Temperature sensitivity of peatland soils respiration across different terrestrial ecosystems

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In laboratory we applied Sequential (S) and Equal-time (ET) methods to assess the temperature sensitivity of peatland soils respiration across different terrestrial ecosystems: southern tundra, northern taiga, and coniferous-broadleaf forests. Q10 values varied widely (1.3–4.8) and in case of ET method decreased from northern to temperate latitudes. In the “cold” range (5–15°С), Q10 increased from the southern tundra (3.5) to the northern taiga (4.8) and then sharply decreased for the coniferous-broadleaf forests (2.5). Meanwhile, “warm” range (15–25°С) showed a clear decline of Q10 from northern to temperate latitudes: southern tundra (2.6) > northern taiga (1.6) > coniferous-broadleaf forest (1.3). Application of S method resulted in low variability of Q10 values. Our results demonstrate higher temperature sensitivity of peatland soils respiration in northern latitudes comparably to temperate ones. Q10 values obtained can be useful for calibration of regional carbon cycle datasets that consider the contribution of peatland soils.

Sobre autores

M. Tarkhov

Lomonosov Moscow State University

Autor responsável pela correspondência
Email: tarkhov.mo@gmail.com

Факультет почвоведения

Rússia, Moscow, 119991

G. Matyshak

Lomonosov Moscow State University

Email: tarkhov.mo@gmail.com

Факультет почвоведения

Rússia, Moscow, 119991

I. Ryzhova

Lomonosov Moscow State University

Email: tarkhov.mo@gmail.com

Факультет почвоведения

Rússia, Moscow, 119991

O. Goncharova

Lomonosov Moscow State University

Email: tarkhov.mo@gmail.com

Факультет почвоведения

Rússia, Moscow, 119991

S. Chuvanov

Lomonosov Moscow State University; Dokuchaev Soil Science Institute

Email: tarkhov.mo@gmail.com
Rússia, Moscow, 119991; Moscow, 119017

M. Timofeeva

Lomonosov Moscow State University; Dokuchaev Soil Science Institute

Email: tarkhov.mo@gmail.com
Rússia, Moscow, 119991; Moscow, 119017

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2. Fig. 1 Exponential dependence of the rate of mineralization of organic matter (RMOM) on temperature for samples of peat oligotrophic soils of the southern tundra (a), northern taiga (b) and the subzone of coniferous-broadleaf forests (c).

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3. Fig. 2. Exponential dependence of the microbial respiration rate (MRR) on temperature for samples of oligotrophic peat soils of the southern tundra (a), northern taiga (b) and the subzone of coniferous-broadleaf forests (c).

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