is the spring flush of nutrients in the tundra controlled ... filetundra controlled by snow depth?...
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Is the spring flush of nutrients in the Is the spring flush of nutrients in the tundra controlled by snow depth?tundra controlled by snow depth?
Kate Buckeridge and Paul GroganDepartment of Biology, Queen’s University
Kingston, ON, Canada
Is there a spring nutrient flush in arctic tundra?
Chapin, 1980, The Mineral Nutrition of Wild Plants, Annual Review of Ecology and Systematics 11: 233-60
Whalen & Cornwell, 1985, Can. J. Fish. Aquat. Sci 42: 797-808
• Ecosystem controls on vegetation patterns• Climate change predictions: deeper snow• Spatial and temporal variability in snow depth
Soil Temp
Litter and SOM
WINTER
microbial community dynamics ?, soil
water, soil C
Snow depth and quality
Soil solution (N)
Microbial Biomass (N)
THAW
DEEPENED SNOW EFFECTS
Is there a nutrient flush?
Is it ecologically significant?
Is it larger with deepened snow?
What triggers the flush?
Denitrification
?
Plant uptake
Leaching ?SPRING
Daring Lake, NWT, Canada (64o 52’N, 111o 35’W)
• ~25 km N of treeline• Continuous permafrost• Birch hummock tundra • Mesic organic soil
Circumpolar distribution
25% of total arctic soil carbon
DOY 129 (May 9)
-20
-15
-10
-5
0
5
10
241 281 321 361 36 76 116 156Julian Day
Soil
tem
pera
ture
, 5 c
m (
o C)ControlSnow fence
0
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40
60
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120
100 110 120 130 140 150 160 170Julian day
Snow
dep
th (c
m)
0
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Soil
wat
er (m
l H2O
m-2)
control snow depth control soil water
-20
-15
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-5
0
5
10
15
100 110 120 130 140 150 160 170Julian Day
Tem
pera
ture
(o C)control soil temperature, 5 cmair temperature DOY 147 (May 27)
-20
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-5
0
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Tem
pera
ture
(o C)control soil temperature, 5 cmsnow fence soil temperature, 5 cmair temperature
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100 110 120 130 140 150 160 170Julian day
Snow
dep
th (c
m)
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Soil
wat
er (m
l H2O
m-2)
control snow depth snow fence snow depthcontrol soil water snow fence soil water
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Snow
dep
th (c
m)
-14-12-10-8-6-4-2024
Dai
ly m
ean
soil
tem
pera
ture
(o C, 5
cm
dep
th)
0
50
100
150
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250
300
Soil
wat
er (m
l H2O
m-2)
Control Snow fence
0102030405060708090
100
100 115 130 145 160 175Julian Day
Dis
solv
ed o
rgan
ic
carb
on (g
m-2)
050
100150200250300350400450
Dis
solv
ed in
orga
nic
nitr
ogen
(mg
m-2)
050
100150200250300350400450
Dis
solv
ed in
orga
nic
phos
phor
us (m
g m
-2)
0.00.51.01.52.02.53.03.5
100 115 130 145 160 175Julian Day
Dis
solv
ed o
rgan
ic
nitr
ogen
(g m
-2)
0
20
40
60
80
100
120
Snow
dep
th (c
m)
-14-12-10-8-6-4-2024
Soil
tem
pera
ture
(o C)
0
50
100
150
200
250
300
Soil
wat
er (m
l H2O
m-2)
Control
0102030405060708090
100
100 115 130 145 160 175Julian Day
Dis
solv
ed o
rgan
ic
carb
on (g
m-2)
050
100150200250300350400450
Dis
solv
ed in
orga
nic
nitr
ogen
(mg
m-2)
050
100150200250300350400450
Dis
solv
ed in
orga
nic
phos
phor
us (m
g m
-2)
0.00.51.01.52.02.53.03.5
100 115 130 145 160 175Julian Day
Dis
solv
ed o
rgan
ic
nitr
ogen
(g m
-2)
100200300400500600700800900
1000
100 115 130 145 160 175
Julian day
Mic
robi
al b
iom
ass
carb
on
(g m
-2)
05
101520253035
Mic
robi
al b
iom
ass
nitr
ogen
(g m
-2)
0
20
40
60
80
100
120
Snow
dep
th (c
m)
-14-12-10-8-6-4-2024
Soil
tem
pera
ture
(oC)
0
50
100
150
200
250
300
Soil
wat
er (g
H2O
m-2)
Control
Snow fence
02468
101214161820
Mic
robi
al b
iom
ass
phos
phor
us
(g M
B-PO
4 m
-2)
5
10
15
20
25
30
35
100 115 130 145 160 175
Julian Day
MBC
:N
100200300400500600700800900
1000
100 115 130 145 160 175
Julian day
Mic
robi
al b
iom
ass
carb
on
(g m
-2)
05
101520253035
Mic
robi
al b
iom
ass
nitr
ogen
(g m
-2)
0
20
40
60
80
100
120
Snow
dep
th (c
m)
-14-12-10-8-6-4-2024
Soil
tem
pera
ture
(o C)
0
50
100
150
200
250
300
Soil
wat
er (g
H2O
m-2)
Control
02468
101214161820
Mic
robi
al b
iom
ass
phos
phor
us
(g M
B-PO
4 m
-2)
5
10
15
20
25
30
35
100 115 130 145 160 175
Julian Day
MBC
:N
Control & snow fence soils:
• No N pulse
• DOC and PO43- pulse may be
important for nutrient transfer from terrestrial to aquatic
• Microbial C:N:P variation suggests microbial community succession
Snow fence soils only:
• DIN + DON pulse ~75% of annual aboveground plant N requirement for this ecosystem
• A second substantial DOC and PO4
3- pulse
• Microbial C:N:P variation suggests microbial community succession
Period 1 Period 2
Moderate fluctuations
Soil Temp
Litter and SOM
WINTER
microbial community dynamics ?, soil
water, soil C
Snow depth and quality
Period 1
Small fluctuations
THAW
DEEPENED SNOW EFFECTSRising air T:
Soil: -7 to -2 oC
Decomposition & leaching ↑
Large fluctuations
Deep snow melt:Soil: -2 to +2 oC
Period 2
Large fluctuations
PredationImmobilization/ mineralization
Soil solution (N)
Microbial Biomass (N)
Denitrification
?Leaching ?
Plant uptake
SPRING
• Yes, there is a spring nutrient flush
• The early thaw flush is C and P• The snow melt flush is C, N and P, under deepened
snow only
• Microbial community succession and SOM quality affected by temperature change, osmotic pressure changes, before snow thaw is complete
• Ecologically significant? Spring flush may contribute to vegetation patchiness across landscape
• Loss or retention of flush depends on plant and microbial uptake before snow thaw is complete
ACKNOWLEDGEMENTS
Field, lab and data:Linda CameronElyn HumphriesPeter LafleurMeghan LaidlawBob ReidMike TrebergMathew Vankoughnett
Logistics:Steve Matthews, GNWT
Funding:Natural Sciences and
Engineering Research Council of Canada (NSERC)
International Polar YearW. Garfield Weston Foundation
(via CNST (ACUNS))Indian and Northern Affairs
Canada (INAC-NSTP)Canadian Tundra Ecosystem
Carbon Study (CTECS) Queen’s University