Structure and dynamics of organic matter pools in clearings in the lichen pine forests of middle taiga subzone of Yenisei Siberia

2013 ◽  
Vol 40 (1) ◽  
pp. 95-102 ◽  
Author(s):  
A. V. Panov ◽  
A. A. Onuchin ◽  
G. K. Zrazhevskaya ◽  
O. B. Shibistova
2021 ◽  
Vol 52 (2) ◽  
pp. 136-145
Author(s):  
S. A. Moshnikov ◽  
V. A. Anan’ev ◽  
I. V. Romashkin

2021 ◽  
Vol 101 (2) ◽  
pp. 273-281
Author(s):  
L. A. Bespyatova ◽  
S. V. Bugmyrin ◽  
S. A. Kutenkov ◽  
I. A. Nikonorova

2021 ◽  
Vol 875 (1) ◽  
pp. 012085
Author(s):  
O Sergeeva ◽  
L Mukhortova ◽  
L Krivobokov

Abstract Litter plays an important role in the carbon cycle of forest ecosystems incorporating significant amount of carbon as a result of annual partial die-off of the biomass and releasing it during complex multistage processes of organic matter decomposition. The balance of these processes in the forests of permafrost zone significantly shifts towards the accumulation of dead organic matter. That makes the assessment of litter stock in these ecosystems particularly relevant, especially in relation to the predicted consequences of climate change in the study region. On the territory of middle taiga of Central Siberia, 14 sampling plots were established in the various landforms (slopes of different exposition, lowlands and uplands). The carbon stock in litter of the main forest types of the studied area varied from 0.47 to 4.46 kgC/m2. Also, the paper considers composition of litter accumulated in these ecosystems, including the ratio between fresh litterfall, fermented and humified plant residues, and dead roots. Our results demonstrated that fermented plant residues prevailed in the litter composition in most types of studied forest ecosystems due to specificity of hydrothermal regime and quality of litterfall. The results obtained might be applied to refine the carbon budget of Siberian forests.


2021 ◽  
Vol 54 (4) ◽  
pp. 631-647
Author(s):  
I. A. Likhanova ◽  
E. G. Kuznetsova ◽  
E. M. Lapteva ◽  
S. V. Deneva ◽  
B. A. Makeev

1983 ◽  
Vol 13 (6) ◽  
pp. 1077-1082 ◽  
Author(s):  
John W. Fitzgerald ◽  
Jaru T. Ash ◽  
Timothy C. Strickland ◽  
Wayne T. Swank

The ability of soils from hardwood, clear-cut, and pine forests to incorporate sulfur from added inorganic sulfate into salt-extractable (adsorbed) and nonsalt-extractable forms was investigated. At least 65% of the added sulfate was adsorbed while 8–27% of the sulfate added was recovered only after treatment of salt-extracted samples with acid and base (nonsalt-extractable sulfur). The incorporation of sulfur into this latter fraction was dependent upon incubation time, temperature, and depth and exhibited both spatial as well as seasonal variation in samples taken along a transect of one of the watersheds. Sulfur incorporation into the nonsalt-extractable fraction was inhibited 75–87% by sodium azide, 62–84% by erythromycin, and 41–68% by candicidin suggesting that the process is mediated by bacteria and fungi. Data on factors influencing sulfur incorporation suggest that sulfate was incorporated into organic matter as a covalent linkage and released after rupture of this linkage during acid and base treatment. The observations that 35S incorporation was inhibited 93–99% by unlabelled sulfate and stimulated 21–65% by increased carbon availability are consistent with this suggestion.


2015 ◽  
Vol 46 (2) ◽  
pp. 143-151 ◽  
Author(s):  
A. V. Timokhina ◽  
A. S. Prokushkin ◽  
A. A. Onuchin ◽  
A. V. Panov ◽  
G. B. Kofman ◽  
...  

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