Interactive comment on “Identification and analysis of low molecular weight dissolved organic carbon in subglacial basal ice ecosystems by ion chromatography” by E. C. Lawson et al

نویسنده

  • E. C. Lawson
چکیده

This paper by Lawson and co-workers reports very interesting results with regard to low molecular weight DOC (LMW-DOC) speciation and abundance in basal ice from glaciers that have different organic and lithological substrates and thermal regimes. The case is made that these LMW-DOC compounds may support and/or be a product of biogeochemical activity beneath glaciers with consequence to regional aquatic

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Interactive comment on “Identification and analysis of low molecular weight dissolved organic carbon in subglacial basal ice ecosystems by ion chromatography” by E. C. Lawson et al

This paper by Lawson and coworkers reports very interesting results with regard to low molecular weight DOC (LMW-DOC) speciation and abundance in basal ice from glaciers that have different organic and lithological substrates and thermal regimes. The case is made that these LMW-DOC compounds may support and/or be a product of biogeochemical activity beneath glaciers with consequence to regional...

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Identification and analysis of low molecular weight dissolved organic carbon in subglacial basal ice ecosystems by ion chromatography” by E. C. O’Donnell et al. Biogeosciences Discussion comments

20 Determining the concentration and composition of dissolved organic carbon (DOC) in glacial 21 ecosystems is important for assessments of in situ microbial activity and contributions to 22 wider biogeochemical cycles. Nonetheless, there is limited knowledge of the abundance and 23 character of DOC in basal ice and the subglacial environment and a lack of quantitative data 24 on low molecular ...

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Interactive comment on “Identification and analysis of low molecular weight dissolved organic carbon in subglacial basal ice ecosystems by ion chromatography” by E. C. Lawson et al

line 13): FAA is used but never defined Abstract (line 25): Why “current” subglacial environments? Could you delete “current”?line 25): Why “current” subglacial environments? Could you delete “current”? I think that the term “allochthonous” is misused throughout. The overrun OC hasn’t been derived from somewhere other than its present location, as the term suggests. Allochthonous has been used ...

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Continuous summer export of nitrogen-rich organic matter from the Greenland Ice Sheet inferred by ultrahigh resolution mass spectrometry.

Runoff from glaciers and ice sheets has been acknowledged as a potential source of bioavailable dissolved organic matter (DOM) to downstream ecosystems. This source may become increasingly significant as glacial melt rates increase in response to future climate change. Recent work has identified significant concentrations of bioavailable carbon and iron in Greenland Ice Sheet (GrIS) runoff. The...

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تاریخ انتشار 2015