Peatlands are globally known as major deposits of fresh water and carbon, affecting the planet's weather and local hydrology; for bearing unique plant and animal species, contributing to biodiversity; and because they represent a major economic resource to humanity. Peatlands are dominated by plants forming dense populations, especially Sphagnum moss and vascular plants belonging to the Cyperaceae and Juncaceae. They present high water table leveis and a deep organic matter layer (peat) below the living layer of plants. The use of fire and logging to clear forests in poor drainage soils have generated a kind of ecosystem similar to peatlands, dominated by Sphagnum moss, where peat accumulation is very low or absent (anthropogenic peatlands ...
Cerro Tocorpuri, belongs to the II region of Chile, in San Pedro de Atacama, on the border of Chile-...
Peatlands are soil environments that store carbon and large amounts of water, due to their compositi...
ABSTRACT In the face of the increasing natural resource demands, soil erosion and climatic variabili...
There is an exceptional group of alpine peatlands in the world situated in the and grasslands of the...
Artículo de publicación ISIPeatlands are a type of wetland characterized by the accumulation of orga...
This chapter highlights different aspects of origin, vegetation development and uses of Tierra del F...
Andean peatlands are important carbon reservoirs for countries in the northern Andes and have a uniq...
Sphagnum peatlands are threatened at a global scale, not only by peat extraction, but also by Sphagn...
Peatlands represent one of the most important water resources in the Puna grassland ecoregion, but t...
High-altitude peatlands in the Andes, i.e., bofedales, play an essential role in alpine ecosystems, ...
[Extract] Peatlands are terrestrial wetland ecosystems in which the production of organic matter exc...
Bryophytes and lichens in peatlands and Tepualia stipularis swamp forests of Isla Grande de Chilo
The tropical Andes store and regulate water outflow that serves nearly 60 million people. Most of th...
The high Andean peatlands, locally known as "bofedales", are a unique type of wetland distributed ac...
We report results of flora and vegetation in two of Sphagnum peatbogs in the Aisén Region
Cerro Tocorpuri, belongs to the II region of Chile, in San Pedro de Atacama, on the border of Chile-...
Peatlands are soil environments that store carbon and large amounts of water, due to their compositi...
ABSTRACT In the face of the increasing natural resource demands, soil erosion and climatic variabili...
There is an exceptional group of alpine peatlands in the world situated in the and grasslands of the...
Artículo de publicación ISIPeatlands are a type of wetland characterized by the accumulation of orga...
This chapter highlights different aspects of origin, vegetation development and uses of Tierra del F...
Andean peatlands are important carbon reservoirs for countries in the northern Andes and have a uniq...
Sphagnum peatlands are threatened at a global scale, not only by peat extraction, but also by Sphagn...
Peatlands represent one of the most important water resources in the Puna grassland ecoregion, but t...
High-altitude peatlands in the Andes, i.e., bofedales, play an essential role in alpine ecosystems, ...
[Extract] Peatlands are terrestrial wetland ecosystems in which the production of organic matter exc...
Bryophytes and lichens in peatlands and Tepualia stipularis swamp forests of Isla Grande de Chilo
The tropical Andes store and regulate water outflow that serves nearly 60 million people. Most of th...
The high Andean peatlands, locally known as "bofedales", are a unique type of wetland distributed ac...
We report results of flora and vegetation in two of Sphagnum peatbogs in the Aisén Region
Cerro Tocorpuri, belongs to the II region of Chile, in San Pedro de Atacama, on the border of Chile-...
Peatlands are soil environments that store carbon and large amounts of water, due to their compositi...
ABSTRACT In the face of the increasing natural resource demands, soil erosion and climatic variabili...