Fine roots and mycorrhizal fungi accelerate leaf litter decomposition in a northern hardwood forest regardless of dominant tree mycorrhizal associations

2020 ◽  
Author(s):  
Ashley K. Lang ◽  
Fiona V. Jevon ◽  
Corinne R. Vietorisz ◽  
Matthew P. Ayres ◽  
Jaclyn Hatala Matthes

1998 ◽  
Vol 28 (9) ◽  
pp. 1365-1372 ◽  
Author(s):  
Patrick J McHale ◽  
Myron J Mitchell ◽  
Francis P Bowles

The response of trace gas fluxes (CO2, CH4, and N2O) and litter decomposition to increased soil temperature was evaluated in a northern hardwood forest. Four experimental plots (10 × 10 m) had heating cables installed within the forest floor. Temperatures at 5 cm were increased 2.5, 5.0, or 7.5°C in individual heated plots during the field season in 1993 and 1994. The fourth plot was a cabled, nonheated reference. Trace gas fluxes were monitored using closed chambers. Soil moisture was monitored using tensiometers and time domain reflectometry. Changes in leaf litter decomposition were quantified using litter bags for American beech (Fagus grandifolia Ehrh.) and sugar maple (Acer saccharum Marsh.) litter. Fluxes of CO2 increased exponentially with increased soil temperatures within treatments and were higher in heated plots than in the reference plot. Temperature coefficients (Q10) and mass remaining of American beech leaf litter decreased with the level of heating, suggesting a nonlinear microbial response to elevated temperatures. Soil water content exhibited the most influence on CH4 and N2O flux in the second season. The experimental manipulations showed the importance of evaluating the influence of soil temperature coupled with effects of N and moisture availability.



Ecosystems ◽  
2015 ◽  
Vol 19 (1) ◽  
pp. 87-97 ◽  
Author(s):  
Gary M. Lovett ◽  
Mary A. Arthur ◽  
Katherine F. Crowley




Ecology ◽  
1992 ◽  
Vol 73 (3) ◽  
pp. 1094-1104 ◽  
Author(s):  
Ronald L. Hendrick ◽  
Kurt S. Pregitzer


2002 ◽  
Vol 32 (9) ◽  
pp. 1692-1697 ◽  
Author(s):  
Geraldine L Tierney ◽  
Timothy J Fahey

We examined fine root turnover using both the minirhizotron and radiocarbon methods within the organic horizon of a northern hardwood forest to better understand discrepancies in turnover estimates obtained using these methods. The recently developed radiocarbon method estimates the mean age of organic matter by comparing its radiocarbon content to recorded atmospheric radiocarbon levels, which peaked in the 1960s as a result of thermonuclear weapons testing. The radiocarbon content of fine roots harvested from minirhizotron tubes did not differ from that of roots collected from the soil, suggesting these two methods sampled the same population of fine roots. However, long-term observation of fine root survivorship using minirhizotrons showed that root age distribution is positively skewed, causing systematic overestimation of fine root turnover by the minirhizotron method and underestimation by the radiocarbon method. We developed a parametric regression model of fine root survivorship. Our estimate of fine root turnover (about 30% per year) using this variation of the minirhizotron method was supported by radiocarbon data considered in conjunction with fine root age distribution.



1988 ◽  
Vol 149 (2) ◽  
pp. 203-208 ◽  
Author(s):  
Thomas W. Jurik ◽  
James A. Weber ◽  
David M. Gates


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