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
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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
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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
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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
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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
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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
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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”
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