Microorganisms have a crucial role to play in the cycling of nutrients within glacial environments. These systems are often nutrient-limited, and so biogeochemical reactions, which ensure the availability of nutrients for microbial communities, are critical for the maintenance of these systems. This study uses molecular biology to characterise the supraglacial cryoconite microbial communities that are capable of cycling carbon and nitrogen in a range of glacial environments. Organisms with the potential to photosynthesise were identified, including Cyanobacteria, Actinobacteria, Betaproteobacteria, Stramenopiles and Haptophyceae. Organisms with the potential to perform nitrification and denitrification processes were also identified and fea...
<p><strong>Figure 4.</strong> RDA triplot showing the effects of environmental variables (dashed arr...
In the present Ph.D. thesis, the succession of nitrogen cycle communities along the Damma glacier ch...
Retreating ice fronts (as a result of a warming climate) expose large expanses of deglaciated forefi...
Microorganisms have a crucial role to play in the cycling of nutrients within glacial environments. ...
<p><strong>Figure 6.</strong> Phylogenetic analysis of the nitrososphaeraceae sequences identified i...
Subglacial environments are located at the interface of glacier ice and bedrock. They represent one ...
<p><b>Table 5.</b> Sequencing depth and diversity and dominance indices for the sele...
<p><strong>Figure 5.</strong> Diversity of prokaryotic phyla in the samples selected for pyrosequenc...
Supraglacial environments occupy 11% of Earth’s surface area and represent a critical interface betw...
<p><b>Table 3.</b> Nutrient concentrations in cryoconite sediment, supraglacial melt...
Glacier forefields are ideal ecosystems to study the development of nutrient cycles as well as singl...
The supraglacial environment is an integral part of the glacial ecosystem. It is known to harbour an...
<p><strong>Figure 3.</strong> Class level assignment of contigs (<em>e</em> ≤ 1 <b>×</b> 10<sup>−5</...
The microbial communities and photosynthetic capacity of cryoconite holes on the Midre Lovénbreen Gl...
<p><b>Table 1.</b> Primer sets used for qPCR of 16S rRNA and <em>amoA</em> genes ...
<p><strong>Figure 4.</strong> RDA triplot showing the effects of environmental variables (dashed arr...
In the present Ph.D. thesis, the succession of nitrogen cycle communities along the Damma glacier ch...
Retreating ice fronts (as a result of a warming climate) expose large expanses of deglaciated forefi...
Microorganisms have a crucial role to play in the cycling of nutrients within glacial environments. ...
<p><strong>Figure 6.</strong> Phylogenetic analysis of the nitrososphaeraceae sequences identified i...
Subglacial environments are located at the interface of glacier ice and bedrock. They represent one ...
<p><b>Table 5.</b> Sequencing depth and diversity and dominance indices for the sele...
<p><strong>Figure 5.</strong> Diversity of prokaryotic phyla in the samples selected for pyrosequenc...
Supraglacial environments occupy 11% of Earth’s surface area and represent a critical interface betw...
<p><b>Table 3.</b> Nutrient concentrations in cryoconite sediment, supraglacial melt...
Glacier forefields are ideal ecosystems to study the development of nutrient cycles as well as singl...
The supraglacial environment is an integral part of the glacial ecosystem. It is known to harbour an...
<p><strong>Figure 3.</strong> Class level assignment of contigs (<em>e</em> ≤ 1 <b>×</b> 10<sup>−5</...
The microbial communities and photosynthetic capacity of cryoconite holes on the Midre Lovénbreen Gl...
<p><b>Table 1.</b> Primer sets used for qPCR of 16S rRNA and <em>amoA</em> genes ...
<p><strong>Figure 4.</strong> RDA triplot showing the effects of environmental variables (dashed arr...
In the present Ph.D. thesis, the succession of nitrogen cycle communities along the Damma glacier ch...
Retreating ice fronts (as a result of a warming climate) expose large expanses of deglaciated forefi...