CO2 release from particulate organic carbon (POC) oxidation during fluvial transit can influence climate over a range of timescales. Identifying the mechanistic controls on such carbon fluxes requires determining where POC oxidation occurs in river systems. While field data show POC oxidation and replacement moving downstream in lowland rivers, flume studies show that oxidation during active fluvial transport is limited. This suggests that most fluvial POC oxidation occurs during transient floodplain storage, but this idea has yet to be tested. Here, we isolate the influence of floodplain storage time on POC oxidation by exploiting a chronosequence of floodplain deposits above the modern groundwater table in the Rio Bermejo, Argentina. Meas...
Geomorphological controls and catchment sediment characteristics control the formation of floodplain...
Floodplains are important organic carbon (OC) storage sites, and the evolution of watercourses modul...
Terrestrial vegetation and soils hold three times more carbon than the atmosphere. Much debate conce...
Identifying drivers of seasonal variations in fluvial particulate organic carbon (POC) composition c...
Rivers transfer terrestrial organic carbon (OC) from mountains to ocean basins, playing a key role i...
Identifying drivers of seasonal variations in fluvial particulate organic carbon (POC) composition c...
Oxidation of particulate organic carbon (POC) during fluvial transit releases CO2 to the atmosphere ...
The mass of carbon stored as organic matter in terrestrial systems is sufficiently large to play an...
The oxidation of organic carbon contained within sedimentary rocks (“petrogenic” carbon, or hereafte...
The oxidation of organic carbon contained within sedimentary rocks ("petrogenic" carbon, or hereafte...
International audienceThe two long-term sources of atmospheric carbon are CO2 degassing from metamor...
Here we report on the effects of an experimental flood on the carbon cycling dynamics in the dry wat...
Productive forests of the Andes are subject to high erosion rates that supply to the Amazon River se...
Floodplains contain soils rich in organic matter and are important ecosystems for agricultural produ...
Physical erosion can mobilise particulate organic carbon (POC) from vegetation and soil, representin...
Geomorphological controls and catchment sediment characteristics control the formation of floodplain...
Floodplains are important organic carbon (OC) storage sites, and the evolution of watercourses modul...
Terrestrial vegetation and soils hold three times more carbon than the atmosphere. Much debate conce...
Identifying drivers of seasonal variations in fluvial particulate organic carbon (POC) composition c...
Rivers transfer terrestrial organic carbon (OC) from mountains to ocean basins, playing a key role i...
Identifying drivers of seasonal variations in fluvial particulate organic carbon (POC) composition c...
Oxidation of particulate organic carbon (POC) during fluvial transit releases CO2 to the atmosphere ...
The mass of carbon stored as organic matter in terrestrial systems is sufficiently large to play an...
The oxidation of organic carbon contained within sedimentary rocks (“petrogenic” carbon, or hereafte...
The oxidation of organic carbon contained within sedimentary rocks ("petrogenic" carbon, or hereafte...
International audienceThe two long-term sources of atmospheric carbon are CO2 degassing from metamor...
Here we report on the effects of an experimental flood on the carbon cycling dynamics in the dry wat...
Productive forests of the Andes are subject to high erosion rates that supply to the Amazon River se...
Floodplains contain soils rich in organic matter and are important ecosystems for agricultural produ...
Physical erosion can mobilise particulate organic carbon (POC) from vegetation and soil, representin...
Geomorphological controls and catchment sediment characteristics control the formation of floodplain...
Floodplains are important organic carbon (OC) storage sites, and the evolution of watercourses modul...
Terrestrial vegetation and soils hold three times more carbon than the atmosphere. Much debate conce...