The lagg is an integral part of the hydrological system of a raised bog and can add significantly to the biological diversity of the ecosystem. Conservation and restoration of raised bogs should therefore involve this transition zone. The ideal situation for conservation is to protect or restore the natural laggy at the outside margin of the bog. However, it is not always possible to restore the lagg where it was historically situated. An analysis of historic maps of a raised bog in British Columbia, Canada, shows that in areas where the outflow of water from the bog has been impeded, lagg plant communities have naturally colonized parts of the bog that were historically open bog. This suggests that it is possible to create the ecohydrologi...
The initial question of any ecological restoration project should be whether the degraded ecosystem...
Choosing past and present-day indicators could strengthen the reference ecosystem used for ecologica...
Mined peatlands do not readily recover their hydrological function, mainly because the dominant peat...
The lagg is an integral part of the hydrological system of a raised bog and can add significantly to...
The lagg of a raised bog is a transition zone where runoff collects from the ombrotrophic (rain-fed)...
The transition zone at the margin of raised bogs (the lagg) is rarely studied, yet it can be importa...
The fen which typically surrounds a raised bog is often considered to be of marginal interest, but t...
In restoration planning for damaged raised bogs, the lagg at the bog margin is often not given consi...
When restoring ecosystems, the simple removal of stresses causing degradation may seem preferable ov...
Inventories of natural assemblages of plant species are critical when planning ecological restoratio...
Burns Bog is a raised ombrotrophic bog in Delta, British Columbia and faced with myriad disturbances...
Harvested sites rarely return to functional ecosystems after abandonment because drainage and peat e...
Abstract. Bogs, economically valuable wetlands, are subjected to exploitation in southern Canada. We...
Soaks (areas of mesotrophic/minerotrophic vegetation within acid bog) add to the overall heterogenei...
Soaks (areas of mesotrophic/minerotrophic vegetation within acid bog) add to the overall heterogenei...
The initial question of any ecological restoration project should be whether the degraded ecosystem...
Choosing past and present-day indicators could strengthen the reference ecosystem used for ecologica...
Mined peatlands do not readily recover their hydrological function, mainly because the dominant peat...
The lagg is an integral part of the hydrological system of a raised bog and can add significantly to...
The lagg of a raised bog is a transition zone where runoff collects from the ombrotrophic (rain-fed)...
The transition zone at the margin of raised bogs (the lagg) is rarely studied, yet it can be importa...
The fen which typically surrounds a raised bog is often considered to be of marginal interest, but t...
In restoration planning for damaged raised bogs, the lagg at the bog margin is often not given consi...
When restoring ecosystems, the simple removal of stresses causing degradation may seem preferable ov...
Inventories of natural assemblages of plant species are critical when planning ecological restoratio...
Burns Bog is a raised ombrotrophic bog in Delta, British Columbia and faced with myriad disturbances...
Harvested sites rarely return to functional ecosystems after abandonment because drainage and peat e...
Abstract. Bogs, economically valuable wetlands, are subjected to exploitation in southern Canada. We...
Soaks (areas of mesotrophic/minerotrophic vegetation within acid bog) add to the overall heterogenei...
Soaks (areas of mesotrophic/minerotrophic vegetation within acid bog) add to the overall heterogenei...
The initial question of any ecological restoration project should be whether the degraded ecosystem...
Choosing past and present-day indicators could strengthen the reference ecosystem used for ecologica...
Mined peatlands do not readily recover their hydrological function, mainly because the dominant peat...