Fig 2 -

• Main Authors: R. M. Wilson (10197022), A. A. Zayed (10197025), K. B. Crossen (10197028), B. Woodcroft (10197031), M. M. Tfaily (10197034), J. Emerson (10197037), N. Raab (4417750), S. B. Hodgkins (10197040), B. Verbeke (10197043), G. Tyson (10197046), P. Crill (10197049), S. Saleska (10197052), J. P. Chanton (2456635), V. I. Rich (10197055)
• Format: Still Image
• Language: unknown
• Published: 2021
• Subjects: Cell Biology; Molecular Biology; Biotechnology; Evolutionary Biology; Ecology; Inorganic Chemistry; Infectious Diseases; Cardiology; Environmental Sciences not elsewhere classified; Chemical Sciences not elsewhere classified; CH 4 production; material; geochemistry; greenhouse gas exchange; field results; CO 2; understanding carbon cycling; incubation; scale geochemical processes; CH 4 dynamics; palsas
• Online Access: https://doi.org/10.1371/journal.pone.0245857.g002

Alpha compared across habitats in the field (panel a) and and in the incubations averaged over 0–5 days (panel b), 20–30 days (panel c), 45–55 days (panel d), 70–80 days (panel e), and 90–100 days (panel f) throughout the incubation for each habitat. The first panel contains significance results of anova comparing the field and timepoints for each habitat. Neither depth of the collapsed palsas or BogD field were significantly different from any time point in the respective incubations. FenD was not significantly different until the end (day 75) of the incubations. BogS and FenS were the only sites that were significantly different from the incubations at all time points.