Related Experiment Video
Updated: Jan 29, 2026

10:12
The MPLEx Protocol for Multi-omic Analyses of Soil Samples
Published on: May 30, 2018
11.7K
Multi-omics reveals nitrogen dynamics associated with soil microbial blooms during snowmelt
Patrick O Sorensen1,2, Ulas Karaoz3, Harry R Beller3
1Department of Natural Resources Science, University of Rhode Island, Kingston, RI, USA. patrick.sorensen@uri.edu.
Nature Microbiology
|January 27, 2026
Summary
Snowmelt causes soil microbes to bloom and crash, impacting nitrogen export. Microbial biomass recycling and specific bacteria drive these nitrogen cycling processes in high-elevation watersheds.
Area of Science:
- Environmental Microbiology
- Biogeochemistry
- Ecology
Background:
- Soil microbial communities drive nitrogen cycling, influencing ecosystem function.
- Snowmelt dynamics significantly impact soil nitrogen availability and export in high-elevation regions.
- Global climate change is altering snowpack, necessitating a better understanding of soil nitrogen processes.
Purpose of the Study:
- To elucidate the microbial mechanisms governing nitrogen cycling during snowmelt in high-elevation watersheds.
- To identify key microbial players and their functional roles in nitrogen transformations.
- To predict soil nitrogen dynamics under declining snowpack conditions.
Main Methods:
- Integration of genome-resolved metagenomics, metatranscriptomics, and metabolomics.
- Analysis of soil microbial communities and their nitrogen cycling gene expression.
- Characterization of dissolved organic nitrogen molecular properties and transformations.
Main Results:
- Distinct soil microorganisms were identified with unique nitrogen cycling capacities during snowmelt.
- Degradation/recycling of microbial biomass supplied nitrogen for biosynthesis during bloom.
- Winter-adapted Bradyrhizobia spp. were key in anaerobic amino acid oxidation and denitrification.
- Spring-adapted Nitrososphaerales drove a nitrate pulse, with significant nitrate retention potential via dissimilatory nitrate reduction to ammonia (DNRA).
Conclusions:
- Microbial biomass dynamics and specific microbial groups critically regulate nitrogen cycling during snowmelt.
- Understanding these microbial processes is crucial for predicting nitrogen export in snow-dominated ecosystems facing climate change.
- The study provides insights into microbial N cycling in sensitive high-elevation environments.
Related Concept Videos
The Soil Ecosystem
24.7K
Plants obtain inorganic minerals and water from the soil, which acts as a natural medium for land plants. The composition and quality of soil depend not only on the chemical constituents but also on the presence of living organisms. In general, soils contain three major components:
24.7K
The Nitrogen Cycle
60.1K
Nitrogen atoms, present in all proteins and DNA, are recycled between abiotic and biotic components of the ecosystem. However, the primary form of nitrogen on Earth is nitrogen gas, which cannot be used by most animals and plants. Thus, nitrogen gas must first be converted into a usable form by nitrogen-fixing bacteria before it can be cycled through other living organisms. The use of nitrogen-containing fertilizers and animal waste products in human agriculture has greatly influenced the...
60.1K
Overview of Nitrogen Metabolism
11.4K
Nitrogen is a very important element for life because it is a major constituent of proteins and nucleic acids. It is a macronutrient, and in nature, it is recycled from organic compounds and stored in the form of ammonia, ammonium ions, nitrate, nitrite, or nitrogen gas by many metabolic processes. Many of these metabolic processes are carried out only by prokaryotes.
The largest pool of nitrogen available in the terrestrial ecosystem is gaseous nitrogen (N2) from the air, but this...
The largest pool of nitrogen available in the terrestrial ecosystem is gaseous nitrogen (N2) from the air, but this...
11.4K
Inorganic Nitrogen Assimilation
520
Nitrogen is an essential element in biological systems, forming a crucial component of proteins, nucleic acids, and other cellular constituents. Many bacteria and archaea acquire nitrogen in the form of nitrate (NO₃⁻) or ammonia (NH₃), which are then assimilated into biomolecules through specific enzymatic pathways.Assimilatory Nitrate ReductionWhen nitrate enters the cell, it undergoes a two-step reduction process known as assimilatory nitrate reduction. Initially, the enzyme...
520
Chirality at Nitrogen, Phosphorus, and Sulfur
7.0K
Chirality is most prevalent in carbon-based tetrahedral compounds, but this important facet of molecular symmetry extends to sp3-hybridized nitrogen, phosphorus and sulfur centers, including trivalent molecules with lone pairs. Here, the lone pair behaves as a functional group in addition to the other three substituents to form an analogous tetrahedral center that can be chiral.
A consequence of chirality is the need for enantiomeric resolution. While this is theoretically possible for all...
A consequence of chirality is the need for enantiomeric resolution. While this is theoretically possible for all...
7.0K
Microbial Morphologies
2.3K
Bacterial and archaeal cells exhibit remarkable diversity in shape and structure, critical in their adaptability and functionality. Among bacteria, the most commonly observed shapes include cocci and bacilli. Cocci are spherical and may exist singly or in groupings such as pairs (diplococci), chains (streptococci), clusters (staphylococci), or tetrads. Bacilli, in contrast, are rod-shaped and can also occur as single cells, in pairs, or chains, depending on their environmental and genetic...
2.3K

