Benthic calcification in the Dutch North Sea area Frederic Gazeau NIOO-CEME Work in progress……...
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Transcript of Benthic calcification in the Dutch North Sea area Frederic Gazeau NIOO-CEME Work in progress……...
Benthic calcification in the Dutch Benthic calcification in the Dutch North Sea area North Sea area
Frederic GazeauFrederic Gazeau
NIOO-CEMENIOO-CEME
Work in progress…… Maspalomas5/12/2006
CalcificationCalcification
► CaCa2+2+ + 2HCO + 2HCO33-- ↔ CaCO↔ CaCO33 + CO + CO2 2 + H+ H22OO
► Process realized by organisms such as corals, calcifying Process realized by organisms such as corals, calcifying macroalgae, foraminifera, echinoderms, pteropods, macroalgae, foraminifera, echinoderms, pteropods, coccolithophorids, molluscs….coccolithophorids, molluscs….
► Increased atmospheric pCOIncreased atmospheric pCO22 may threatened these may threatened these organismsorganisms BUT most studies focused on corals, macroalgae and BUT most studies focused on corals, macroalgae and
planktonic calcifiersplanktonic calcifiers
► Recent experiment showed preliminary evidences that Recent experiment showed preliminary evidences that molluscs calcification will be reduced under higher molluscs calcification will be reduced under higher atmospheric COatmospheric CO22 in the range of IPCC expectations for in the range of IPCC expectations for 21002100
► Very few estimates of benthic calcification in temperate Very few estimates of benthic calcification in temperate ecosystems over large areas (last to date: Smith, 1972 ecosystems over large areas (last to date: Smith, 1972 over the Southern California shelf)over the Southern California shelf)
0
-0.25
0.25
0.50
0
r2 = 0.87, P < 0.0001
0
250 500 750 1000 1250 1500-0.25
0.25
0.50
0
r2 = 0.80, P < 0.0001
pCO2 (ppmv)
Ne
t ca
lcifi
catio
n (
mo
l Ca
CO 3
g F
W-1
h-1
)
DatasetsDatasets
► 2 datasets used2 datasets used Netherlands Institute for Fisheries Research Netherlands Institute for Fisheries Research National Institute for Coastal and Marine Management / National Institute for Coastal and Marine Management /
RIKZRIKZ
► > 130,000 records, 2,500 sampling stations, area of > 60,000 > 130,000 records, 2,500 sampling stations, area of > 60,000 kmkm22
► Data of densities and fresh weights from 1990 to 2004Data of densities and fresh weights from 1990 to 2004
► Calcimass (g CaCOCalcimass (g CaCO33 m m-2-2) calculated from fresh weight ) calculated from fresh weight vs.vs. shell weight relationshipsshell weight relationships
► Gross calcification = calcimass x turnover (yrGross calcification = calcimass x turnover (yr -1-1))► Turnover data for major species provided by Joana Turnover data for major species provided by Joana
Cardoso (NIOZ)Cardoso (NIOZ)
Only intertidal areas sampled in the Westerschelde,Oosterschelde and Wadden Sea
0
2500
5000
7500
10000
Cerastoderma edule (71%)
Macoma balthica (19%)
Other species (10%)
A
Bio
mas
s (t
FW
)
10000
20000
30000
40000
Cerastoderma edule (74%)
Crassostrea gigas (14%)
Mytilus edulis (9%)
Other species (3%)
B
0
100000
200000
300000
Cerastoderma edule (56%)
Macoma balthica (19%)
Mytilus edulis (17%)
Other species (8%)
C
Bio
mas
s (t
FW
)
100000
200000
300000
400000
500000Spisula subtruncata (59%)
Ensis (16%)
Other species (18%)
D
Asterias rubens (7%)
Species counts
Westerschelde : 5 Oosterschelde: 7 Wadden Sea: 8 Coastal zone: 38
Cockles are very important in intertidal areas
In the 0-20m area Spisula subtruncata Ensis
BiodiversityBiodiversityWhat are the major species?What are the major species?
Westerschelde Oosterschelde
Wadden Sea Coastal zone0-20 m
BiodiversityBiodiversitydepths > 20mdepths > 20m
213 species!!!!!
Clear dominance of Echinoids
Work in progress
Fresh weight / Shell weightFresh weight / Shell weight
0 10 20 300
10
20
30Cerastoderma edule
Mytilus edulis
Crassostrea gigas
Macoma balthica
Spisula subtruncata
Ensis
Fresh weight (g)
Shel
l wei
ght (
g)
0.0
0.5
1.0
1.5
2.0
2.5
3.0
3.5
Tur
nove
r (P
/B in
yr
-1)
Cerastoderma edule
Mytilus edulis
Crassostrea gigas
Macoma balthica
Spisula subtruncata
Ensis
1 year
2 years
≥3 years
1 year
2 years
≥3 years
1 year
2 years
≥3 years
Turnover = Growth rateTurnover = Growth rate
Data from Joana Cardoso (NIOZ)
All data based on SHELL growth
OosterscheldeOosterschelde
► No large temporal variationsNo large temporal variations
► Cockles are the main producersCockles are the main producers
► BUT:BUT: Oysters were not well sampledOysters were not well sampled
► Kater (2003): Kater (2003): ► >300 g CaCO>300 g CaCO33 m m-2-2 yr yr-1-1
Important aquaculture site in Important aquaculture site in the Netherlands (oysters and the Netherlands (oysters and mussels)mussels)
► Based on production values Based on production values provided by the Dutch Fish provided by the Dutch Fish Product BoardProduct Board
Mussels: 100 g mMussels: 100 g m-2-2 yr yr-1-1
Oysters: > 500 g mOysters: > 500 g m-2-2 yr yr-1-1 19
9019
9219
9419
9619
9820
0020
0220
040
10
20
30
40
50
60
70
80
90Cerastoderma edule
Mytilus edulis
Year
G (
g C
aCO
3 m
-2 y
r-1)
Westerschelde estuaryWesterschelde estuary
► No aquacultureNo aquaculture
► Cockles are the main Cockles are the main producersproducers
► Very low calcimass and Very low calcimass and calcification ratescalcification rates
1992
1994
1996
1998
2000
2002
2004
0
5
10
15
20
25
Macoma balthicaCerastoderma edule
Year
G (
g C
aCO
3 m
-2 y
r-1)
Wadden SeaWadden Sea
► Large variations:Large variations: 5-155 g CaCO5-155 g CaCO33 m m-2-2 yr yr-1-1
► Wild mussels are the main producersWild mussels are the main producers
► Also an important site for Also an important site for aquacultureaquaculture
But large ecosystem (2700 kmBut large ecosystem (2700 km22)) Mussel culture covers 15% of the Mussel culture covers 15% of the
surface area of the Dutch surface area of the Dutch Wadden SeaWadden Sea
► 8 g CaCO8 g CaCO33 m m-2-2 yr yr-1-1 19
9019
9219
9419
9619
9820
0020
0220
040
100
200
Macoma balthicaMytilus edulis
Cerastoderma edule
Year
G (
g C
aCO
3 m
-2 y
r-1)
Coastal zone (0-20 m)Coastal zone (0-20 m)
► Very large variationsVery large variations
► Values between 1 and Values between 1 and 28 CaCO28 CaCO33 m m-2-2 yr yr-1-1
1994
1995
1996
1997
1998
1999
2000
2001
2002
2003
2004
0
5
10
15
20
25
30
35Ensis
Spisula subtruncata
Year
G (
g C
aCO
3 m
-2 y
r-1)
Gross calcificationg CaCO3 m-2 yr-1
Cerastoderma edule 24 Mytilus edulis 11Crassostrea gigas* 328Culture Mytilus edulis 100Culture Crassostrea gigas 550Sub-Total ~1000
Cerastoderma edule 8 Macoma balthica 1 Sub-Total 9
Cerastoderma edule 21 Macoma balthica 1 Mytilus edulis 43
Culture Mytilus edulis 8Sub-Total 73
Spisula subtruncata 4 Ensis 6 Sub-Total 10
15 mmol CO2 m-2 d-1
Oosterschelde
Westerschelde
Wadden Sea
Coastal zone0-20 m
0.2 mmol CO2 m-2 d-1
1.2 mmol CO2 m-2 d-1
0.3 mmol CO2 m-2 d-1
Derived CO2 fluxes(ψ = CO2/CaCO3 of 0.6)
* Derived from Kater (2003)
Coastal zone> 20 m
Work in progress…….
Close to coral reefs estimates
Low values
Preliminary conclusionsPreliminary conclusions
► Aquaculture is very important and represents a main source of Aquaculture is very important and represents a main source of carbonate productioncarbonate production
► COCO22 production by gross calcification production by gross calcification► COCO22 production by shell burning production by shell burning
► Oosterschelde close to coral reef production (Milliman: 1500 g CaCOOosterschelde close to coral reef production (Milliman: 1500 g CaCO33 mm-2-2 yr yr-1-1))
► Small values for the coastal zone, Westerschelde estuary and Small values for the coastal zone, Westerschelde estuary and Wadden SeaWadden Sea
► A low total Dutch North Sea benthic calcification rate is expectedA low total Dutch North Sea benthic calcification rate is expected► < Milliman’s estimate for shelves (20-100)< Milliman’s estimate for shelves (20-100)► << Smith’s estimate for the Southern California shelf (400)<< Smith’s estimate for the Southern California shelf (400)
Future workFuture work
► Gross calcification in the >20m areaGross calcification in the >20m area► Shell removal by fisheries (Shell removal by fisheries (knownknown))► Estimates of shell removal by birds (Estimates of shell removal by birds (knownknown))► Data on shell weight in sediments (Data on shell weight in sediments (knownknown))
Together with sedimentation rates Together with sedimentation rates estimatesestimates
► Estimate of net accumulation rates and net Estimate of net accumulation rates and net COCO22 fluxes fluxes