Potential Activity of Subglacial Microbiota Transported to Anoxic River Delta Sediments
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F17%3A10360625" target="_blank" >RIV/00216208:11310/17:10360625 - isvavai.cz</a>
Výsledek na webu
<a href="http://dx.doi.org/10.1007/s00248-016-0926-2" target="_blank" >http://dx.doi.org/10.1007/s00248-016-0926-2</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1007/s00248-016-0926-2" target="_blank" >10.1007/s00248-016-0926-2</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Potential Activity of Subglacial Microbiota Transported to Anoxic River Delta Sediments
Popis výsledku v původním jazyce
The Watson River drains a portion of the SW Greenland ice sheet, transporting microbial communities from subglacial environments to a delta at the head of Sondre Stromfjord. This study investigates the potential activity and community shifts of glacial microbiota deposited and buried under layers of sediments within the river delta. A long-term (12-month) incubation experiment was established using Watson River delta sediment under anaerobic conditions, with and without CO2/H-2 enrichment. Within CO2/H-2-amended incubations, sulphate depletion and a shift in the microbial community to a 52% predominance of Desulfosporosinus meridiei by day 371 provides evidence for sulphate reduction. We found evidence of methanogenesis in CO2/H-2-amended incubations within the first 5 months, with production rates of similar to 4 pmol g(-1) d(-1), which was likely performed by methanogenic Methanomicrobiales-and Methanosarcinales-related organisms. Later, a reduction in methane was observed to be paired with the depletion of sulphate, and we hypothesise that sulphate reduction out competed hydrogenotrophic methanogenesis. The structure and diversity of the original CO2/H-2-amended incubation communities changed dramatically with a major shift in predominant community members and a decline in diversity and cell abundance. These results highlight the need for further investigations into the fate of subglacial microbiota within downstream environments.
Název v anglickém jazyce
Potential Activity of Subglacial Microbiota Transported to Anoxic River Delta Sediments
Popis výsledku anglicky
The Watson River drains a portion of the SW Greenland ice sheet, transporting microbial communities from subglacial environments to a delta at the head of Sondre Stromfjord. This study investigates the potential activity and community shifts of glacial microbiota deposited and buried under layers of sediments within the river delta. A long-term (12-month) incubation experiment was established using Watson River delta sediment under anaerobic conditions, with and without CO2/H-2 enrichment. Within CO2/H-2-amended incubations, sulphate depletion and a shift in the microbial community to a 52% predominance of Desulfosporosinus meridiei by day 371 provides evidence for sulphate reduction. We found evidence of methanogenesis in CO2/H-2-amended incubations within the first 5 months, with production rates of similar to 4 pmol g(-1) d(-1), which was likely performed by methanogenic Methanomicrobiales-and Methanosarcinales-related organisms. Later, a reduction in methane was observed to be paired with the depletion of sulphate, and we hypothesise that sulphate reduction out competed hydrogenotrophic methanogenesis. The structure and diversity of the original CO2/H-2-amended incubation communities changed dramatically with a major shift in predominant community members and a decline in diversity and cell abundance. These results highlight the need for further investigations into the fate of subglacial microbiota within downstream environments.
Klasifikace
Druh
J<sub>imp</sub> - Článek v periodiku v databázi Web of Science
CEP obor
—
OECD FORD obor
10618 - Ecology
Návaznosti výsledku
Projekt
<a href="/cs/project/GJ15-17346Y" target="_blank" >GJ15-17346Y: Světlé zítřky subglaciálních ekosystémů: Dopady odledňování na mikrobiální aktivitu a koloběh uhlíku pod ledovci</a><br>
Návaznosti
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)
Ostatní
Rok uplatnění
2017
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Microbial Ecology
ISSN
0095-3628
e-ISSN
—
Svazek periodika
74
Číslo periodika v rámci svazku
1
Stát vydavatele periodika
US - Spojené státy americké
Počet stran výsledku
4
Strana od-do
6-9
Kód UT WoS článku
000403255500002
EID výsledku v databázi Scopus
2-s2.0-85008698564