Peatlands are carbon‐rich ecosystems that cover 185–423 million hectares (Mha) of the
earth's surface. The majority of the world's peatlands are in temperate and boreal zones …

About half of the world's tropical peatlands occur in Southeast (SE) Asia, where they serve
as a major carbon (C) sink. Nearly 80% of natural peatlands in this region have been …

Peatlands represent large terrestrial carbon banks. Given that most peat accumulates in
boreal regions, where low temperatures and water saturation preserve organic matter, the …

Peatlands are important carbon sinks, therefore their degradation mainly due to lowering of
the water table, has an adverse effect to the carbon cycle and largely burden the …

Tropical peatlands are vital ecosystems that play an important role in global carbon storage
and cycles. Current estimates of greenhouse gases from these peatlands are uncertain as …

Globally, peatlands play an important role in the carbon (C) cycle. High water level is a key
factor in maintaining C storage in peatlands, but water levels are vulnerable to climate …

Tropical peatlands now emit hundreds of megatons of carbon dioxide per year because of
human disruption of the feedbacks that link peat accumulation and groundwater hydrology …

Soil-derived dissolved organic matter (DOM) has a major influence in biogeochemical
processes related to contaminant dynamics and greenhouse gas emissions, due to its …

Tropical peat swamp forests sequester globally significant stores of carbon in deep layers of
waterlogged, anoxic, acidic and nutrient-depleted peat. The roles of microbes in supporting …

Adsorptive fractionation and oxidation of dissolved organic matter (DOM) on manganese
(Mn) oxide surfaces alter the molecular composition and stability of DOM, but the impact of …