Stable isotope evidence for the biogeochemical transformation of ancient organic matter beneath Suess Glacier, Antarctica

Glaciers overrun organic matter (OM) during periods of advance, making this overrun OM available as a metabolic substrate for subglacial microbes. The biogeochemical fate of this overrun OM remains poorly understood, ultimately limiting our understanding of subglacial biogeochemical cycling, particu...

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Bibliographic Details
Published in:Arctic, Antarctic, and Alpine Research
Main Authors: Joel D. Barker, Andréa G. Grottoli, W. Berry Lyons
Format: Article in Journal/Newspaper
Language:English
Published: Taylor & Francis Group 2018
Subjects:
Online Access:https://doi.org/10.1080/15230430.2018.1448643
https://doaj.org/article/9b87836e8bb848eea4d99f2383d1fc39