Temperature sensitivity of CO₂ and CH₄ fluxes from coarse woody debris in northern boreal forests

verfasst von

Liudmila Mukhortova, Natalia Pashenova, Maria Meteleva, Leonid Krivobokov, Georg Guggenberger

Abstract

Carbon dioxide (CO₂) and methane (CH₄) are recognized as the main greenhouse gases causing climate warming. In forest ecosystems, the death of trees leads to the formation of coarse woody debris (CWD) that is one of the sources of greenhouse gas emissions due to wood decomposi-tion. We quantified the CO₂ and CH₄ fluxes from CWD of larch (Larix gmelinii (Rupr.)) and birch (Betula tortuosa Ledeb.) collected in the northern boreal forests of Central Siberia. The CWD samples were incubated at +5, +15 and +25^◦ C. The CO₂ and CH₄ fluxes showed strong correlations with temperature, moisture, decomposition stage and the type of wood’s rot. The temperature coefficient Q₁₀ indicated higher temperature sensitivity of CO₂ flux within the temperature interval from +5 to +15^◦ C than from +15 to +25^◦ C. Methane flux had higher temperature sensitivity within the interval from +15 to +25^◦ C. It was found that, in boreal forests, CWD of early decay stage can serve as a source of methane to the atmosphere when air temperatures increased above +15^◦ C. Strong positive correlation between CH₄ production and CO₂ emission indicated a biological source and supported findings on aerobic origin of the main process contributing to the CH₄ flux from decomposing CWD.

Organisationseinheit(en)

Institut für Bodenkunde
AG Bodenchemie

Externe Organisation(en)

Russian Academy of Sciences (RAS)

Typ

Artikel

Journal

FORESTS

Band

12

ISSN

1999-4907

Publikationsdatum

14.05.2021

Publikationsstatus

Veröffentlicht

Peer-reviewed

Ja

ASJC Scopus Sachgebiete

Forstwissenschaften

Ziele für nachhaltige Entwicklung

SDG 13 – Klimaschutzmaßnahmen

Elektronische Version(en)

https://doi.org/10.3390/f12050624 (Zugang: Offen)