The potential of shoreface nourishments for habitat enhancement A - - PowerPoint PPT Presentation
The potential of shoreface nourishments for habitat enhancement A - - PowerPoint PPT Presentation
The potential of shoreface nourishments for habitat enhancement A case of the Sand Engine lagoon as a nursery for juvenile plaice ( Pleuronectes platessa L.) Lotte Meeuwissen, Ralf van Hal, Lorna Teal, Marjolein Post Sand engine; mega
Sand engine; mega nourishment 2011
The Netherlands: Ter Heijde
Lagoon Lagoon Lagoon
1.5 km 21.5 Mm3 128 ha sand Shallow artificial lagoon Pilot project for sustainable coastal protection 2 km
Over time…
October 13, 2011 May 14 , 2012 July 1 , 2013
Lagoon Lagoon Lagoon
Lagoon as nursery area?
Plaice (Pleuronectes platessa L.)
§ Dutch shallow coastal area as nursery area
- Entering larvae (0-group): March and April
§ Changing habitat requirements
- Increasing length à More coarse sand and lower temperatures
§ Spatial distribution pattern change during life cycle
- Increasing length à Optimal temperature and tolerance range
Growth (cm day -1) Temperature (°C) 5 10 15 20 25 30 0.00 0.05 0.10 0.15
Temperature (°C)
40 cm 25 cm 10 cm (Teal et al., 2010)
Effect of nourishment on coast
Habitat enhancement
SHALLOW WATERS HIGHER GROWTH SEA WATER TEMPERATURE RISES
Material and Methods; fieldwork
Every 2 weeks: 2012: end of April – end of August 2013: mid May – mid August 2 m beam trawl Mesh size: 1 and 2 cm Depth: 1.5-3 m and 4-5 m 1-3 trawls Distance and time Temperature Numbers and length of 0-group plaice à predominant flatfish species
Material and Methods; nursery quality
§ Numbers in m2 § Growth in mm per day § Estimates of growth potential
Comparing predicted and observed growth: Dynamic Energy Budget (DEB) modelling (ad lib.) (Van der Veer, 2009; Teal et
al., 2012)
Growth and DEB: only lagoon and area South 2012 compared
Results; numbers
2012: Density lagoon increased, peak end of May, decrease till the end Density North and South 0 at beginning, later low 2013: Density lagoon decreasing Plaice present in North and South Density lower in all areas in 2013
Difference in axes!
Results; length
2012: Smallest plaice in lagoon Biggest plaice in South 2013: Bigger plaice in additional areas. At the beginning plaice in lagoon bigger than in 2012 Smaller sizes in 2013 than in 2012
Results; growth
Lagoon: Peak in growth rate South: Increasing growth rate
Results; Dynamic Energy Budget Model
Lagoon: Observed growth lower than predicted growth South: Observed and predicted growth more equal
Discussion; numbers
§ Lagoon suitable habitat for flatfish
- Mainly plaice
§ Lagoon increased attraction in 2012
- Fluctuation in larvae supply
Determined by year-specific abiotic and biotic conditions
- Changing morphology
Discussion; growth
§ Similar growth pattern found in Balgzand 1975-1988 and
1990-2002 (north-eastern North Sea) and Ems estuary Wadden Sea 1992 (Teal et al., 2008, Jager et al., 1995)
§ Lower growth rates due to food limitation
- Supported by DEB
- Lagoon nearly a closed system
§ Outer areas harbour better growth conditions
Habitat enhancement with nourishment?
§ Lagoon temporary nursery area
- Only in 2012 habitat enhancement due to design
Sand Engine
§ Size of the Sand Engine § Species specific habitat preferences
Questions?
Meeuwissen, L., van Hal, R., Teal, L., Post, M.H.M., 2017, Journal of Sea Research, In review The potential of shoreface nourishments for habitat enhancement: a case of the Sand Engine lagoon as a nursery for juvenile plaice (Pleuronectes platessa L.) Contact: lottemeeuwissen@live.nl
Many thanks to: Adriaan Rijnsdorp Shore Symposium
Still looking for a job ;-)
16
Species Lagoon South North Far South Plaice (Pleuronectes platessa) Sole (Solea solea) Turbot (Scophthalmus maximus) Dab (Limanda limanda) Common shrimp (Crangon crangon) Goby species (Pomatoschistus species) Sprat (Sprattus sprattus) 2012 2013 2012 2013 2012 2013 2013 325
- 1
459 100 6 84
- 95
35 3 52 4 5 3 304 94 33 113 1 6 5 5795 395
- 12
1 3
- 711
34 17 12 4 5 3 7833 188 1 49 1 5 3 5888 5336 4
Total numbers per species caught per sampled area in 2012 and 2013.
July 2017
Temperature
The average seawater surface temperature (°C) of the trawls for every date in each sampling area in 2012 (solid black lines) and 2013 (grey dotted lines).
Sampling area Mesh size Depth 24- April 2- May 23- May 7- June 20- June 26- June 27- July 10- Aug 29- Aug Lagoon 1 cm 1.5-3 m 1 2 1 1
- 1 cm
4-5 m 1 1 1
- South
1 cm 1.5-3 m 1 2 2 2 1
- 1 cm
4-5 m 1 2 2 2 1
- North
1 cm 1.5-3 m 1 1 2 2 1
- 1 cm
3.5-4.5
- 1
- Lagoon
2 cm 1.5-3.5 m
- 2
2 1 1 2 5 2 cm 3-4 m
- 1
- 3
2 cm 4-5 m
- 1
- 1
1 2 2 South 2 cm 1.5-3.5 m
- 2
3 2 3
- 2 cm
4-5.5 m
- 1
2 2 2
- North
2 cm 1.5-3.5 m
- 1
1 2 1
- 2 cm
3.5-4.5 m
- 1
- Total
5 9 8 10 10 9 8 10 10 The number of performed trawls per sampling area per day with corresponding depth and used mesh size of the beam trawl in 2012.
Sampling area Mesh size Depth 16-May 28-May 11- June 2- July 17-July 23-July 20-Aug Lagoon 1 cm 1.5-3 m
- 1
- 2
1 1 1 cm 4-5 m 1 1
- 1
1 1 1 Far south 1 cm 1.5-3 m 1 1 1 1 1 1 1 1 cm 4-5 m 1 1 1 1 1 1 1 South 1 cm 1.5-3 m 1 2 1 1 1 1 1 1 cm 4-5 m 1 1 1 1 1 1 1 North 1 cm 1.5-3 m 1 1 1 1 1 1 1 Lagoon 2 cm 1.5-3 m 1 1 1 1 2 1 1 2 cm 4-5 m 1 1 1 1 1 1 1 Far south 2 cm 1.5-3 m 1
- 1
1 1 1 1 2 cm 4-5 m 1 2 1 1 1 1 1 South 2 cm 1.5-3 m 1
- 1
1 1 1 1 2 cm 4-5 m 1 1 1 1 1 1 1 North 2 cm 1.5-3 m 2 1 1 1 1 1 1 2 cm 4-5 m
- 1
- Total
14 14 13 13 16 14 14 The number of performed trawls per sampling area per day with corresponding depth and used mesh size of the beam trawl in 2013.
21
In order to calculate the growth rate per day of the 0-group plaice which had been caught on the first sampling day a reference length of 12 mm at 1 March was used, derived from a research performed in the western Wadden Sea (Van der Veer, 1986).
DEB Model
22
!" !# = &' ṗ
)* +, -./0 1[3*]× 678
9: 9;<=19: 9
" &' >? @[>A]
The effect of temperature on physiological rates in the DEB model is incorporated by multiplying the rates with an enzyme fraction that is in its active state (Kooijman, 2010). This fraction Fr is calculated as: 𝐺𝑠 = exp 𝑈
H
𝑈IJ' − 𝑈
H
𝑈 × 1 + exp 𝑈
HN
𝑈IJ' − 𝑈
HN
𝑈N + exp 𝑈
HO
𝑈O − 𝑈
HO
𝑈IJ' 1 + exp 𝑈
HN
𝑈 − 𝑈
HN
𝑈N + exp {𝑈
HO
𝑈O − 𝑈
HO