Anaerobic respiration in a boreal wetland and surrounding habitats, across a hydrological transect ...

• Main Authors: Baysinger, Mackenzie, Jentzsch, Katharina, Liebner, Susanne, Strauss, Jens, Yang, Sizhong, Treat, Claire C
• Format: Dataset
• Language: unknown
• Published: PANGAEA 2024
• Subjects: Anaerobic incubation; Boreal; CH4; CO2; Laboratory experiment; peat; Soil profile; sphagnum; Event label; Type of study; Year of sampling; Sample code/label; LATITUDE; LONGITUDE; Site; Country; Day of experiment; Habitat; Depth, description; Incubation temperature; Replicate; Zone; Description; Vegetation type; Major vegetation; Soil horizon; Soil type; pH, soil; Soil water content, volumetric; Density, wet bulk; Carbon, total; Carbon, organic, total; Carbon, inorganic, total; Nitrogen, total; Carbon/Nitrogen ratio; Depth, soil, minimum; Depth, soil, maximum; DEPTH, soil; Carbon dioxide, production rate, CO2-C per mass soil; Methane, production rate, CH4-C per mass soil; Carbon dioxide, production rate, CO2-C per mass carbon; Methane, production rate, CH4-C per mass carbon; Peat corer; Carbon and nitrogen and sulfur CNS isotope element analyzer, Elementar, Vario EL III; Gas chromatograph 7890A, Agilent Technologies, USA with flame ionization detection FID; FN-Land_2021_SiikanevaPeatland; AWI Arctic Land Expedition; Arctic; Fid
• Online Access: https://dx.doi.org/10.1594/pangaea.964303; https://doi.pangaea.de/10.1594/PANGAEA.964303

This dataset reports measurements from a laboratory incubation of soils sourced from a boreal peatland and surrounding habitats (Siikaneva Bog, Finland). In August 2021, soil cores were collected from three habitat zones: a well-drained upland forest, an intermediate margin ecotone, and a Sphagnum moss bog. The cores from each habitat were taken from surface to approximately 50cm below surface using an Eijelkamp peat corer and subdivided by soil horizon. The samples were then incubated anaerobically for 140 days in three temperature treatment groups (0, 4, 20°C). Subsamples of the incubations headspace (250 µL) were measured on a gas chromatograph (7890A, Agilent Technologies, USA) with flame ionization detection (FID) for CO2 and CH4 concentrations. The rate of respiration from the samples were calculated per gram carbon and per gram soil as described in the method of Robertson., et al. (1999) and reported here, along with other relevant parameters. ...