The importance of plant-mediated CH4 transport was studied in a northe
rn wetland. CH4 transport through Eriophorum, a dominant sedge, was fo
und to be the major pathway for CH4 fluxes. Mean emission from Sphagnu
m lawns was low (34 mu g CH4 m(-2) h(-1)) and significantly higher fro
m tussocks of Eriophorum vaginatum (974 mu g CH4 m(-2) h(-1) U-test, p
< 0.05). Mean flux from single tillers of Eriophorum angustifolium wa
s 92 mu g CH4 h(-1) In contrast to other ecosystems, no CH4 oxidation
was associated with Eriophorum. Hence, the lack of oxidation is one re
ason for the high emission rates from these ecosystems. This finding i
s a caveat for models of CH4 emission and may also have consequences f
or carbon flow models of northern wetlands.