Effects of 5-year experimental warming in the Alpine belt on soil Archaea: Multi-omics approaches and prospects

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61388971%3A_____%2F23%3A00574681" target="_blank" >RIV/61388971:_____/23:00574681 - isvavai.cz</a>

Výsledek na webu

<a href="https://ami-journals.onlinelibrary.wiley.com/doi/10.1111/1758-2229.13152" target="_blank" >https://ami-journals.onlinelibrary.wiley.com/doi/10.1111/1758-2229.13152</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1111/1758-2229.13152" target="_blank" >10.1111/1758-2229.13152</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Effects of 5-year experimental warming in the Alpine belt on soil Archaea: Multi-omics approaches and prospects

Popis výsledku v původním jazyce

We currently lack a predictive understanding of how soil archaeal communities may respond to climate change, particularly in Alpine areas where warming is far exceeding the global average. Here, we characterized the abundance, structure, and function of total (by metagenomics) and active soil archaea (by metatranscriptomics) after 5-year experimental field warming (+1 degrees C) in Italian Alpine grasslands and snowbeds. Our multi-omics approach unveiled an increasing abundance of Archaea during warming in snowbeds, which was negatively correlated with the abundance of fungi (by qPCR) and micronutrients (Ca and Mg), but positively correlated with soil water content. In the snowbeds transcripts, warming resulted in the enrichment of abundances of transcription and nucleotide biosynthesis. Our study provides novel insights into possible changes in soil Archaea composition and function in the climate change scenario.

Název v anglickém jazyce

Effects of 5-year experimental warming in the Alpine belt on soil Archaea: Multi-omics approaches and prospects

Popis výsledku anglicky

We currently lack a predictive understanding of how soil archaeal communities may respond to climate change, particularly in Alpine areas where warming is far exceeding the global average. Here, we characterized the abundance, structure, and function of total (by metagenomics) and active soil archaea (by metatranscriptomics) after 5-year experimental field warming (+1 degrees C) in Italian Alpine grasslands and snowbeds. Our multi-omics approach unveiled an increasing abundance of Archaea during warming in snowbeds, which was negatively correlated with the abundance of fungi (by qPCR) and micronutrients (Ca and Mg), but positively correlated with soil water content. In the snowbeds transcripts, warming resulted in the enrichment of abundances of transcription and nucleotide biosynthesis. Our study provides novel insights into possible changes in soil Archaea composition and function in the climate change scenario.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

10606 - Microbiology

Projekt

—

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2023

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Environmental Microbiology Reports

ISSN

1758-2229

e-ISSN

1758-2229

Svazek periodika

15

Číslo periodika v rámci svazku

4

Stát vydavatele periodika

US - Spojené státy americké

Počet stran výsledku

7

Strana od-do

291-297

Kód UT WoS článku

000961313200001

EID výsledku v databázi Scopus

2-s2.0-85152032749