Related Experiment Video
Updated: May 6, 2026

Estimating Sediment Denitrification Rates Using Cores and N2O Microsensors
Published on: December 6, 2018
Microbial biomass and activity in subsurface sediments from Vejen, Denmark
1Department of Environmental Engineering/Groundwater Research Centre, Technical University of Denmark, DK-2800, Lyngby.
Microbial populations in Quaternary glacio-fluvial sediments varied in size and activity. Sediment texture influenced bacterial numbers and mineralization rates, but no single abiotic factor explained microbial variations.
Area of Science:
- Geomicrobiology
- Quaternary geology
- Environmental microbiology
Background:
- Subsurface microbial communities play crucial roles in biogeochemical cycles.
- Understanding microbial life in geologically young sediments provides insights into early ecosystem development.
- Glacio-fluvial environments harbor unique microbial populations influenced by sediment characteristics.
Purpose of the Study:
- To characterize the microbial populations in Quaternary glacio-fluvial sediments.
- To investigate the relationships between microbial abundance, activity, and abiotic sediment parameters.
- To compare microbial data from young sediments with those from older geological formations.
Main Methods:
- Collection and analysis of subsurface sediment samples (4-31 m depth).
- Measurement of physicochemical properties: pH, electrical conductivity, chloride, organic matter, grain size.
- Quantification of microbial parameters: viable counts, acridine orange direct counts (AODC), [(3)H]-thymidine incorporation, (14)C-labelled compound mineralization.
Main Results:
- Bacterial abundance ranged from 0.5 to 1,203 x 10^3 CFU/gdw (viable) and 1.7 to 147 x 10^7 cells/gdw (AODC).
- Growth rates and mineralization rates varied significantly, with sediment texture influencing microbial numbers and activity.
- Increasing clay/silt content correlated with higher AODC and decreased mineralization; permeability correlated positively with acetate mineralization.
Conclusions:
- Sediment texture is a key factor influencing microbial populations in young glacio-fluvial sediments.
- No single abiotic parameter fully explains the variation in microbial size and activity.
- Geological age and formation type are likely important determinants of microbial community structure and function.
More Related Videos
15:23Determination of Microbial Extracellular Enzyme Activity in Waters, Soils, and Sediments using High Throughput Microplate Assays
Published on: October 1, 2013
10:30Soil Lysimeter Excavation for Coupled Hydrological, Geochemical, and Microbiological Investigations
Published on: September 11, 2016
Related Concept Videos
Deep Sea Microbial Ecology
Marine Microbial Ecology
Microbial Mats
Microbial Bioremediation of Hydrocarbons
Soil Microbial Ecology
Microbial Growth Measurement: Indirect Methods