Abstract: From hilltop to kettle hole: what trends across the terrestrial-aquatic transition zone are revealed by organic matter stable isotope (δ<sup>13</sup>C and δ<sup>15</sup>N) composition? (2016 AGU Fall Meeting)

From hilltop to kettle hole: what trends across the terrestrial-aquatic transition zone are revealed by organic matter stable isotope (δ¹³C and δ¹⁵N) composition?

Zachary E Kayler^1,2, Kai Nils Nitzsche³, Arthur Gessler⁴, Michael L Kaiser⁵, Carsten Hoffmann⁶, Katrin Premke² and Ruth Ellerbrock⁶, (1)US Forest Service Houghton, Houghton, MI, United States, (2)Inst for Landschaftsstoffdynam, Muncheberg, Germany, (3)Leibniz Centre for Agricultural Landscape Research, Institute for Landscape Biogeochemistry, Müncheberg, Germany, (4)WSL Swiss Federal Institute for Forest, Snow and Landscape Research, Forest Growth and Climate, Birmensdorf, Switzerland, (5)University of Kassel, Environmental Chemistry, Kassel, Germany, (6)Leibniz Centre for Agricultural Landscape Research, Institue of Soil Landscape Research, Müncheberg, Germany

Back to: Soil Carbon Dynamics: Models and Experiments Investigating Controls on Soil Organic Matter Vulnerability in Dynamic Landscapes I

From hilltop to kettle hole: what trends across the terrestrial-aquatic transition zone are revealed by organic matter stable isotope (δ13C and δ15N) composition?

From hilltop to kettle hole: what trends across the terrestrial-aquatic transition zone are revealed by organic matter stable isotope (δ¹³C and δ¹⁵N) composition?