DYNAMICS OF LEAF LITTER STRUCTURAL COMPOUNDS IN C. SATIVA AND P. PINASTER FOREST ECOSYSTEMS DURING THE DECOMPOSITION PROCESS: INTERACTIONS WITH SOIL ORGANIC MATTER AND NUTRIENT RELEASE

1999 ◽  
pp. 161-166 ◽  
Author(s):  
A. Martins ◽  
S. Azevedo ◽  
L. Carvalho
2010 ◽  
Vol 42 (2) ◽  
pp. 220-233 ◽  
Author(s):  
Karen Vancampenhout ◽  
Bruno De Vos ◽  
Katinka Wouters ◽  
Hans Van Calster ◽  
Rudy Swennen ◽  
...  

2007 ◽  
Vol 39 (5) ◽  
pp. 1202-1205 ◽  
Author(s):  
Andrew J. Rawlins ◽  
Ian D. Bull ◽  
Philip Ineson ◽  
Richard P. Evershed

2006 ◽  
Vol 52 (8) ◽  
pp. 701-716 ◽  
Author(s):  
T Osono

The ecology of endophytic and epiphytic phyllosphere fungi of forest trees is reviewed with special emphasis on the development of decomposer fungal communities and decomposition processes of leaf litter. A total of 41 genera of phyllosphere fungi have been reported to occur on leaf litter of tree species in 19 genera. The relative proportion of phyllosphere fungi in decomposer fungal communities ranges from 2% to 100%. Phyllosphere fungi generally disappear in the early stages of decomposition, although a few species persist until the late stages. Phyllosphere fungi have the ability to utilize various organic compounds as carbon sources, and the marked decomposing ability is associated with ligninolytic activity. The role of phyllosphere fungi in the decomposition of soluble components during the early stages is relatively small in spite of their frequent occurrence. Recently, the roles of phyllosphere fungi in the decomposition of structural components have been documented with reference to lignin and cellulose decomposition, nutrient dynamics, and accumulation and decomposition of soil organic matter. It is clear from this review that several of the common phyllosphere fungi of forest trees are primarily saprobic, being specifically adapted to colonize and utilize dead host tissue, and that some phyllosphere fungi with marked abilities to decompose litter components play important roles in decomposition of structural components, nutrient dynamics, and soil organic matter accumulation.Key words: carbon cycle, community, endophyte, epiphyte, succession.


EDIS ◽  
2007 ◽  
Vol 2007 (20) ◽  
Author(s):  
Yoana C. Newman ◽  
David L. Wright ◽  
Cheryl Mackowiak ◽  
J.M.S. Scholberg ◽  
C. M. Cherr

SS-AGR-272, a 4-page fact sheet by Y.C. Newman, D.W. Wright, C. Mackowiak, J.M.S. Scholberg and C.M. Cherr, discusses the benefits of cover crops in agricultural production, the benefits of soil organic matter; how to match cover crop nutrient release with future crop demand; timing and depth of residue incorporation; and erosion, pest and weed control. Includes references. Published by the UF Department of Agronomy, November 2007. SS AGR 272/AG277: Benefits of Cover Crops for Soil Health (ufl.edu)


2018 ◽  
Vol 106 (2) ◽  
pp. 502-513 ◽  
Author(s):  
Luke M. Jacobs ◽  
Benjamin N. Sulman ◽  
Edward R. Brzostek ◽  
John J. Feighery ◽  
Richard P. Phillips

2014 ◽  
Author(s):  
Lori D Bothwell ◽  
Paul C Selmants ◽  
Christian P Giardina ◽  
Creighton M. Litton

Decomposing litter in forest ecosystems supplies nutrients to plants, carbon to heterotrophic soil microorganisms and is a large source of CO2 to the atmosphere. Despite its essential role in carbon and nutrient cycling, the temperature sensitivity of leaf litter decay in tropical forest ecosystems remains poorly resolved, especially in tropical montane wet forests where the warming trend may be amplified compared to tropical wet forests at lower elevations. We quantified leaf litter decomposition rates along a highly constrained 5.2 °C mean annual temperature (MAT) gradient in tropical montane wet forests on the Island of Hawaii. Dominant vegetation, substrate type and age, soil moisture, and disturbance history are all nearly constant across this gradient, allowing us to isolate the effect of rising MAT on leaf litter decomposition and nutrient release. Leaf litter decomposition rates were a positive linear function of MAT, causing the residence time of leaf litter on the forest floor to decline by ~31 days for each 1 °C increase in MAT. Our estimate of the Q10 temperature coefficient for leaf litter decomposition was 2.17, within the commonly reported range for heterotrophic organic matter decomposition (1.5 – 2.5) across a broad range of ecosystems. The percentage of leaf litter nitrogen (N) remaining after six months declined linearly with increasing MAT from ~ 88% of initial N at the coolest site to ~74% at the warmest site. The lack of net N immobilization during all three litter collection periods at all MAT plots indicates that N was not limiting to leaf litter decomposition, regardless of temperature. These results suggest that leaf litter decay in tropical montane wet forests may be more sensitive to rising MAT than in tropical lowland wet forests, and that increased rates of N release from decomposing litter could delay or prevent progressive N limitation to net primary productivity with climate warming.


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