1. The patterns and consequences of post-fire successional trajectories in Alaska’s boreal forest The “Generators” - Fire severity - Abiotic and biotic site characteristics The consequences for -Nitrogen cycling, carbon storage and other key ecosystem processes -Future landscape and vegetation patterns (including biome shifts)

2. 90 sites established in 2004 burns along Dalton, Taylor, and Steese Highways 32 intensive study sites –arranged across combinations of high-low site moisture & high- low burn severity 7 treeline sites Detailed pre-fire stand data available for 14 sites Reconstruction of pre-fire conditions at remaining sites JFSP Study design

3. Dry Wet Low High JFSP Study design

4. What drives natural post-fire seedling recruiment? Differential sensitivity of functional groups to site characteristics and fire regime -Spruce recruitment (as measured by post-fire seedling density) is most influenced by elevation, pre-fire spruce density, and site moisture. Fire severity (CBI) and stand age had weaker effects -50 % of Deciduous recruitment can be explained by fire severity; also important were elevation, latitude, moisture, and distance to nearest unburned deciduous stand. - The ratio of spruce/deciduous recruitment is driven by the relationship between deciduous and fire severity. Important role of fire severity in “tipping” the balance between coniferous and deciduous dominance Johnstone, Hollingsworth, Chapin, and Mack (in prep) Global Change Biology

5. What drives post-fire vegetation composition? Bernhardt, Hollingsworth, Chapin, and Viereck (in prep) Journal of Vegetation Science

6. - Energy balance NECB ? ↓ N avail. ↓ productivity ↑ [CO 2 ] ↑ T ↑ Fire Frequency, intensity, and area

7. ↑ [CO 2 ] ↑ T ↑ Fire NECB + ↓ N avail. ↓ productivity Frequency, intensity, and area

8. Fire  N availability N pool size N turnover time Environment for decomposition Plant species composition –Pool size –TT –Environment –Uptake and use

9. Net loss of N from forest floor/organic soil = Pre-fire forest floor N pool - Remaining N pool [+ Ash from plants and upper layers] [- Leaching, erosion, gaseous loss] Calculating soil N loss

10. Mean offset between adv. roots and moss across 30 unburned sites: 3.2 ± 0.3 cm Adventitious root

11. Adventitious root collar to burned soil = depth of organic matter combusted Residual organic soil depth, bulk density and [N] N pool in missing layers = root collar depth x empirical relationships derived from unburned stands

12. DryWet Moisture class 0.03 0.04 0.05 0.06 0.07 0.08 0.09 0.10 0.11 0.12 N loss (kg N m -2 ) Mean =80 ± 4 g ·N m -2 1-94 % of pre-fire organic layer N pool Soil organic layer N loss across sites High Low Burn severity Moisture:F=0.69, P=0.41 Severity:F=4.62. P=0.04 M x S:F=0.19, P=0.67 N inputs are low Alder fixation max. Lichen/moss norm. (<0.1 g·N m -2 yr -1 ) Mean stand age: 94 ± 5.4 yrs Mining N? Alder inputs? Occult N? *

13. www.gina.alaska.edu Comparing the boreal forest to the Arctic

14. Anaktuvuk River Fire 2007 An opportunity for synthesis between a fire-naïve versus a fire-experienced biome

15. Research Questions How much carbon and nitrogen was lost during the Anaktuvuk River Fire? Do our known relationships between seedling regeneration, vegetation composition, and site characteristics hold true for tundra fires?

17. Estimating pre-fire soil organic matter pools Meristem to mineral soil depth (cm) Organic layer depth (cm) R 2 =0.94, P=<0.01

18. Pre-fire pools and fire-driven losses of nitrogen from tundra and taiga PoolsMATBlack spruce Pre-fire O layer Mean:280 200 (g N m -2 ) Range:206 to 578 50 to 429 N:2090 O layer N loss33103 (g N m -2 ) 7to 20930 to 180 % O layer N loss10.450 2 to 361 to 94

19. 0.0100200300400 500 Dry, high Dry, low Wet, high Wet, low Pre-fire N pool (g N m -2 ) N loss versus pre-fire N pool High-Dry R 2 =0.61, P<0.02 No relationship for other categories All sites R 2 =0.86, P<0.001 Black spruce taiga Moist Acidic Tundra N loss (kg N m -2 )

20. 9 transects across the Anaktuvuk River fire sampled 10 points along each transect sampled and combined for a) mineral soil and b) organic soils Germinated alder and spruce seedlings Autoclaved Tanana River silt as growth substrate Innoculated with organic or mineral soil from 9 sites (18 treatments) Minimal fertilizer (want them to survive but not thrive) Plant methods

21. Preliminary results Spruce Alder SpruceAlder a a b

22. Conclusions In taiga, sites with more accumulated N lost a smaller % of total N, while sites with more N lost a larger % –Fire driven N loss reinforces landscape patterns of N accumulation In arctic tundra, sites with more accumulated N lost more N –Fire smoothes landscape heterogeneity in N accumulation In arctic tundra, effects of mycorrhizal innoculum on plant height growth is related to soil horizon, not fire severity