MODELLING THE GROWTH OF MYTILUS EDULIS(L.) BY COUPLING A
Transcript of MODELLING THE GROWTH OF MYTILUS EDULIS(L.) BY COUPLING A
Spot Image, 1999, with shellfish leases and polders represented (GIS in development)
MODELLING THE GROWTH OF MYTILUS EDULIS (L.) BY COUPLING A DYNAMIC ENERGY BUDGET MODEL WITH SATELLITE DERIVED ENVIRONMENTAL DATA
Yoann Thomas, Joseph Mazurié, StéphanePouvreau, Cédric Bacher, Francis Gohin,
Caroline Struski, Patrick Le Mao
Ifremer Brest, La Trinité/mer, Saint-Malo
Ackowledgments to the SRC-BN (Section Régionale de la Conchyliculture de Bretagne Nord)
fot its support
Sedimentary enclave of 500 km2
intertidal zone of 240 km2
Bed communities dominated by suspension feeders, both natural, cultivated and invasive
Mont Saint-Michel bay
The site and shellfish farming
Yoann Thomas
Oyster O. edulisStock 3000 tonsProduction 1500 tons
Oyster C. gigasStock 8000 tonsProduction 5000 tons
Mussel M. edulisStock 10-12000 tonsProduction 10-12000 tons (~320,000 poles)
2003->2006 :spatial reorganisation of shellfish leases
1- 150 000 mussel poles ->Easward (more productive ?)
1
2- 150 ha of oyster leases -> Eastward (less muddy)
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=> Questions about Carrying Capacity of the Bay ?
Objective of the study
develop a growth model of Mytilus edulis based on Dynamic Energy Budget Theory (Kooijman, 2000)
Within the framework of
Assess the variability of mussel growth with respect to spatial and temporal variability of environmental parameters
Use Satellite data as forcing variables (spatially available)
Summary
1. Growth data (sampling strategy, variables)
2. Satellite data(Sources, data, validation, images…)
3. Model implementation(assumptions, calibration, application at two scales)
4. Discussion-Conclusion
I- Growth data acquisitionSAMPLING 3x5 Poles from 5 zones (A, B, C, D, E) harvested every 2 month, (april to dec. 2004) and then sub-sampled for measurements
A B
C
D
E
extension
1 km
Mussel growth april to oct 2004
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who
le w
eigh
t per
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sell
(g) E
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B
C
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=> Growth exhibits a positive gradientbetween ancient area (A, B, C)
and new area (D, E)(mainly acquired during the 1st year 2003)
GROWTH VARIABLES Whole, shell, meat weights…(2nd year of growth)
1st year 2003
2nd year2004
II- Satellite Imagery : (1) Sources
ftp://ftp.ifremer.fr/ifremer/cersat/products/gridded/ocean-color/
Data (Geotiff, NetCdf)
http://www.ifremer.fr/nausicaa/marcoast/index.htm /roses/index.htm
/gascogne/index.htm/medit/index.htm
Maps(on simple registration)
II- Satellite imagery : (2) data used
(1) Seawater surface temperature : NAR/NOAA satellites 2 Satellites operate at 8 h intervals surface temperature is calculated from two thermic infrared wave length spatial resolution of 1.1 km – 2 kmThermic resolution 0.12°C:
(2) Chlorophyll ASeaWIFS Sensor (OSC /SeaStar) (1998-2004) Daily coverage 12h-14h UT Spatial resolution 1 km²Reflectance data analyzed at Ifremer- Brest
(empirical look-up table OC 5 for the coastal domain Gohin et al. 2002)
MODIS Sensor (GSFC-Nasa) Since 2002 (free an unrestricted data)
"Ocean color data used in this study were produced by the SeaWiFS Project at Goddard Space Flight Center. The data were obtained from the Goddard Earth Sciences Distributed Active Archive Center under the auspices of the National Aeronautics and Space Administration. Use of this data is in accord with the SeaWiFS Research"
Reference : Gohin F., Druon J.N., and L. lampert, 2002 A five channel chlorophyll algorithm applied to SeaWiFSdata processed by SeaDAS in coastal waters,, International Journal of Remote Sensing, Vol. 23 , 8, pp 1639-1661,
II- Satellite imagery(3) validation of Chl-A locally
Cancale station, Years 2003-2004 :
good fit
Chlorophyll A (2003-2004) compared between field samples and Satellite estimations (SeaWIFS, MODIS)
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CHLa-fied sampleCHLa_ModisCHLa-Seawifs
Ifremer REPHY monitoring station at Cancale, provides data every 15 days, since1992, on water quality (temperature, salinity, suspended matter, phytoplankton…) (www.ifremer.envlit)
5 Mussel growth sampling stations
=> Compared with Satellite data from the nearest pixel (SeaWifs or Modis)
Modis OC5 IFR Choro 02/08/2003
Modis OC5 IFR Choro 04/10/2003
Modis OC5 IFR Choro 24/01/2003
Modis OC5 IFR Choro 06/05/2003
II-Satellite imagery : (3) Typical Chl-A images, per season
III Growth model (1) experimental sources for main assumptions
Food source = phytoplankton
(Chl-a)
Isotopic markers : Mussels food : 80 % ocean POM (mainly Phytoplankton)
Riera (2007)
Food ingestion = Maximum ingestion rate : experimental (Pouvreau, Ifremer)
Reproduction period and
effort
From histology (Donval, Brest Un.) => Spawnings in march-april
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INIT-2ans PONDU-2ans
TDW
(g)
perte = 34%
Experimental spawnings at lab =>34% weight loss
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j j a s o n d j f m a m j j a s o n d j
Poid
s en
tier (
g)
HoLesimulé-Hermelles
Growth data
The DEB Modeldetailed in next presentations
III Growth model : (2) calibration
Ingestion as a function of Food
density
Ing.max
50 %
Xk X : [Food concentration]
This parameter is not yet independent of sites (« generic »)(does not catch all the trophic differences between sites)
=> has been adjusted ( best fit between growth simulations and observations )
Xk = 2.1 µg.l-1 Chla, in this model
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Concentration (10-3cell.ml-1)
Inge
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-1)
Ing(X) = Ing.max
X + Xk
Forster & Smith (1975)
X
Xk, a key factor for energy acquisition,most parameters from van der Veer et al. (2006)
III- Growth Model (3) applied to 5 mussel sites
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f m a m j j a s o n d j f m a m j j a s o n
Date (month)
Tem
pera
ture
(°C
)
A B C D E
5 Temperature series
5 Chl-A series averaged per zone of 14 pixels (lack of
data with 1 pixel)
Monthly satellite Chlorophyll A, in 5 stations from Jan. 2003 to Dec. 2004
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Chl
.a (µ
g/L)
ABCDE
Whole weight simulated from march 2003 to oct.2004
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who
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eigh
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Positive growth
gradient from West (A) to
East (E) may be roughly
represented
Questionable point 1 : zones
limits
Questionablepoint 2 : initial
conditions uncertain
III Growth Model : (4) applied at bay scale
378 pixels of Chla monthly
averages
378 pixels of Temperature
monthly averages
Simulated Weight at harvest
Final whole weight as a function of mean Chl- A
y = 9.4x - 3.6R2 = 0.85
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mean Chl-A over growth period
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l Who
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eigh
t (g)
Mean Chl-A => Weight at harvest (after 18 month growth)
Conclusion : Main Results
1- Temperature, Chl-A (and suspended matter) appear to be fairly estimated by existing treatments of satellite seawater reflectance data.
2- Ecophysiological models (specially of DEB type) establish the relationship between these environmental parameters and Growth of various species
=> Forcing of ecophysiological Growth Models with satellite environmental data broadens their field to application (habitat suitability, aquaculture potential, GIS…)
Discussion : limits of the study, perspectives
1. Limits of the growth data useduncontrolled initial conditions, sampling variations…=> (use of experimental standard mesh bags…)
2. Spatial & temporal resolution of satellite images• Spatial resolution 1 km unsufficient for small scale studies : improved in future satellite-
sensors
• Moreover, In the intertidal area (border of images), temporal series have to be completedfrom neighbour pixels => grouping to be optimized
3. Effectiveness of Chl-a as food indicator ?Seasonal variations in Chl-a content of Phytoplankton (photo-adaptation)Phytoplankton cell size and qualitydetritic food…
4. Unability to answer to carrying capacity evaluations that require dynamic modellingnot only of energy budgets, but also ofhydrodynamics and primary production
Hydro-Sediment
Model
Primary Production
Model
Molluscs Bioenergetics
Model