building early ontogeny pelagic exposure profiles for goa ... · larval feeding ecology larval...

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gulfofalaska.nprb.org Building Early Ontogeny Pelagic Exposure Profiles for GOA-IERP Species based on Historical Ichthyoplankton Data—Pacific Cod Miriam Doyle Joint Institute for the Study of the Atmosphere and Ocean, College of the Environment, University of Washington, Seattle, WA Alaska Fisheries Science Center, National Marine Fisheries Service, National Oceanic and Atmospheric Administration, Seattle, WA The recommendations and general contents presented in this poster do not necessarily represent the views or official position of the Department of Commerce, the National Oceanic and Atmospheric Administration or the National Marine Fisheries Service. Seasonal Patterns Interannual Patterns: Late-Spring Shelikof Time-Series Eastern vs. Western GOA Multispecies Perspective Synthesis Larvae occur in the plankton in March, peak in abundance during late April, and continue to be abundant through early June. Larvae >15 mm are not sampled efficiently by 60 cm Bongo nets.. Larvae are primarily associated with the upper 50 m of the water column to which they migrate rapidly on hatching. Length frequency distributions indicate that growth rates of larvae are higher between May and June than between April and May. Larvae are common during spring months throughout the WGOA shelf but are most abundant between the Shumagin Islands and Unimak Pass. The late-spring GOA time-series shows the occasional occurrence of anomalously high levels of abundance during the years 1989-1997 and 2007-09. Doyle et al. (2009) have identified a positive association between late spring larval abundance and cooler winters, and strength and direction of alongshore winds during spring. Interannual variation in length frequency distributions of larvae reflect a shift in timing of sampling from year to year but also indicate diminished and enhanced growth of larvae during cold and warm years, respectively. Pacific cod larvae belong to a shelf assemblage of larval fish species that prevails April-June in the WGOA (Doyle et al., 2002). Pacific cod, walleye pollock, and northern rock sole belong to an early life history strategy “Abundant” (high fecundity) group that is characterized by high production of eggs/larvae with peak abundance of larvae in April, relatively limited larval duration, and moderate to high spatial ubiquity of larvae (Doyle and Mier, 2012). Synchronicity is observed in the abundance of these species’ larvae across the time-series, with tightest synchrony between Pacific cod and northern rock sole. During the historical peak period of abundance of larvae in the WGOA, Pacific cod larvae seem to be rare in the EGOA. Temporal Exposure of Pacific cod larvae is characterized by a narrow spring peak in abundance - likely coincides with early production in GOA zooplankton. Spatial Exposure extends throughout WGOA shelf waters and the area from the Shumagin Islands to Unimak Pass seems to be a hot spot for larval production. Vertical Distribution of larvae indicates that circulation models representing the upper 50 m (primarily upper 30 m) of the water column during April-June will be suitable for describing potential transport pathways for larvae. The Early Life History strategy (ELH) common to Pacific cod, walleye pollock, and northern rock sole results in sufficient production of eggs and larvae to withstand high levels of early mortality but with limited larval duration that may risk potential mismatch with peaks in food resources, or exposure of the bulk of the larval population to other unfavorable conditions (e.g. sub-optimal temperatures and transport). Pelagic exposure-response coupling: Evidence in support of this is provided by the synchrony observed among the above three species in the time-series of larval abundance and similarities in links with environmental variables (Doyle et al., 2009; Doyle and Mier, 2012.). Occurrence and abundance of larvae seems diminished in the EGOA relative to the WGOA. Gaps in ELH knowledge: Spawning areas and ELH habitat in the EGOA Larval feeding ecology Larval predation Habitat and ecology of late stage and transitioning larvae Age-0 through juvenile stage ecology References Doyle, M.J., Mier, K.L., Brodeur, R.D., and Busby, M.S. (2002). Regional variations in springtime ichthyoplankton assemblages in the northeast Pacific Ocean. Prog. Oceanogr. 53(2-4): 247-282. Doyle, M.J., Picquelle, S.J., Mier, K.L., Spillane, M.C., and Bond, N.A. (2009). Larval fish abundance and physical forcing in the Gulf of Alaska, 1981-2003. Prog. Oceanogr. 80:163-187. Doyle, M.J. and Mier, K.L. (2012). A new conceptual framework for evaluating the early ontogeny phase of recruitment processes among marine fish species. Can. J. Fish. Aquat. Sci. 69: 2112-2129. Seasonal Progression in Distribution of Larvae Vertical Distribution Early Life History (ELH) Exposure-Response Framework Doyle and Mier 2012 Larval abundance x half month 140°W 150°W 160°W 170°W 60°N 55°N 50°N Depth m 200 1000 May 1-15 Mean No./10 m² 0 <10 <50 <100 <500 <1000 <10000 Extent of Grid 60°N 55°N Depth m 200 1000 Apr 1 - 15 150°W 160°W 60°N 55°N 150°W 160°W Apr 16 - 30 May 1 - 15 May 16 - 31 Mean No./10 m 2 0 <10 <50 <100 <500 <1000 <10000 150°W 160°W 60°N 55°N Depth m 200 1000 Jun 1-15 Mean No./10 m 2 0 <10 <50 <100 <500 <1000 <10000 J F M A M J J A S O N D Mean abundance (no./10 m 2 ) positive tows 0 25 50 75 100 125 Larvae Pacific cod Standard length (mm) 0 5 10 15 20 25 30 Length frequency (%) 0 10 20 30 40 50 60 70 Apr (1151) May (14042) Jun (752) Length mm 0 5 10 15 Mid net depth m 0 50 100 150 200 250 Log 10 no./1000 m 3 0 1 2 3 4 5 Mid net depth m 0 50 100 150 200 250 1985 1990 1995 2000 2005 2010 Mean abundance (no./10 m 2 ) 0 20 40 60 Larval abundance % Frequency of catch by larval length bins (mm): Pacific cod 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 WMA 1981 144 -4 135 9.71 3.40 1982 147 -1 158 7.65 22.56 9.68 1983 145.5 -2.5 78 8.13 24.15 6.08 1985 148 0 174 7.96 22.86 6.07 1987 142 -6 19 7.33 25.03 3.40 1988 150 2 87 8.36 24.43 1.46 1989 152.5 4.5 1590 7.86 19.51 50.27 1990 152 4 521 9.33 20.91 29.00 1991 141.5 -6.5 161 5.27 19.67 11.15 1992 143.5 -4.5 694 5.69 23.22 49.53 1993 148.5 0.5 64 7.68 23.04 4.18 1994 148 0 266 6.45 23.58 12.46 1995 145 -3 647 5.98 20.99 34.86 1996 149 1 324 9.37 23.21 11.46 1997 147 -1 313 6.30 23.31 20.20 1998 146 -2 33 9.75 28.53 2.76 1999 149 1 831 5.66 20.06 5.82 2000 151.5 3.5 570 8.06 23.25 11.59 2001 149 1 161 9.02 25.31 6.81 2002 148 0 424 6.67 23.07 14.33 2003 149.5 1.5 183 8.20 27.56 3.09 2004 149.5 1.5 99 9.20 22.70 2.65 2005 148 0 398 9.30 25.31 0.87 2006 147 -1 733 8.76 23.23 12.18 2007 144 -4 578 6.09 18.88 34.13 2008 147 -1 311 6.33 20.15 20.70 2009 152.5 4.5 404 6.00 18.69 14.98 2010 147 -1 107 7.08 24.28 2.99 2011 156.5 8.5 38 11.43 22.56 2.59 N = number of larvae measured WMA = weighted mean abundance (no./10 m 2 ) % Frequency: 0 >0<1 1<5 5<10 10<15 15<20 20<25 25<30 30<35 35<55 WML = weighted mean length mm, Time-series (May 16-Jun 9) Julian Day mid-point of sampling coverage: 148 J-M SST = Cumulative mean SST for Jan through May from monthly mean values NOAA Optimum Interpolation (OI) SST V2; at Long 155.5, Lat 57.5 (color coded: light blue coldest to dark green warmest) WML vs WMA: -0.43 WML vs Cum J-M SST: 0.49 WML vs. Mid-cruise Shift: 0.46 WMA vs Cum J-M SST: -0.53 WMA vs. Mid-Cruise shift: -0.07 Expected tendency for smaller larvae to be more abundant than larger larvae. Interannual variation in larval length positively related to shift in sampling dates and SST. Interannual variation in larval abundance negatively related to SST, and not related to shift in sampling dates. Interannual Variation in Larval Length Distributions L M W N r a e Y Mid-Cruise Julian Day Mid-Cruise Shift (JD) J-M SST Cumulative mean Correlations: 1985 1990 1995 2000 2005 2010 Normalized mean abundance (no./10 m 2 ) -2 -1 0 1 2 3 4 Pacific cod Walleye pollock Northern rock sole Abundant group (Correlations 0.55, 0.36, 0.73)

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Page 1: Building Early Ontogeny Pelagic Exposure Profiles for GOA ... · Larval feeding ecology Larval predation Habitat and ecology of late stage and transitioning larvae Age-0 through juvenile

gulfofalaska.nprb.org

Building Early Ontogeny Pelagic Exposure Profiles for GOA-IERP Species based on Historical Ichthyoplankton Data—Pacific Cod

Miriam Doyle Joint Institute for the Study of the Atmosphere and Ocean, College of the Environment, University of Washington, Seattle, WA Alaska Fisheries Science Center, National Marine Fisheries Service, National Oceanic and Atmospheric Administration, Seattle, WA

The recommendations and general contents presented in this poster do not necessarily represent the views or official position of the Department of Commerce, the National Oceanic and Atmospheric Administration or the National Marine Fisheries Service.

Seasonal Patterns

Interannual Patterns: Late-Spring Shelikof Time-Series

Eastern vs. Western GOA

Multispecies Perspective

Synthesis

• LarvaeoccurintheplanktoninMarch,peakinabundanceduringlateApril,andcontinuetobeabundantthroughearlyJune.Larvae>15mmarenotsampledefficientlyby60cmBongonets..

• Larvaeareprimarilyassociatedwiththeupper50mofthewatercolumntowhichtheymigraterapidlyonhatching.

• LengthfrequencydistributionsindicatethatgrowthratesoflarvaearehigherbetweenMayandJunethanbetweenAprilandMay.

• LarvaearecommonduringspringmonthsthroughouttheWGOAshelfbutaremostabundantbetweentheShumaginIslandsandUnimakPass.

• Thelate-springGOAtime-seriesshowstheoccasionaloccurrenceofanomalouslyhighlevelsofabundanceduringtheyears1989-1997and2007-09.

• Doyleetal.(2009)haveidentifiedapositiveassociationbetweenlatespringlarvalabundanceandcoolerwinters,andstrengthanddirectionofalongshorewindsduringspring.

• Interannualvariationinlengthfrequencydistributionsoflarvaereflectashiftintimingofsamplingfromyeartoyearbutalsoindicatediminishedandenhancedgrowthoflarvaeduringcoldandwarmyears,respectively.

• PacificcodlarvaebelongtoashelfassemblageoflarvalfishspeciesthatprevailsApril-JuneintheWGOA(Doyleetal.,2002).

• Pacificcod,walleyepollock,andnorthernrocksolebelongtoanearlylifehistorystrategy“Abundant”(highfecundity)groupthatischaracterizedbyhighproductionofeggs/larvaewithpeakabundanceoflarvaeinApril,relativelylimitedlarvalduration,andmoderatetohighspatialubiquityoflarvae(DoyleandMier,2012).

• Synchronicityisobservedintheabundanceofthesespecies’larvaeacrossthetime-series,withtightestsynchronybetweenPacificcodandnorthernrocksole.

• DuringthehistoricalpeakperiodofabundanceoflarvaeintheWGOA,PacificcodlarvaeseemtoberareintheEGOA.

• Temporal ExposureofPacificcodlarvaeischaracterizedbyanarrowspringpeakinabundance-likelycoincideswithearlyproductioninGOAzooplankton.

• Spatial ExposureextendsthroughoutWGOAshelfwatersandtheareafromtheShumaginIslandstoUnimakPassseemstobeahotspotforlarvalproduction.

• Vertical Distributionoflarvaeindicatesthatcirculationmodelsrepresentingtheupper50m(primarilyupper30m)ofthewatercolumnduringApril-Junewillbesuitablefordescribingpotentialtransportpathwaysforlarvae.

• TheEarly Life History strategy(ELH)commontoPacificcod,walleyepollock,andnorthernrocksoleresultsinsufficientproductionofeggsandlarvaetowithstandhighlevelsofearlymortalitybutwithlimitedlarvaldurationthatmayriskpotentialmismatchwithpeaksinfoodresources,orexposureofthebulkofthelarvalpopulationtootherunfavorableconditions(e.g.sub-optimaltemperaturesandtransport).

• Pelagic exposure-response coupling:Evidenceinsupportofthisisprovidedbythesynchronyobservedamongtheabovethreespeciesinthetime-seriesoflarvalabundanceandsimilaritiesinlinkswithenvironmentalvariables(Doyleetal.,2009;DoyleandMier,2012.).

• OccurrenceandabundanceoflarvaeseemsdiminishedintheEGOArelativetotheWGOA.

• Gaps in ELH knowledge:

◊ SpawningareasandELHhabitatintheEGOA

◊ Larvalfeedingecology

◊ Larvalpredation

◊ Habitatandecologyoflatestageandtransitioninglarvae

◊ Age-0throughjuvenilestageecology

References

Doyle,M.J.,Mier,K.L.,Brodeur,R.D.,andBusby,M.S.(2002).RegionalvariationsinspringtimeichthyoplanktonassemblagesinthenortheastPacificOcean.Prog.Oceanogr.53(2-4):247-282.

Doyle,M.J., Picquelle, S.J.,Mier,K.L., Spillane,M.C., andBond,N.A. (2009). LarvalfishabundanceandphysicalforcingintheGulfofAlaska,1981-2003.Prog.Oceanogr.80:163-187.

Doyle,M.J.andMier,K.L.(2012).Anewconceptualframeworkforevaluatingtheearlyontogenyphaseofrecruitmentprocessesamongmarinefishspecies.Can.J.Fish.Aquat.Sci.69:2112-2129.

Seasonal Progression in Distribution of Larvae

Vertical Distribution

Early Life History (ELH) Exposure-Response Framework

Doyle and Mier 2012

Larval abundance x half month

140°W150°W160°W170°W

60°N

55°N

50°NDepth m

2001000

May 1-15Mean No./10 m²0<10<50<100<500<1000<10000

Extent of G

rid

60°N

55°N

Depth m200

1000

Apr 1 - 15

150°W160°W

60°N

55°N

150°W160°W

Apr 16 - 30

May 1 - 15 May 16 - 31

Mean No./10 m2

0

<10

<50

<100

<500

<1000

<10000

150°W160°W

60°N

55°N

Depth m200

1000

Jun 1-15Mean No./10 m2

0

<10

<50

<100

<500

<1000

<10000

J F M A M J J A S O N D

Mea

n ab

unda

nce

(no.

/10

m2 ) p

ositi

ve to

ws

0

25

50

75

100

125 Larvae

Pacific cod

Standard length (mm)0 5 10 15 20 25 30

Leng

th fr

eque

ncy

(%)

0

10

20

30

40

50

60

70Apr (1151)May (14042)Jun (752)

Length mm0 5 10 15

Mid

net

dep

th m

0

50

100

150

200

250

Log10 no./1000 m3

0 1 2 3 4 5

Mid

net

dep

th m

0

50

100

150

200

250

1985 1990 1995 2000 2005 2010

Mea

n ab

unda

nce

(no.

/10

m2 )

0

20

40

60 Larval abundance % Frequency of catch by larval length bins (mm): Pacific cod3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 WMA

1981 144 -4 135 9.71 3.401982 147 -1 158 7.65 22.56 9.681983 145.5 -2.5 78 8.13 24.15 6.081985 148 0 174 7.96 22.86 6.071987 142 -6 19 7.33 25.03 3.401988 150 2 87 8.36 24.43 1.461989 152.5 4.5 1590 7.86 19.51 50.271990 152 4 521 9.33 20.91 29.001991 141.5 -6.5 161 5.27 19.67 11.151992 143.5 -4.5 694 5.69 23.22 49.531993 148.5 0.5 64 7.68 23.04 4.181994 148 0 266 6.45 23.58 12.461995 145 -3 647 5.98 20.99 34.861996 149 1 324 9.37 23.21 11.461997 147 -1 313 6.30 23.31 20.201998 146 -2 33 9.75 28.53 2.761999 149 1 831 5.66 20.06 5.822000 151.5 3.5 570 8.06 23.25 11.592001 149 1 161 9.02 25.31 6.812002 148 0 424 6.67 23.07 14.332003 149.5 1.5 183 8.20 27.56 3.092004 149.5 1.5 99 9.20 22.70 2.652005 148 0 398 9.30 25.31 0.872006 147 -1 733 8.76 23.23 12.182007 144 -4 578 6.09 18.88 34.132008 147 -1 311 6.33 20.15 20.702009 152.5 4.5 404 6.00 18.69 14.982010 147 -1 107 7.08 24.28 2.992011 156.5 8.5 38 11.43 22.56 2.59

N = number of larvae measuredWMA = weighted mean abundance (no./10 m2) % Frequency: 0 >0<1 1<5 5<10 10<15 15<20 20<25 25<30 30<35 35<55WML = weighted mean length mm, Time-series (May 16-Jun 9) Julian Day mid-point of sampling coverage: 148J-M SST = Cumulative mean SST for Jan through May from monthly mean values NOAA Optimum Interpolation (OI) SST V2; at Long 155.5, Lat 57.5(color coded: light blue coldest to dark green warmest)

WML vs WMA: -0.43 WML vs Cum J-M SST: 0.49 WML vs. Mid-cruise Shift: 0.46WMA vs Cum J-M SST: -0.53 WMA vs. Mid-Cruise shift: -0.07

Expected tendency for smaller larvae to be more abundant than larger larvae.Interannual variation in larval length positively related to shift in sampling dates and SST.Interannual variation in larval abundance negatively related to SST, and not related to shift in sampling dates.

Interannual Variation in Larval Length DistributionsLMWNraeY Mid-Cruise

Julian DayMid-Cruise Shift (JD)

J-M SST Cumulative

mean

Correlations:

1985 1990 1995 2000 2005 2010Nor

mal

ized

mea

n ab

unda

nce

(no.

/10

m2 )

-2

-1

0

1

2

3

4Pacific cod Walleye pollockNorthern rock sole

Abundant group(Correlations0.55, 0.36, 0.73)