NARA Discovery
Article Details
← Back to Search Results
Journal Article

Elevated CO 2 increases the long‐term decomposition rate of Quercus myrtifolia leaf litter

MYRA C. HALL; PETER STILING; DANIEL C. MOON; BERT G. DRAKE; MARK D. HUNTER
Global Change Biology · Vol. 12, Issue 3 · pp. 568-577 · 2006

Abstract

Decomposition of Quercus myrtifolia leaf litter in a Florida scrub oak community was followed for 3 years in two separate experiments. In the first experiment, we examined the effects CO 2 and herbivore damage on litter quality and subsequent decomposition. Undamaged, chewed and mined litter generated under ambient and elevated (ambient+350 ppm V) CO 2 was allowed to decompose under ambient conditions for 3 years. Initial litter chemistry indicated that CO 2 levels had minor effects on litter quality. Litter damaged by leaf miners had higher initial concentrations of condensed tannins and nitrogen (N) and lower concentrations of hemicellulose and C : N ratios compared with undamaged and chewed litter. Despite variation in litter quality associated with CO 2 , herbivory, and their interaction, there was no subsequent effect on rates of decomposition under ambient atmospheric conditions. In the second experiment, we examined the effects of source (ambient and elevated) of litter and decomposition site (ambient and elevated) on litter decomposition and N dynamics. Litter was not separated by damage type. The litter from both elevated and ambient CO 2 was then decomposed in both elevated and ambient CO 2 chambers. Initial litter chemistry indicated that concentrations of carbon (C), hemicellulose, and lignin were higher in litter from elevated than ambient CO 2 chambers. Despite differences in C and fiber concentrations, litter from ambient and elevated CO 2 decomposed at comparable rates. However, the atmosphere in which the decomposition took place resulted in significant differences in rates of decomposition. Litter decomposing under elevated CO 2 decomposed more rapidly than litter under ambient CO 2 , and exhibited higher rates of mineral N accumulation. The results suggest that the atmospheric conditions during the decomposition process have a greater impact on rates of decomposition and N cycling than do the atmospheric conditions under which the foliage was produced.

Bibliographic Information

JournalGlobal Change Biology
PublisherWiley
Publication Date2006-03-01
Publication Year2006
Volume12
Issue3
Pages568-577
Document TypeJournal Article
Print ISSN1354-1013
eISSN1365-2486
DOI10.1111/j.1365-2486.2006.01119.x
SubjectConservation Science

Access Information

NARA Access Coverage1997-01-01~Current
Journal Homepagehttps://onlinelibrary.wiley.com/loi/13652486
Publisher PageOpen Publisher Page
Full-text access depends on NARA's subscribed coverage and institutional access.