Fig 2 -

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...

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Bibliographic Details
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
Description
Summary: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.

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