shrub and desert. Global stocks of living microbial biomass C were estimated to be 12.6 (6.6–16.4) Pg C for FBC and 4.3 (0.5–10.3) Pg C for BBC in topsoil. These findings advance our understanding of the global distribution of fungal and bacterial biomass, which facilitates the incorporation of fungi and bacteria into Earth system models. The global maps of bacterial and fungal biomass serve as a benchmark for validating microbial models in simulating the global C cycle under a changing climate.

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publication status
published
subject
keywords
Bacteria, Biogeography, F:B ratio, Fungi, Pattern
in
Soil Biology and Biochemistry
volume
151
article number
108024
publisher
Elsevier
external identifiers
  • scopus:85091902923
ISSN
0038-0717
DOI
10.1016/j.soilbio.2020.108024
language
English
LU publication?
yes
id
e32f3b75-2c3d-44ed-9ea4-ee533bc7689d
date added to LUP
2020-10-28 13:35:08
date last changed
2021-01-06 02:26:34
@article{e32f3b75-2c3d-44ed-9ea4-ee533bc7689d,
  abstract     = {<p>Bacteria and fungi, representing two major soil microorganism groups, play an important role in global nutrient biogeochemistry. Biogeographic patterns of bacterial and fungal biomass are of fundamental importance for mechanistically understanding nutrient cycling. We synthesized 1323 data points of phospholipid fatty acid-derived fungal biomass C (FBC), bacterial biomass C (BBC), and fungi:bacteria (F:B) ratio in topsoil, spanning 11 major biomes. The FBC, BBC, and F:B ratio display clear biogeographic patterns along latitude and environmental gradients including mean annual temperature, mean annual precipitation, net primary productivity, root C density, soil temperature, soil moisture, and edaphic factors. At the biome level, tundra has the highest FBC and BBC densities at 3684 (95% confidence interval: 1678–8084) mg kg<sup>−1</sup> and 428 (237–774) mg kg<sup>−1</sup>, respectively; desert has the lowest FBC and BBC densities at 16.92 (14.4–19.89) mg kg<sup>−1</sup> and 6.83 (6.1–7.65) mg kg<sup>−1</sup>, respectively. The F:B ratio varies dramatically, ranging from 1.8 (1.6–2.1) in savanna to 8.6 (6.7–11.0) in tundra. An empirical model was developed for the F:B ratio and it is combined with a global dataset of soil microbial biomass C to produce global maps for FBC and BBC in 0–30 cm topsoil. Across the globe, the highest FBC is found in boreal forest and tundra while the highest BBC is in boreal forest and tropical/subtropical forest, the lowest FBC and BBC are in shrub and desert. Global stocks of living microbial biomass C were estimated to be 12.6 (6.6–16.4) Pg C for FBC and 4.3 (0.5–10.3) Pg C for BBC in topsoil. These findings advance our understanding of the global distribution of fungal and bacterial biomass, which facilitates the incorporation of fungi and bacteria into Earth system models. The global maps of bacterial and fungal biomass serve as a benchmark for validating microbial models in simulating the global C cycle under a changing climate.</p>},
  author       = {He, Liyuan and Mazza Rodrigues, Jorge L. and Soudzilovskaia, Nadejda A. and Barceló, Milagros and Olsson, Pål Axel and Song, Changchun and Tedersoo, Leho and Yuan, Fenghui and Yuan, Fengming and Lipson, David A. and Xu, Xiaofeng},
  issn         = {0038-0717},
  language     = {eng},
  publisher    = {Elsevier},
  series       = {Soil Biology and Biochemistry},
  title        = {Global biogeography of fungal and bacterial biomass carbon in topsoil},
  url          = {http://dx.doi.org/10.1016/j.soilbio.2020.108024},
  doi          = {10.1016/j.soilbio.2020.108024},
  volume       = {151},
  year         = {2020},
}