AbstractThe major part of carbon (C) flow into forest soil consists of continually renewed fine roots and aboveground litterfall. We studied the belowground C input from the fine root litter of trees and understorey vegetation in relation to their aboveground litterfall in two Norway spruce (Picea abies L.) stands located in northern and southern Finland. The production of fine roots was estimated by using turnover and biomass data from minirhizotrons and soil cores. The foliage litter production of trees was estimated from litter traps, and that of the understorey vegetation from its annual growth and coverage. Finally, we augmented the data with four spruce plots in Sweden in order to study the above- and belowground litter ratios along l...
There is evidence that anthropogenic nitrogen (N) deposition enhances carbon (C) sequestration in bo...
There is evidence that anthropogenic nitrogen (N) deposition enhances carbon (C) sequestration in bo...
Litterfall is a major, yet poorly studied, process within forest ecosystems globally. It is importan...
The major part of carbon (C) flow into forest soil consists of continually renewed fine roots and ab...
The major part of carbon (C) flow into forest soil consists of continually renewed fine roots and ab...
AbstractThe major part of carbon (C) flow into forest soil consists of continually renewed fine root...
Forest ecosystem productivity is strongly linked to site nutrient availability, which is influenced ...
Abstract 1. Fine root turnover plays a critical role in carbon and nutrient cycling in forest ecosys...
Boreal forests capture and store substantial amounts of carbon in a global perspective, and the soil...
Background: In contrast with the negligible contribution of the forest understorey to the total abov...
Nutrient enrichment can alleviate productivity limitations and thus substantially increase carbon (C...
We synthesised results on soil carbon (C) and nitrogen (N) fluxes and the accumulation of soil organ...
Allocation of C to belowground plant structures is one of the most important, yet least well quantif...
Dissolved organic carbon (DOC) derived from plant litter plays an important role in the ecosystem ca...
There is evidence that anthropogenic nitrogen (N) deposition enhances carbon (C) sequestration in bo...
There is evidence that anthropogenic nitrogen (N) deposition enhances carbon (C) sequestration in bo...
Litterfall is a major, yet poorly studied, process within forest ecosystems globally. It is importan...
The major part of carbon (C) flow into forest soil consists of continually renewed fine roots and ab...
The major part of carbon (C) flow into forest soil consists of continually renewed fine roots and ab...
AbstractThe major part of carbon (C) flow into forest soil consists of continually renewed fine root...
Forest ecosystem productivity is strongly linked to site nutrient availability, which is influenced ...
Abstract 1. Fine root turnover plays a critical role in carbon and nutrient cycling in forest ecosys...
Boreal forests capture and store substantial amounts of carbon in a global perspective, and the soil...
Background: In contrast with the negligible contribution of the forest understorey to the total abov...
Nutrient enrichment can alleviate productivity limitations and thus substantially increase carbon (C...
We synthesised results on soil carbon (C) and nitrogen (N) fluxes and the accumulation of soil organ...
Allocation of C to belowground plant structures is one of the most important, yet least well quantif...
Dissolved organic carbon (DOC) derived from plant litter plays an important role in the ecosystem ca...
There is evidence that anthropogenic nitrogen (N) deposition enhances carbon (C) sequestration in bo...
There is evidence that anthropogenic nitrogen (N) deposition enhances carbon (C) sequestration in bo...
Litterfall is a major, yet poorly studied, process within forest ecosystems globally. It is importan...