carbon cycling of high latitude ecosystems (terrestrial lecture 8) Flashcards
1
Q
What are the characteristics of boreal forest (taiga?)
A
- freezing temperatures for 6-8 months
- characterised by coniferous needleleaf forest
- ~16 million km^2 = 11.5% terrestrial ecosystem area
2
Q
What are the characteristics of arctic tundra?
A
- tundra = “treeless”
- lands beyond the northern tree limit
- 7.5 million km^2 = 5.5% terrestrial ecosystem area
- temp above freezing for only 2-6 months
- dominated by grasses/sedges/shrubs
3
Q
What do taiga and tundra have in common?
- environment
- ecology
A
environment:
- cold
- short GSL (summer)
- long snow cover duration
- environmental extremes
- permafrost
- high winds: ice abrasion
ecology:
- slow decomposition
- low nutrients
- freeze tolerant plants
- low biodiversity
- slow growth
- high longevity
4
Q
What are the carbon stocks in taiga/tundra like?
- amount/density
- soil vs biomass
- carbon turnover rates
A
- taiga second in amount of C to tropical, comparable in C density (34.2kg/m2 vs 35)
- tundra lower amount of C, but density (20.5kg/m2) comparable to croplands, wetlands, temperate grasslands and forest
- both store more C in soil than biomass
- taiga 2-3x more
- tundra 5x more
- wayyyyy lower C turnover rate than tropical forests
- taiga: 53.3yrs
- tundra: 65.2yrs
- tropical: 14.2yrs
5
Q
How are high latitude systems changing?
- greening
- treeline advance
- shrubification
A
- greening: phenology changes. biomass is increasing so more C gain
- 20% increase 1982-2014
- boreal treeline advance: moving onto tundra
- younger spruces and higher proportion of seedlings at treeline edge
- shrubification of tundra
- 1950-2000 shrubs increased by 28% (hilltop) to 160% (floodplains)
- Sturm et al., 2005 & Tape et al., 2006
6
Q
High latitude C stocks - biomass increase vs soil respiration?
A
- models say increased biomass will increase C removed from atmosphere
- but more C in soil than biomass
- greening may prime ground decomposition and release C from soil
7
Q
What is the age of C respired in taiga/tundra through the growing season?
A
- age of respiring C can be measured through C14 isotope leftover from test bombing in 50s
- tundra gradually increases age of respired C thoughout GS
- taiga has peak in C age respired in middle of GS - peak photosynthesis time
- allocation of C below ground may stimulate decomposition of older recalcitrant C = “priming”