Decoding Nutrient Limitations in Cedar Bog's Alkaline Fens
Fens store up to 200–450 petagrams of carbon globally—equivalent to 25–50% of atmospheric CO₂ 3 . Unlike acidic bogs, alkaline fens (pH 7–8) are fed by calcium-rich groundwater, creating unique conditions where bacteria, not fungi, dominate decomposition.
Microbes require balanced carbon (C), nitrogen (N), and phosphorus (P) to thrive. Imbalances trigger nutrient limitation:
Enzyme | Function | Activity (nmol·g⁻¹·h⁻¹) |
---|---|---|
β-glucosidase | Cellulose decomposition | 24.3 ± 2.5 |
Phosphatase | Organic P mineralization | 183.7 ± 14.1 |
LAP | Peptide breakdown | 0.5 ± 0.1 |
Data show P-acquisition dominates metabolic effort—a classic sign of P limitation 1 .
Only +C and +CNP boosted CO₂ by >300%. N or P alone had negligible effects.
Treatment | BG Activity (% change) | AP Activity (% change) | LAP Activity (% change) |
---|---|---|---|
+C | +15% | -12% | +8% |
+P | +3% | -65% | +5% |
+NP | +10% | -58% | +20% |
+CNP | +22% | -63% | +25% |
Sediments contained abundant total phosphorus, but most was locked in calcium-phosphate complexes. Bacteria could only access this via phosphatase enzymes—metabolically expensive to produce. Adding labile P (e.g., +CNP) let microbes redirect energy from mining to growth.
Alkaline fens are dual-limited ecosystems:
As climate change dries fens, reduced plant productivity may starve microbes of C. Paradoxically, rewetting could intensify P limitation by diluting dissolved nutrients.
"These bacteria hold the keys to the carbon vault. Understanding their nutritional needs is our first step toward keeping it locked."