Diel-depth distributions of fish larvae off the Balearic ... · Diel-depth distributions of fish...
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Diel-depth distributions of fish larvae off the Balearic Islands (western Mediterranean) under two environmental scenarios
M P Olivar1 A Sabatés1 F Alemany2 R Balbín2 and A Pérez2M. P. Olivar , A. Sabatés , F. Alemany , R. Balbín and A. Pérez
1 Institut de Ciències del Mar (CSIC), Passeig Marítim 37-49, 08003 Barcelona, Spain.
2 Centre Oceanogràfic de Balears Instituto Español de Oceanografía IEO Palma de Mallorca Spain2 Centre Oceanogràfic de Balears. Instituto Español de Oceanografía, IEO. Palma de Mallorca, Spain.
OUTLINE
Introduction on ichthyoplanktonIntroduction on ichthyoplankton
Objectives
Material and Methods
General hydrographic featuresy g p
Results:
Comparisons of integrated abundanceComparisons of integrated abundance
Larval assemblages
Vertical patterns (day-night and size stratification)
Conclusions
INTRODUCTION: Life cycle of fishes
LARVAE
Meso & macrozooplankton 0-200 mp
TRANSFORMING
ADULT
JUVENILE
RECLUTAMIENT PROCESS (Houde 1987)
OBJECTIVES
Objective
Analyse the effect of seasonal variability on the early developmentalAnalyse the effect of seasonal variability on the early developmental stages of fishes that live and reproduce on the shelf and slope off the Balearic region
Determine the diel-depth vertical distribution of the different species in relation to the environmental situation
OCEANOGRAPHIC STUDY REGION
MATERIAL AND METHODS
OCEANOGRAPHIC CRUISES
STUDY REGION
December 2009 July 2010
L b SAMPLING
Environment
Lab. Fish larvae
CTDStratified collectionStratified collection
HYDROGRAPHY: Vertical structure
December 2009December 2009
July 2010
HYDROGRAPHY: Integrated fluorescence
December 2009 July 2010y
0
25
0 0.2 0.4 0.6 0.8 1 1.2
Fluorescence
(m)
0
25
50
0 0.2 0.4 0.6 0.8 1 1.2
Fluorescence
(m)
50
75
100
Dep
th (50
75
100
Dep
th
MATERIAL AND METHODSDecember July
°N
39.8
1 21000 m
200 m
Mallorca Island
39.3
0.25 m21 m2
800 mCabrera
MultinetDecember 2009
. CTD
°E1.8 2.3 2.8 3.338.8
MocnessJuly 2010
Fixed stations 24-48
RESULTS: INTEGRATED DATA. DIFFERENCES AMONG ZONES
39 species1.6December 2009
3.5December 2009 39 species
1.2
1.4
N. S
pp
December 2009
2.5
3.0
abun
danc
e
December 2009
Autumn
CShelf Slope0.8
1.0
log
CShelf Slope1.5
2.0lg to
tal
60 speciesSummer
C S
Shelf SlopeBathymetric strata
C S
Shelf SlopeBathymetric strata
1 4
1.5
1.6July 2010
3 0
3.2
3.4
ance
July 2010
1.1
1.2
1.3
1.4
log
N. S
pp
2 2
2.4
2.6
2.8
3.0
log
tota
l abu
nda
C S
Shelf SlopeBathymetric strata
0.9
1.0
C S
Shelf SlopeBathymetric strata
2.0
2.2l
Higher number of species in summerThe majority of the species were present both in the Cabrera and Sóller zonesDominance of mesopelagic larvae both at shelf and slopep g p
RESULTS: GROUPS OF SAMPLESDecember 2009
Hlvl2D Stress: 0.14 range mHlvlSURTbTbDL
g0-6060-90
90-100-120100-120-300
>300
no significant differences by zone orbathymetric strata
July 2010lvlHid
SUR
2D Stress: 0.16
SURTbTbDL
i ifi t diff i l tirange m
significant differences in relation to the level of the water column
i ifi t d i ht diff
0-2525-5050-100100-300
>300significant day-night differences
High overlapping among surface and thermocline samples
RESULTS: GROUPS OF SPECIES TRANSFORMING AND JUVENILES
0-150 -100 -50 0 50
N/1000 m3
0-400 -200 0 200
N/1000 m3
0
100
200
0
100
200200
300
400pth
(m)
200
300
400pth
(m)
500
600
Dep
500
600
Dep
700
800
Cyclothone braueriDecember Slope
700
800
Cyclothone braueriJuly Slope
e.g., T & J C. braueri
RESULTS: GROUPS OF SPECIES *DEEP LARVAE
0-8 -4 0 4 8
N/1000 m3
0-8 -4 0 4 8 12
N/1000 m3
0
100
200
0
100
200200
300
400pth
(m)
200
300
400pth
(m)
500
600
Dep
500
600
Dep
700
800
Argyropelecus hemigymnusDecember Slope 700
800
Argyropelecus hemigymnusJuly Slope
FlexionPreflexion
PostflexionTransforming
RESULTS: GROUPS OF SPECIES *SUR & T DECEMBER 2009
B. glaciale C. maderensis C. braueri H. benoitiB. glacialeB. glaciale
105
75
45
15
105
75
45
15
105
75
45
15
105
75
45
15
105
75
45
15
105
75
45
15
4 2 0 2 4 6 8
155
25 20 15 10 5 0 5
155
150 100 50 0 50 100
155
60 40 20 0 20
155
15
H. hygomii
15
L. crocodilus
15
L. pusillus
15
L. dofleini
4 2 0 2 4 6 8
155
4 2 0 2 4 6 8
155
155
105
75
45
155
105
75
45
155
105
75
45
155
105
75
45
60 40 20 0 20 15 10 5 0 5 10 15 100 50 0 50 40 30 20 10 0 10
45
15
S. veranyi
45
15
V. attenuata
45
15
S. pilchardus
45
15
Lestidiops sp.
20 15 10 5 0 5 10
155
105
75
30 20 10 0 10
155
105
75
60 40 20 0 20 40
155
105
75
15 10 5 0 5 10
155
105
75
*Distribution in the *upper mixed layer and thermocline. Higher concentration at the gradient zone at night. Vertical sinking and retention at the thermocline Shallower distribution during the day. Higher light intensity. Higher food availability?
*
RESULTS: GROUPS OF SPECIES SURFACE JULY 2010
0-25
Arnoglossus
0-25
A. rocheiA. rochei
0-25
E. encrasicolus
0-25
T. draco
151-200
126-150
101-125
76-10051-75
26-50
151-200
126-150
101-125
76-10051-75
26-50
151-200
126-150
101-125
76-10051-75
26-50
151-200
126-150
101-125
76-10051-75
26-50
40 30 20 10 0 10 20 30 20 10 0 10 20 30 20 10 0 10 20 15 10 5 0 5 10
51-75
26-50
0-25
T. thynnus
51-75
26-50
0-25
T. mediterraneus
76 10051-75
26-50
0-25
C. julis
51-75
26-50
0-25
S. hepatus
20 15 10 5 0 5 10
151-200
126-150
101-125
76-100
4 2 0 2 4
151-200
126-150
101-125
76-100
20 10 0 10
151-200
126-150
101-125
76-100
C. pygmea D. holti
4 2 0 2 4
151-200
126-150
101-125
76-100
126-150
101-125
76-10051-75
26-50
0-25
pyg
126-150
101-125
76-10051-75
26-50
0-25
D. holti
SUR
50 40 30 20 10 0 10
151-200
4 2 0 2 4
151-200
6 50
Larvae restricted to the surface both day and nightLarvae restricted to the surface both day and nightMostly shelf dwelling species
RESULTS: GROUPS OF SPECIES JULY 2010
0-25
C. maderensis
0-25
C. braueri
0-25
H. benoiti
0-25
L. dofleini
SURFACE & THERMOCLINE
151-200
126-150
101-125
76-10051-75
26-50
151-200
126-150
101-125
76-10051-75
26-50
151-200
126-150
101-125
76-10051-75
26-50
151-200
126-150
101-125
76-10051-75
26-50
*800 600 400 200 0 200 400 600 400 200 0 200 400 1000 500 0 500 1000 10 5 0 5 10
51-75
26-50
0-25
L. crocodilus
51-75
26-50
0-25
L. pusillus
51-75
26-50
0-25
S. veranyi
51-75
26-50
0-25
V. attenuataTHERMOCLINE
60 40 20 0 20 40
151-200
126-150
101-125
76-100
20 10 0 10 20 30
151-200
126-150
101-125
76-100
20 15 10 5 0 5
151-200
126-150
101-125
76-100
20 10 0 10
151-200
126-150
101-125
76-100
BELOW THERMOCLINE
101-125
76-10051-75
26-50
0-25
B. glaciale
101-125
76-10051-75
26-50
0-25
Lestidiops spp
101-125
76-10051-75
26-50
0-25
M. puctatum
101-125
76-10051-75
26-50
0-25
N. rissoiBELOW THERMOCLINE
150 100 50 0 50
151-200
126-150
100 50 0 50 100
151-200
126-150
40 30 20 10 0 10
151-200
126-150
0 5
15 10 5 0 5 10
151-200
126-150
No shallower concentration during daylight hours
RESULTS: LARVAL SIZE STRATIFICATION. MYCTOPHIDS
-30 -20 -10 0 10N/1000 m3
-400 -200 0 200 400N/1000 m3
0
50
)
0
50
)
100
150
Dep
th (m
)100
150
Dep
th (m
)
PreflexionFlexion
200
Hygophum benoitiDecember Shelf
Hygophum benoitiJuly Shelf
200
-20 -10 0 10N/1000 m3
Postflexion
0
50
20 10 0 10 Preflexion stages preference shallower layersPostflexion stages reached deeper layers
100
150
Dep
th (m
)
Flexion and postflexion stages migration to 150
200
Hygophum hygomiiDecember Shelf
p g gsurface during the day in December
-60 -40 -20 0 20N/1000 m3
-10 0 10N/1000 m3
RESULTS: LARVAL SIZE STRATIFICATION. MYCTOPHIDS
0
50
m)
0
50
m)
Postflex and flex migration to the surface during the day, particularly in December
100
150
Dep
th (m
Lampanyctus pusillus Lampanyctus pusillus
100
150
Dep
th (m
y p y
200
Lampanyctus pusillusDecember Shelf
Lampanyctus pusillusJuly Shelf
200
0-40 -20 0 20 40
N/1000 m3
50
(m)
Preflexion stages shallower distributionPostflexion stages wider nocturnal range
Lampanyctus crocodilusJ l Sh lf
100
150
Dep
th Postflexion stages wider nocturnal range
P fl i July Shelf200
Preflexion
PostflexionFlexion
CONCLUSIONS
Variation in specific composition among periods, mainly due to the shelf species.p p g p , y p
No differences between zones (same species, similar abundance)
Larval depth vertical ranges differed among species with vertical habitatpartitioning:
Deep species (100-300): A. hemigymnus
Below thermocline species (from lower thermocline 200 m): B glacialeBelow thermocline species (from lower thermocline - 200 m): B. glaciale
Thermocline species: H. benoiti
Surface species: C. maderensis and many of the shelf speciesp y p
Transforming and juveniles appeared below 300 m.
Differences in diel vertical distributions between periods are relate to the
water column structure
In summer the majority of species were concentrated in the first 50 m
of the water column (thermocline), both day and night.
In autumn larvae were also concentrated in the surface layers during
the day (upper mixed layer) but showed a deeper distribution at nightthe day (upper mixed layer), but showed a deeper distribution at night(thermocline layer).
CONCLUSIONS
Larval size stratification was evident. Younger stages occupy the upper layers,g g py pp y ,
day and night. Postflexion reached much deeper layers and performed
vertical displacement to surface, during the day.
The thermocline acts as a retention structure during the non active night
hours. While light is the trigger factor for day migration to the surface.
Up to the moment remains an open question whether this displacement isUp to the moment remains an open question whether this displacement is
related to a suitable light intensity for feeding, or to a higher availability of food.
Thank you!