peatlands's Usage Examples:

It is unique to natural areas called peatlands, bogs, mires, moors, or muskegs.

many thematic areas throughout the world, including the links between peatlands and climate change, as well as wetlands and waterbird migration, based.

Indonesia is also the world's third-largest carbon emitter, largely as a result of deforestation and the burning of peatlands.

draining of peatlands is probably the most important and long lasting threat to peatlands all over the world but especially in the tropics.

peatlands to determine the significance of ebullition as a source of methane.

Tropical peatlands are vulnerable to destabilisation through human and climate induced changes.

Middle Ages this began to change as rising sea levels and storms started to eat away at the coastal areas which consisted mainly of peatlands.

High acidity and the waterlogged conditions of peatlands such as Burns Bog prevent complete decomposition of fixed carbon.

peatlands are vulnerable to destabilisation through human and climate induced changes.

bryologist and peatland ecologist, recognized as a leading expert on peatlands.

Paludification is the most common process by which peatlands in the boreal zone are formed.

reproduction by fragmentation, producing much of the living material in sphagnum peatlands.

Tropical peatlands are significant carbon sinks and store large amounts of carbon and their.