GROWTH OF ACER-SACCHARUM SEEDLINGS IN DEEPLY SHADED UNDERSTORIES OF NORTHERN WISCONSIN - EFFECTS OF NITROGEN AND WATER AVAILABILITY

Citation
Mb. Walters et Pb. Reich, GROWTH OF ACER-SACCHARUM SEEDLINGS IN DEEPLY SHADED UNDERSTORIES OF NORTHERN WISCONSIN - EFFECTS OF NITROGEN AND WATER AVAILABILITY, Canadian journal of forest research, 27(2), 1997, pp. 237-247
Citations number
48
Categorie Soggetti
Forestry
ISSN journal
00455067
Volume
27
Issue
2
Year of publication
1997
Pages
237 - 247
Database
ISI
SICI code
0045-5067(1997)27:2<237:GOASID>2.0.ZU;2-9
Abstract
Availability of soil nitrogen, soil moisture, and light were examined, along with the growth, biomass allocation, and leaf nitrogen concentr ation of naturally established Acer saccharum Marsh. seedlings, in the understories of 12 forest sites in northern Wisconsin. The sites repr esented a nutrient and moisture gradient (poor to rich) according to a habitat classification system. We asked (1) Are seedling growth rates , biomass allocation patterns, and leaf nitrogen related to soil water and nitrogen availability? and (2) Do soil resource rankings predicte d by habitat classifications mirror our direct observations? Across si tes compared in a low-light data set (plots with <5% canopy openness), rich sites had 2- to 4-fold higher seedling growth, percent leaf nitr ogen, nitrogen mineralization rates, and nitrification rates than poor sites. Seedling growth in low light correlated (P less than or equal to 0.05) positively with nitrification, total nitrogen mineralization, percent leaf nitrogen, soil moisture, and organic carbon, and negativ ely with fine root density. In multiple regression, soil moisture (P = 0.033) and nitrification (P = 0.015) together explained 79% of the va riation in growth. Thus, seedling growth in shade was enhanced on rich er sites in part because of higher nitrate N and water availability. T his has potential implications for forest dynamics, since the probabil ity of sugar maple becoming the dominant woody regeneration in any giv en understory may be partially dependent upon the level of soil resour ces.