Subsurface C dynamics
Wetlands Meeting 2025
June 20th, 2025
Susan Pit
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Outline
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Yampah Marsh
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Which reactions dominate subsurface C decomposition?
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(OβMeara et al., 2024)
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Yampah Marsh
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Porter
North
Yampah
Hester
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Yampah Marsh
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Sample collection
Dry/Warm Season
Wet/Cold Season
High Tide
Low Tide
Vegetated
Mud
Vegetated
Mud
Vegetated
Mud
Vegetated
Mud
High Tide
Low Tide
x2
Updates since June 2024
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Yampah Marsh
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Subsurface carbon dynamics in a pristine salt marsh
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Yampah sampling site
Transport Regime
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Respiration:
Nitrate,
Fe(II) and
Sulfate
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Respiration:
Nitrate,
Fe(II) and
Sulfate
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More respiration means vegetated cores have more dissolved C
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BSR/AOM at depth
S ox. at surface
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AOM:
CH4 + SO42- + H+ β H2S + HCO3- + H2O
BSR:
OM+ SO42- β H2S + 2HCO3- + 0.3NH4+
Methanogenesis at low tide?
AOM at high tide?
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Yampah Marsh
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AOM
Methanogenesis
Large interanual
differences
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Yampah Marsh
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AOM
Methanogenesis
S Oxidation
ΞTA:DIC ratios:
combination of denitrification, BSR, Fe reduction, and some aerobic respiration
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Yampah Marsh
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Methanogene
Vegetated Mud
Wet Season Dry Season
Preliminary Conclusions
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Mathematica RTM
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Assumption: each POCdegr produces 1 CH4 and 1 HCO3-.
Included reactions:
Depth [cm]
SO4 depletion [mM]
Preliminary results
Vegetated core, Dry22
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Reaction Rates [umol cm-2 yr-1] | ||
| High Tide | Low Tide |
POC degradation | 187 | 273 |
BSR | 78 | 61 |
Methanogenesis | 78 | 61 |
AOM | 109 | 153 |
*Depth integrated
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Questions?
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Wolf-Gladrow et al., (2007)
Liu et al., (2021)
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Alongi (2020)