effects of marine-derived nutrients on productivity in sockeye systems
TRANSCRIPT
Effects of Marine-Derived Nutrients on Productivity in Sockeye Systems
Collaborative ProjectFunded by Watersheds Initiative of the Gulf
Ecosystem Monitoring (GEM) Component of EVOS
IMS/UAFBruce Finney
Terry WhitledgeDean StockwellMelanie Rohr
ADF&G/KodiakSteve Honnold
Switgard DuesterlohSteve Thomsen
General Rationale for EVOS Initiative
• Marine-Derived Nutrients from Salmon may be Important in Aquatic and Terrestrial Ecosystem Processes
• Traced into Freshwater Plankton, Juvenile Anadromous and Resident Fish
• Traced into Riparian Vegetation and Terrestrial Animals
• MDN Fluxes are Linked to Ocean Processes Through Climate, Fishing, Oil Spills
• Ecosystem-Based Management Needs Data to Determine MDN Pathways, Ecosystem Importance and Monitoring Protocols
• Basic Research Needed!
Study Design: Sampling
Sockeye (Karluk) and Control (Spiridon) Lakes
3 Year Study
9 Samplings/year (April - October)
2 Lake and 2 River (mouth) Stations at Each Lake
Full Water Column Sampling (5 m intervals to bottom)
Karluk SpiridonElevation (ft) 368 446Watershed area (106 m2) 275 54 Lake area (106 m2) 39.4 9.2Volume (106 m3) 1920 319Mean depth (m) 48 35Residence time (yr) 4.6 8.0Anadromous YES NO
Stocked
Long-term limnological and salmon data available
Site Characteristics
Study Design: Analyses
Temperature, DO, pH, light
TP, dissolved P, NO3-, Si
Chlorophyll, POM, phytoplankton, zooplankton, juvenile and adult salmon
Primary Productivity
Stable Isotopes (15N, 13C) on: POM, periphyton, zooplankton, juvenile and adult sockeye
Exploratory Studies: 15N, 13C on terrestrial plants, bears, birds
Unique Study
• Relatively well-matched pair of lakes, except for salmon
• Previous Limnological and Paleoecological data showstrong impact of MDN in Karluk Lake
• Detailed spatial and temporal sampling
• Measuring primary productivity
• Complete/integrated stable isotope analyses
15N: enriched in salmon carcasses - tracer of MDN
Comparison of Limnological Profiles Between Lakes
4 6 8 10 12 14 16 18
0
10
20
30
40
50
Kodiak Lakes - Late Aug. 2004
KarlukSpiridon
Temperature (°C)
Depth (m)
0 0.1 0.2 0.3 0.4 0.5
0
10
20
30
40
50
Kodiak Lakes - Late Aug. 2004
KarlukSpiridon
Dissolved P (uM/L)
Depth (m)
Same for Early October
0 5 10 15
0
10
20
30
40
50
Kodiak Lakes - Early June 2004
KarlukSpiridon
Nitrate (uM)
Depth (m)
0 5 10 15
0
10
20
30
40
50
Kodiak Lakes - Early Oct. 2004
Karluk
Spiridon
Nitrate (uM)
Depth (m)
0 20 40 60 80 100
0
10
20
30
40
50
Kodiak Lakes - Late Aug. 2004
Karluk
Spiridon
Si (uM)
Depth (m)
0 1 2 3
0
10
20
30
40
50
Kodiak Lakes - Early Oct. 2004
KarlukSpiridon
Chlorlophyll a (ug)
Depth (m)
Summary Part 1 (Limnology):
• Similar physical regime
• Very different ratios of major nutrientsSpiridon: P-limitedKarluk: P, Si and N limited
• Consistent with MDN sourceMDN: high P, zero Si
• Higher algal standing stock in Karluk by ~ 4X
Comparison of seasonal cycles between lakes and rivers
0
10000
20000
30000
40000
50000
60000
70000
80000
100 150 200 250 300
Karluk Sockeye Escapement
20042005
Sockeye Escapement
Julian Day
River spawners Beach spawners
0
1
2
3
4
5
6
7
100 150 200 250 300
Kodiak Lakes 2005
KarlukSpiridonKarluk riverSpiridon river
Chl a (mg/L)
Julian Day
Surface
0
0.2
0.4
0.6
0.8
1
100 150 200 250 300
Kodiak Lakes 2005
KarlukSpiridon
Primary Productivity (gC/m
2 /day)
Julian Day
2
4
6
8
10
100 150 200 250 300
Kodiak Lakes POM 2005
KarlukSpiridonKarluk riverSpiridon river
15N
Julian Day
2
4
6
8
10
0
200000
400000
600000
800000
100 150 200 250 300
Karluk Lake 2005
15 N River POM
15 N Lake POM
Cum Esc
15N
Cumulative Escapement
Julian Day
2
4
6
8
10
12
100 150 200 250 300
Kodiak Lakes:Zooplankton 2004 and 2005
Karluk 2 2004Spiridon 1 2004Karluk 2 2005Spiridon 1 2005
15N
Julian Day
6
8
10
12
14
16
18
-28 -26 -24 -22 -20
Sockeye Smolts 2006
SpiridonKarluk
15N
13C
Summary Part 2 (Temporal perspective):
• Karluk Lake higher Chl a and primary productivity by ~ 5X
• 15N higher in Karluk Lake and river phytoplankton (POM), zooplankton and juvenile sockeye relative to Spiridon Lake
• Differing seasonality: Late summer/early fall peaks in Chl a, primary productivity, biota 15N and some nutrients in Karluk
• Temporal relationships suggests influence from the early, river spawning run of sockeye: reasonable lag between escapement at downstream weir, rivers and open lake stations
• Transfer into higher trophic levels indicated
• Data support hypothesis that MDN is main control
Thanks to:
EVOS/GEM for fundingPhil Mundy
The dedicated field and lab personnel
30201003
7
11
15
Escapement/Lake area (1000s/km2)
15N
Zooplankton
Sockeye smolts
0
4
8
12
16
100 150 200 250 300
POM 2005KarlukSpiridon
15N
Julian Day
Controversy? Two Views
Salmon-derived nutrients are essential to freshwater and terrestrial ecosystems, and are key to the restoration and sustainability of salmon
Salmon-derived nutrients are not that important, and the top-down effects of escapement on lake ecosystems is substantial
Salmon-Derived Nutrients -Productivity Feedback
FreshwaterProductivity
Nutrients
SpawnerAbundance
(escapement)
Juveniles