Methane transport mechanisms and isotopic fractionation in emergent macrophytes of an Alaskan tundra lake

• Main Authors: Chanton, Jeffrey P., Martens, Christopher S., Kelley, Cheryl A., Crill, Patrick M., Showers, William J.
• Format: Other/Unknown Material
• Language: unknown
• Published: 1992
• Subjects: 51; Arctophila fulva; Tundra
• Online Access: http://ntrs.nasa.gov/search.jsp?R=19930032547

The stable carbon isotopic composition of methane associated with and emitted by the two dominant emergent macrophytes abundant in the many Alaskan tundra lakes, Carex rostrata and Arctophila fulva, is determined. The carbon isotopic composition of the methane was -58.6 +/- 0.5 (n=2) for Arctophila and -66.6 +/- 2.5 (n=6) for Carex. The methane emitted by these species is depleted in C-13 by 12 per mil for Arctophila and 18 per mil for Carex relative to methane withdrawn from plant stems 1-2 cm below the waterline. The results suggest more rapid transport of (C-12)H4 relative to (C-13)H4 through plants to the atmosphere. Plant stem methane concentrations ranged from 0.2 to 4.0 percent in Arctophila, with an isotopic composition of -46.1 +/- 4.3 percent (n=8). Carex stem methane concentrations ranged from 150 to 1200 ppm, with an isotopic composition of -48.3 +/- 1.4 per mil (n=3).