We studied mature and adjacent open lichenâ spruce woodlands (LWs) and closed-canopy spruceâ feathermoss stands (FMs) growing under similar edaphic conditions in the continuous boreal forest zone in Quebec (Canada). A total of 6 pairs of stands were investigated by profile sampling. Stem density, basal area, and biomass were about 4 times greater in FMs than in LWs on an area basis. In the humus layer, total stocks of C and N and of exchangeable K, Ca, Mg, Al, and Na were 1.4 to 2.3 times larger in FM than in LW soils. The first 30 cm and first meter of mineral soils in LWs and FMs displayed similar available nutrient pools except for total C stocks, which were more than twice as large in FM as in LW soils in these soil layers. For the wh...
Black spruce (Picea mariana (Mill.) B.S.P.)-feathermoss forests are a common subtype of the norther...
An environmental study using the association concept and the 'ecological groups' within the biogeocl...
Soil organic carbon (C), accumulated over millennia, comprise more than half the C stored in boreal ...
We studied mature and adjacent open lichenâ spruce woodlands (LWs) and closed-canopy spruceâ feath...
International audienceAt the northernmost extent of the managed forest in Quebec, Canada, the boreal...
In the boreal forest, long-lasting canopy gaps are associated with lichens on dry sites and with Sph...
Climate change is likely to affect the growth, development and regeneration of the black spruce stan...
Lichen woodlands (LWs) are persistent unproductive areas of the Canadian boreal forests whose affore...
Open lichen woodlands (LWs) are degraded stands that lack the ability to regenerate naturally due to...
Open lichen woodlands (LWs) are degraded stands that lack the ability to regenerate naturally due to...
Changes in forest ecosystem vegetation also bring about changes to the associated soil. In order to ...
The consequences of forest fragmentation and edge effects on soil nutrient availability and nutritio...
Improving knowledge on the dynamics and maintenance of the boreal soil’s C pool is of particular imp...
Abstract: Carbon (C) stocks were assessed for hybrid interior spruce (Picea glauca (Moench) Voss × P...
The interacting influence of disturbances and nutrient dynamics on aboveground biomass, forest floor...
Black spruce (Picea mariana (Mill.) B.S.P.)-feathermoss forests are a common subtype of the norther...
An environmental study using the association concept and the 'ecological groups' within the biogeocl...
Soil organic carbon (C), accumulated over millennia, comprise more than half the C stored in boreal ...
We studied mature and adjacent open lichenâ spruce woodlands (LWs) and closed-canopy spruceâ feath...
International audienceAt the northernmost extent of the managed forest in Quebec, Canada, the boreal...
In the boreal forest, long-lasting canopy gaps are associated with lichens on dry sites and with Sph...
Climate change is likely to affect the growth, development and regeneration of the black spruce stan...
Lichen woodlands (LWs) are persistent unproductive areas of the Canadian boreal forests whose affore...
Open lichen woodlands (LWs) are degraded stands that lack the ability to regenerate naturally due to...
Open lichen woodlands (LWs) are degraded stands that lack the ability to regenerate naturally due to...
Changes in forest ecosystem vegetation also bring about changes to the associated soil. In order to ...
The consequences of forest fragmentation and edge effects on soil nutrient availability and nutritio...
Improving knowledge on the dynamics and maintenance of the boreal soil’s C pool is of particular imp...
Abstract: Carbon (C) stocks were assessed for hybrid interior spruce (Picea glauca (Moench) Voss × P...
The interacting influence of disturbances and nutrient dynamics on aboveground biomass, forest floor...
Black spruce (Picea mariana (Mill.) B.S.P.)-feathermoss forests are a common subtype of the norther...
An environmental study using the association concept and the 'ecological groups' within the biogeocl...
Soil organic carbon (C), accumulated over millennia, comprise more than half the C stored in boreal ...