Warming affects soil metabolome: The case study of Icelandic grasslands
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F86652079%3A_____%2F21%3A00544730" target="_blank" >RIV/86652079:_____/21:00544730 - isvavai.cz</a>
Výsledek na webu
<a href="https://www.sciencedirect.com/science/article/pii/S1164556321000534?via%3Dihub#" target="_blank" >https://www.sciencedirect.com/science/article/pii/S1164556321000534?via%3Dihub#</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1016/j.ejsobi.2021.103317" target="_blank" >10.1016/j.ejsobi.2021.103317</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Warming affects soil metabolome: The case study of Icelandic grasslands
Popis výsledku v původním jazyce
The effect of warming is stronger in arctic and sub-arctic latitudes than in temperate and tropical zones. We studied soil metabolomes along two soil-warming gradients (0 to +15 degrees C). One temperature gradient has been present for at least 50 years and possibly even centuries (long-term treatment), while the second gradient was created after a shallow crustal earthquake in 2008 (short-term treatment). Soil metabolomes at the two sites responded differently to warming. At the short-term warmed site, warming of +3 degrees C already shifted soil metabolomic profiles relative to the controls, whereas at the long-term warmed site the soil metabolome only shifted at temperatures +5 degrees C. Saccharides and amino acids, primary metabolites involved in protective mechanisms against heat, were the main compounds accumulated at the highest soil warming levels. Some secondary metabolites associated with a broad spectrum of stressors, like phenolic acids and terpenes, were also up-regulated. Across the IPCC scenario's, most climate models predict a substantial rise in mean annual temperature of up to 8 degrees C in the Arctic region by the end of the 21st century. Our results suggest that temperature increases of >+5 degrees C would permanently alter soil metabolomic profile, whereas smaller temperature increases of (<+3 <degrees>C) would affect soil metabolome profile transiently, not permanently.
Název v anglickém jazyce
Warming affects soil metabolome: The case study of Icelandic grasslands
Popis výsledku anglicky
The effect of warming is stronger in arctic and sub-arctic latitudes than in temperate and tropical zones. We studied soil metabolomes along two soil-warming gradients (0 to +15 degrees C). One temperature gradient has been present for at least 50 years and possibly even centuries (long-term treatment), while the second gradient was created after a shallow crustal earthquake in 2008 (short-term treatment). Soil metabolomes at the two sites responded differently to warming. At the short-term warmed site, warming of +3 degrees C already shifted soil metabolomic profiles relative to the controls, whereas at the long-term warmed site the soil metabolome only shifted at temperatures +5 degrees C. Saccharides and amino acids, primary metabolites involved in protective mechanisms against heat, were the main compounds accumulated at the highest soil warming levels. Some secondary metabolites associated with a broad spectrum of stressors, like phenolic acids and terpenes, were also up-regulated. Across the IPCC scenario's, most climate models predict a substantial rise in mean annual temperature of up to 8 degrees C in the Arctic region by the end of the 21st century. Our results suggest that temperature increases of >+5 degrees C would permanently alter soil metabolomic profile, whereas smaller temperature increases of (<+3 <degrees>C) would affect soil metabolome profile transiently, not permanently.
Klasifikace
Druh
J<sub>imp</sub> - Článek v periodiku v databázi Web of Science
CEP obor
—
OECD FORD obor
10511 - Environmental sciences (social aspects to be 5.7)
Návaznosti výsledku
Projekt
Výsledek vznikl pri realizaci vícero projektů. Více informací v záložce Projekty.
Návaznosti
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)
Ostatní
Rok uplatnění
2021
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
European Journal of Soil Biology
ISSN
1164-5563
e-ISSN
1778-3615
Svazek periodika
105
Číslo periodika v rámci svazku
JUL-AUG
Stát vydavatele periodika
FR - Francouzská republika
Počet stran výsledku
8
Strana od-do
103317
Kód UT WoS článku
000674539100009
EID výsledku v databázi Scopus
2-s2.0-85107737759