The mineralosphere—interactive zone of microbial colonization and carbon use in grassland soils
(2021) In Biology and Fertility of Soils 57(5). p.587-601- Abstract
To improve our understanding of early microbial colonization of pristine minerals and their group-specific C utilization, we exposed minerals (illite/goethite/quartz) amended with artificial root exudates (ARE, glucose, and citric acid) in grassland soils for a period of 24 weeks. FTIR spectra indicated that mineral-associated ARE were used within the first 2 weeks of exposure and were replaced by other carbohydrates derived from living or dead cells as well as soil-borne C sources transported into the mineralosphere after heavy rain events. Fungi and Gram-positive bacteria incorporated ARE-derived C more rapidly than Gram-negative bacteria. Gram-negative bacteria presumably profited indirectly from the ARE by cross-feeding on... (More)
To improve our understanding of early microbial colonization of pristine minerals and their group-specific C utilization, we exposed minerals (illite/goethite/quartz) amended with artificial root exudates (ARE, glucose, and citric acid) in grassland soils for a period of 24 weeks. FTIR spectra indicated that mineral-associated ARE were used within the first 2 weeks of exposure and were replaced by other carbohydrates derived from living or dead cells as well as soil-borne C sources transported into the mineralosphere after heavy rain events. Fungi and Gram-positive bacteria incorporated ARE-derived C more rapidly than Gram-negative bacteria. Gram-negative bacteria presumably profited indirectly from the ARE by cross-feeding on mineral-associated necromass of fungi and Gram-positive bacteria. The Gram-negative bacterial phyla Verrucomicrobia, Planctomycetes, Gemmatimonadetes, Armatimonadetes, and Chloroflexi showed a positive correlation with Gram-negative PLFA abundances. After 24 weeks of exposure in the grassland soils, abundances of soil microorganisms in the mineralosphere reached only 3.1% of the population density in soil. In conclusion, both bacteria and fungi slowly colonize new surfaces such as pristine minerals, but quickly assimilate artificial root exudates, creating an active microbial community in the mineralosphere.
(Less)
- author
- organization
- publishing date
- 2021-07-01
- type
- Contribution to journal
- publication status
- published
- subject
- keywords
- Carbon turnover, Exudates, Meadow, Minerals, Pasture, Soil microorganisms
- in
- Biology and Fertility of Soils
- volume
- 57
- issue
- 5
- pages
- 15 pages
- publisher
- Springer
- external identifiers
-
- scopus:85102561347
- ISSN
- 0178-2762
- DOI
- 10.1007/s00374-021-01551-7
- language
- English
- LU publication?
- yes
- id
- 462f3ab2-a8b8-4935-9cef-d8703d4af1cf
- date added to LUP
- 2021-03-29 10:42:12
- date last changed
- 2024-05-04 04:40:57
@article{462f3ab2-a8b8-4935-9cef-d8703d4af1cf, abstract = {{<p>To improve our understanding of early microbial colonization of pristine minerals and their group-specific C utilization, we exposed minerals (illite/goethite/quartz) amended with artificial root exudates (ARE, glucose, and citric acid) in grassland soils for a period of 24 weeks. FTIR spectra indicated that mineral-associated ARE were used within the first 2 weeks of exposure and were replaced by other carbohydrates derived from living or dead cells as well as soil-borne C sources transported into the mineralosphere after heavy rain events. Fungi and Gram-positive bacteria incorporated ARE-derived C more rapidly than Gram-negative bacteria. Gram-negative bacteria presumably profited indirectly from the ARE by cross-feeding on mineral-associated necromass of fungi and Gram-positive bacteria. The Gram-negative bacterial phyla Verrucomicrobia, Planctomycetes, Gemmatimonadetes, Armatimonadetes, and Chloroflexi showed a positive correlation with Gram-negative PLFA abundances. After 24 weeks of exposure in the grassland soils, abundances of soil microorganisms in the mineralosphere reached only 3.1% of the population density in soil. In conclusion, both bacteria and fungi slowly colonize new surfaces such as pristine minerals, but quickly assimilate artificial root exudates, creating an active microbial community in the mineralosphere.</p>}}, author = {{Boeddinghaus, Runa S. and Marhan, Sven and Gebala, Aurelia and Haslwimmer, Heike and Vieira, Selma and Sikorski, Johannes and Overmann, Jörg and Soares, Margarida and Rousk, Johannes and Rennert, Thilo and Kandeler, Ellen}}, issn = {{0178-2762}}, keywords = {{Carbon turnover; Exudates; Meadow; Minerals; Pasture; Soil microorganisms}}, language = {{eng}}, month = {{07}}, number = {{5}}, pages = {{587--601}}, publisher = {{Springer}}, series = {{Biology and Fertility of Soils}}, title = {{The mineralosphere—interactive zone of microbial colonization and carbon use in grassland soils}}, url = {{http://dx.doi.org/10.1007/s00374-021-01551-7}}, doi = {{10.1007/s00374-021-01551-7}}, volume = {{57}}, year = {{2021}}, }