Effects of Surface Fires and Below Ground Heating on the Biogeochemical Structures of Endomycorrhizal Fungal Spores
Poster Number
03
College
College of Arts and Sciences
Department
Chemistry, Physics, Geology, & the Environment
Faculty Mentor
Dr. Scott Werts
Abstract
The impact of surface fires on soil properties can vary from negligible to severe, depending on a multitude of factors on both the surface of the soil and within the soil itself. Once a fire moves through an ecosystem, there are no simple ways to know exactly how deep the heat from the fire penetrated into the soil or what those temperatures actually were. Having this information may provide insight into ecosystem recovery and may have further applications to archaeological studies. We are investigating the biogeochemical structure of endomycorrhizal fungal spores, which show little to no morphological change when exposed to temperatures exceeding 500°C and should remain present in the soil following a fire event. We obtained soil samples from a pine dominated forest and a deciduous forest in two different soil types from the piedmont of the southeastern US and extracted the fungal spores for temperature experiments. We utilized a scanning electron microscope with emission dispersive spectroscopy to seek information on the biogeochemical structure of the spores and note any changes in nature of the structure and makeup as temperature increased. Initial results suggest that oxygen ratios may be changing with temperature, however, more work is being done on various species to see if there are species-specific trends.
Previously Presented/Performed?
American Geophysical Union (AGU) Conference, San Francisco, California, December 2015
Start Date
22-4-2016 12:00 PM
End Date
22-4-2016 2:00 PM
Effects of Surface Fires and Below Ground Heating on the Biogeochemical Structures of Endomycorrhizal Fungal Spores
Rutledge
The impact of surface fires on soil properties can vary from negligible to severe, depending on a multitude of factors on both the surface of the soil and within the soil itself. Once a fire moves through an ecosystem, there are no simple ways to know exactly how deep the heat from the fire penetrated into the soil or what those temperatures actually were. Having this information may provide insight into ecosystem recovery and may have further applications to archaeological studies. We are investigating the biogeochemical structure of endomycorrhizal fungal spores, which show little to no morphological change when exposed to temperatures exceeding 500°C and should remain present in the soil following a fire event. We obtained soil samples from a pine dominated forest and a deciduous forest in two different soil types from the piedmont of the southeastern US and extracted the fungal spores for temperature experiments. We utilized a scanning electron microscope with emission dispersive spectroscopy to seek information on the biogeochemical structure of the spores and note any changes in nature of the structure and makeup as temperature increased. Initial results suggest that oxygen ratios may be changing with temperature, however, more work is being done on various species to see if there are species-specific trends.
