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...
Published in: | Arctic, Antarctic, and Alpine Research |
---|---|
Main Authors: | , , |
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 |