Microbial formation of labile organic carbon in Antarctic glacial environments

Nature Geoscience
By: , and 



Roughly six petagrams of organic carbon are stored within ice worldwide. This organic carbon is thought to be of old age and highly bioavailable. Along with storage of ancient and new atmospherically deposited organic carbon, microorganisms may contribute substantially to the glacial organic carbon pool. Models of glacial microbial carbon cycling vary from net respiration to net carbon fixation. Supraglacial streams have not been considered in models although they are amongst the largest ecosystems on most glaciers and are inhabited by diverse microbial communities. Here we investigate the biogeochemical sequence of organic carbon production and uptake in an Antarctic supraglacial stream in the McMurdo Dry Valleys using nanometre-scale secondary ion mass spectrometry, fluorescence spectroscopy, stable isotope analysis and incubation experiments. We find that heterotrophic production relies on highly labile organic carbon freshly derived from photosynthetic bacteria rather than legacy organic carbon. Exudates from primary production were utilized by heterotrophs within 24 h, and supported bacterial growth demands. The tight coupling of microbially released organic carbon and rapid uptake by heterotrophs suggests a dynamic local carbon cycle. Moreover, as temperatures increase there is the potential for positive feedback between glacial melt and microbial transformations of organic carbon.

Additional publication details

Publication type Article
Publication Subtype Journal Article
Title Microbial formation of labile organic carbon in Antarctic glacial environments
Series title Nature Geoscience
DOI 10.1038/ngeo2925
Volume 10
Year Published 2017
Language English
Publisher Nature
Contributing office(s) St. Petersburg Coastal and Marine Science Center
Description 4 p.
First page 356
Last page 359
Other Geospatial McMurdo Dry Valleys