spawning stock and recruitment relationship in north sea cod shaped by food and climate
TRANSCRIPT
3rd GLOBEC Open Science Meeting
Victoria, BC, Canada 22-26 June 2009
Spawning stock and recruitment relationship in North Sea cod shaped by food and climate
Geir Ottersen
Based on a submitted paper by
E. M. Olsen1,2, G. Ottersen1,2, M. Llope2, K.-S. Chan3, G. Beugrand4 & N. C. Stenseth1,2
1Institute of Marine Research, Norway 2Centre for Ecological and Evolutionary Synthesis, University of Oslo, Norway 3University of Iowa, USA 4National Center for Scientific Research (CNRS), France
Image: Glynn Gorick for ICES WG Cod and Climate Change
Centre for Ecological and Evolutionary Synthesis
Edwards et al. (2006)
Switch from C finmarchicus -> C helgolandicus
Marcos Llope, CEES, UiO
Increasing sea temperatures
Decline in cod abundance and biomass
North Sea Cod Juvenile Biomass
SSB 1-year old
Modelling the Spawning Stock-Recruitment
relationship for North Sea cod by a Beverton-Holt type relation??
Beverton-Holt or Ricker or both?
Modeling an environmental effect on recruitment in gadoids: Apply a family of recruitment curves depending on initial larval- and zooplankton densities Overcompensation (Ricker) at limited food levels. Beverton-Holt type relation at high food levels At low food levels the time to metamorphosis is delayed to the extent that larval mortality accumulates and makes the recruitment curve overcompensatory
Based upon theoretical work by R. Johansen (2007): A model for the interaction between gadoid larvae and their nauplii prey. Math. Bios. 208:177-192
North Sea cod
Our approch to enhance the S-R relation: Apply temperature, annual average values for the region from COADS Apply zooplankton from G. Beaugrand’s CPR based index
Data sets
1960 1970 1980 1990 2000
5010
015
020
025
0
a
SSB
(100
0 t)
1960 1970 1980 1990 2000
200
400
600
800 b
Rec
ruitm
ent (
mill)
1960 1970 1980 1990 2000
-4-2
02
4
c
Zoop
lank
ton
inde
x
1960 1970 1980 1990 2000
9.5
10.0
10.5
11.0
d
Sea
surfa
ce te
mpe
ratu
re (C
)
Model Structure 1 log(R/S) = a + log(exp(-b•S)) log(R)-log(S)=a-bS 2 log(R/S) = a – log(1 + exp(c)•S/maxS) 3 log(R/S = a + log(exp(-b•S)•(1-Z) + 1/(1 + exp(c)•S/maxS)•Z) 4 log(R/S) = a – (a1•T) + log(exp(-b·S)•(1-Z) + 1/(1 + exp(c)•S/maxS)•Z)
1 Traditional Ricker model 2 Traditional Beverton-Holt model 3 Combined Ricker-Beverton-Holt model including a zooplankton effect only 4 Combined Ricker-Beverton-Holt model including zooplankton (Z) and temperature (T) effects
A-priori set of stock (S) and recruitment (R) models
T is sea temperature and Z the zooplankton index developed by Beaugrand et al. (2002) Sea temperature is standardized to a mean of zero and a standard deviation of one. Zooplankton is standardized to range from 0 to 1
Model # Parameters AIC Support* 1 2 80.4 0 2 2 80.6 0 3 3 64.6 0.24 4 4 62.3 0.76
Model selection
*normalised Akaike weights (Burnham and Anderson 1998)
Model 4: log(R/S) = a – (a1•T) + log(exp(-b·S)•(1-Z) + 1/(1 + exp(c)•S/maxS)•Z)
Combined Ricker-Beverton-Holt model including zooplankton (Z) and temperature (T) effects
0 50 100 150 200 250
0.0
0.2
0.4
0.6
0.8
1.0
Spawning stock biomass
Zoop
lank
ton
abun
danc
e
Spawning stock biomass
Zo
opla
nkto
n Red dots = recruitment
Data points sponsored by Disney?
Conclusions Our results suggest that the stock-recruitment relationship of North Sea cod is not stationary, but that its shape depends on environmental conditions, i.e food (zooplankton) availability and sea temperature A full recovery of North Sea cod is not to be expected until the environment – both food availability and temperature - becomes more favourable