obey the law: calanus finmarchicus dormancy explained
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Obey the LAW: Calanus finmarchicus dormancy explained. Jeffrey Runge School of Marine Sciences, University of Maine and Gulf of Maine Research Institute Andrew Leising NOAA, Southwest Fisheries Science Center Catherine Johnson University of British Columbia. Objectives: - PowerPoint PPT PresentationTRANSCRIPT
Obey the LAW: Calanus finmarchicus dormancy explained
Jeffrey RungeSchool of Marine Sciences, University of Maine and
Gulf of Maine Research Institute
Andrew LeisingNOAA, Southwest Fisheries Science Center
Catherine JohnsonUniversity of British Columbia
Objectives:
•Identify environmental processes that control dormancy in Calanus finmarchicus
•Develop a mechanistic understanding of dormancy for inclusion in population dynamics modeling
Approach:
•Compile Calanus and environmental data across regions in the NW Atlantic
•Look for common patterns and cues
•Using individual-based models, develop quantitative hypotheses to explain patterns
Proxies for dormancy entry and exit
Entry: Fifth copepodid (CV) half-max proxy
Dormant when… CV proportion >= x-bar /2 where x-bar = average max. CV
proportion over all years
1. Exit:Emergence when…
1. Adult (CVI) proportion >= 0.1
2. Back-calculation from early
copepodid appearance, using
development time-temperature
relationship
Copepodids Nauplii
AdultsDormancyat CV stage
Data sources
Data from:
DFO – AZMP: 1999 – 2005 (E.Head, P.Pepin)
DFO – IML:1990 – 1991 (S. Plourde, P. Joly)
US-GLOBEC: 1995 – 1999 (E. DurbIn, M. Casas)
PULSE – NEC: 2003 – 2005 (R. Jones)
AG: Anticosti Gyre, NW Gulf of St. LawrenceS
tage
Pro
port
ion
Abu
ndan
ce (
no.
m-2)
Photoperiod at emergence and onset
Rimouski
Anticosti Gyre
Newfoundland
Scotian Shelf
Day
leng
th (
h)
Day of Year
Emergencedate
Previousand nextdate
Temperature at 5 m
Tem
pera
ture
(°C
)
Rimouski
Anticosti Gyre
Newfoundland
Scotian ShelfOnsetEmergence
Climatological temperature at
5 m
OnsetEmergence
Rimouski
Anticosti Gyre
Newfoundland
Scotian Shelf
Tem
pera
ture
(°C
)
Mean chlorophyll-a, 0 – 50 m
Chl
-a (
mg
m-3)
Rimouski
Anticosti Gyre
Newfoundland
Scotian Shelf
Chl-a values truncated at 1.6 mg m-3
(threshold forgrowth)
Onset
Emergence
Conclusions• No single observed environmental cue
explains dormancy patterns• Dormancy entry and emergence occur over a
broad range of times, both among individuals and years
• The mechanistic understanding of dormancy transitions must involve interaction of multiple environmental factors. We propose a “Lipid-Accumulation Window” hypothesis to explain observed life history patterns.
Growth of Neocalanus plumchrus copepodids in the southeastern Bering Sea
Development time is a function of temperature and food concentration in Calanus finmarchicus
Campbell, R. M. Wagner, G. Teegarden, C. Boudreau and E. Durbin. 2001. Growth and development rates of the copepod Calanus finmarchicus reared in the laboratory. Mar. Ecol. Prog. Ser. 221: 161-183
Miller et al. 1977.Growth rules in the marine copepod genus Acartia. L&O. 22: 326-335.
Lipid Accumulation Window hypothesis:Step 1 - Conditions allowing dormancy: suppose only copepods with > 50% lipid content can enter
Integrated Temperature
Integrated
Food
Fraction lipid content at end of CV stage
0.0
0.5
0.1
0.2
0.3
0.4
Lipid accumulation window hypothesis:Step 2 - Temporal Filter
Time
Favorable Env. Conditions
Cumulative conditions that will allow dormancy in CIV and CV
Lipid Threshold
Lipid accumulation window hypothesis: Step 2 - Temporal Filter
Time
Favorable Env. Conditions
Cumulative conditions that will allow dormancy Resulting
period when they go dormant
Lipid accumulation window hypothesis: Step 3 - Predation Filter
Time
Favorable Env. Conditions
Predation Removal here
Resulting population entering dormancy
Missing cohort here
Lipid accumulation window hypothesis: Step 4 - Emergence Timing linked to Entry
Emergence survival linked to entry and Env.
Time
Favorable Env. Conditions
JanJan
Population entering dormancy
Population exiting dormancy
Successful females
Dormancy Length, f(T during dormancy,% lipids at entry)
Testing the hypothesis1. Identify lipid accumulation windows by starting individual-based
model runs, driven by temperature and chlorophyll, at each date
Time
Chl
orop
hyll
(mg
m-3)
Tem
pera
ture
(°C
)
…
Pot
entia
l lip
id
accu
mul
atio
n
Time
Threshold for onset of dormancy
2. CVs produced during the lipid accumulation window can enter dormancy
Utility of the model for this calculation• Growth and development are decoupled• Ability to include temporally variable forcing data (food
and temperature)• Can include or ignore predation filter• Mechanistic and physiological basis for growth and
developmentExample for Calanus pacificus
0
20
40
60
80
100
120
140
0 10 20 30 40 50
Time (days)
Weig
ht
(µg
C)
Model 8 DegreesModel 12Model 16Observed Data 8Observed Data 12Observed Data 15.5
Example Results for C. pacificus
•Top figure is based on climatology from NH20, Newport Line, OR; Bottom figure based on SCB climatology
•In the south, copepods spawned as early as day 50 can enter dormancy, whereas in the north, it’s 40 days later.
•Peak dormancy entrance date is between days 125-175 in the S, and between days 175-225 in N.
•Predation during the “Green” period would remove potentially successful copepods
•Suboptimal cold temperatures(and low food) in the N during the early part of the year limit success then, whereas overly warm temperatures later in the year limit success in S during that time (recall the optimal window)
Final Conclusions• Our findings for C. finmarchicus, C. pacificus and C.
marshallae strongly suggest that multiple environmental factors are the likely cues for dormancy, as these copepods enter and exit dormancy over a wide range of times and conditions.
• Our modeling results (for C. pacificus so far) suggest that lipid accumulation (or some equivalent storage compound) is a likely player in how dormancy is triggered.
• OBEY THE LAW!!!!
Implications
• Previous coupled 3-d physical-biological models of Calanus have forced dormancy transitions empirically using an advective-diffusive approach
• While these models provide diagnostic insight, they cannot be used for prediction
• A mechanistic, coupled IBM-physical model that tracks lipid accumulation is needed to understand and predict Calanus population responses to climate changes