Aphid infested Norway spruce are "hot spots" in throughfall carbon chemistry in coniferous forests

Citation
B. Stadler et B. Michalzik, Aphid infested Norway spruce are "hot spots" in throughfall carbon chemistry in coniferous forests, CAN J FORES, 28(11), 1998, pp. 1717-1722
Citations number
24
Categorie Soggetti
Plant Sciences
Journal title
CANADIAN JOURNAL OF FOREST RESEARCH-REVUE CANADIENNE DE RECHERCHE FORESTIERE
ISSN journal
00455067 → ACNP
Volume
28
Issue
11
Year of publication
1998
Pages
1717 - 1722
Database
ISI
SICI code
0045-5067(199811)28:11<1717:AINSA">2.0.ZU;2-G
Abstract
Throughfall chemistry in deciduous and coniferous forests is characterized by a high spatial and temporal variability, the sources of which are largel y unknown. Aphids on Norway spruce (Picea abies (L.) Karst.) produce large quantities of honeydew, which is rich in sugars. We investigated the effect of changes in aphid abundance on throughfall carbon chemistry of Norway sp ruce using a rainfall simulation experiment. Aphid numbers in the experimen t paralleled field infestations. Infested trees showed significantly higher concentrations of dissolved organic carbon (DOC) and hexose-C in throughfa ll solutions compared with uninfested trees. There was also a pronounced se asonal trend in the concentrations of these carbon compounds with highest c oncentrations recorded at the time of peak aphid abundance at the end of Ju ne - beginning of July. The throughfall from a spruce tree showed no spatia l (center vs. periphery) differences in DOC and hexose-C concentrations. Th e number of aphids on a tree was the best predictor of the carbohydrate con centration of throughfall, explaining more than 60% of the variability. Dur ing the period of aphid infestation (May-September) average estimated field fluxes of DOC in throughfall collected under heavily infested trees ("hot spots") were 11.6 and 240 times higher than those recorded under moderately and uninfested trees, respectively. The results implicate herbivores as a major potential source of the spatiotemporal heterogeneity in flows of nutr ients in forests.