1
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 Eastern vs. Western GOA Multispecies Perspective Synthesis Rockfish larvae occur in plankton samples from April through November with a peak in abundance during June and July. Larvae >15 mm are not sampled efficiently by 60 cm Bongo nets. Larvae are common in the upper 100 m of the water column but are most abundant above 50 m. A few recently hatched larvae have been sampled below 100 m. Length frequency distributions indicate the existence of a separate and smaller sized cohort of larvae (different species) in the summer relative to spring. Larvae are common during spring and summer months throughout the WGOA but are most abundant over the continental slope and particularly in association with Amatuli Trough and outer Shelikof Sea Valley which seem to be significant regions of cross shelf transport of larvae. The appearance of larvae in Shelikof Strait seems to result from ingress of larvae in these locations. The late-spring GOA time-series for rockfish larvae is characterized by low levels of abundance through 1996, and subsequent dramatic fluctuations with increasing abundance overall and highest positive anomalies in 1998, 2001 and 2011. Doyle et al. (2009) have identified a positive association between late spring larval abundance and warm spring temperatures. Interannual variation in larval length frequency distributions indicate stability in timing of release of larvae into the plankton over the time-series. The weak negative relationship between larval length and temperature suggests that larvae tend to be slightly larger overall during colder years, which seems counter- intuitive. Rockfish larvae belong to a slope assemblage of larval fish species that prevails during spring and summer in the WGOA (Doyle et al., 2002). Rockfish belong to an early life history strategy “Synchronous” (late spawning) group that is characterized by production of larvae that is synchronized well with peak spring production in the zooplankton (Doyle and Mier, 2012). Other members of this group include starry flounder and southern rock sole. Although interannual variation in larval abundance for these species is not as tightly synchronized as for the “Abundant” group, they share a pattern of increasing abundance overall across the time-series with occasional high anomalies in later years including a shared dramatic high in 2001. During spring, rockfish larvae are abundant over the slope and in deep water in both the WGOA and the EGOA. Temporal Exposure of rockfish larvae is characterized by late spring to summer peaks in abundance that is synchronized well with the annual peak in zooplankton production in the GOA. Bothe the spring and summer cohorts of larvae are likely to encounter plentiful zooplankton prey. Spatial Exposure extends throughout WGOA and EGOA waters primarily along the continental slope and in deep water, with highest densities of larvae associated with troughs that likely facilitate on-shelf transport of larvae. Vertical Distribution of larvae indicates that circulation models representing the upper 100 m of the water column (shelf) are suitable for tracking larval drift, and that highest densities of larvae occur in the upper 50 m. The Early Life History strategy (ELH) common to rockfish, starry flounder and southern rock sole results in an early ontogeny pelagic phase that is well synchronized with abundant larval food resources in the plankton. Pelagic exposure-response coupling: The shared pattern of spring-summer pelagic “exposure” of these species may be reflected in the common trend of increasing larval abundance over the time-series (Doyle and Mier, 2012). A positive association between larval abundance and spring water temperatures is also shared by rockfish and southern rock sole (Doyle et al., 2009). Occurrence and abundance of larvae is comparable between the EGOA and WGOA. Gaps in ELH knowledge: Distinction among multiple rockfish species in the larval stage 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 % Frequency of catch by larval length bins (mm): Rockfish 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 68 5.32 5.61 1982 147 -1 53 4.82 22.56 6.69 1983 145.5 -2.5 83 5.59 24.15 8.63 1985 148 0 541 5.36 22.86 53.81 1987 142 -6 0 25.03 0.00 1988 150 2 103 5.25 24.43 1.90 1989 152.5 4.5 108 5.70 19.51 4.19 1990 152 4 83 6.62 20.91 6.34 1991 141.5 -6.5 107 6.01 19.67 12.01 1992 143.5 -4.5 191 5.91 23.22 11.65 1993 148.5 0.5 356 6.06 23.04 16.51 1994 148 0 182 6.14 23.58 12.48 1995 145 -3 191 6.40 20.99 19.83 1996 149 1 117 6.25 23.21 5.19 1997 147 -1 410 5.87 23.31 41.29 1998 146 -2 1484 5.87 28.53 206.79 1999 149 1 612 7.25 20.06 3.62 2000 151.5 3.5 207 5.47 23.25 15.20 2001 149 1 1000 5.72 25.31 149.24 2002 148 0 192 6.18 23.07 8.97 2003 149.5 1.5 743 5.46 27.56 55.27 2004 149.5 1.5 546 5.76 22.70 12.87 2005 148 0 1097 6.68 25.31 32.12 2006 147 -1 564 6.70 23.23 4.71 2007 144 -4 141 6.34 18.88 30.25 2008 147 -1 476 6.04 20.15 43.66 2009 152.5 4.5 569 6.42 18.69 49.31 2010 147 -1 1418 6.02 24.28 74.41 2011 156.5 8.5 518 6.37 22.56 178.71 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<75 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: -0.01 WML vs Cum J-M SST: -0.35 WML vs. Mid-cruise Shift: -0.02 WMA vs Cum J-M SST: 0.41 WMA vs. Mid-Cruise shift: 0.25 Expected tendency for smaller larvae to be more abundant than larger larvae not apparent. Interannual variation in larval length negatively related to SST but not shift in sampling dates. Interannual variation in larval abundance positively related to SST, and weakly to shift in sampling dates. Interannual Variation in Larval Length Distributions Year N WML Mid- Cruise Julian Day Mid- Cruise Shift (JD) J-M SST Cumulative mean Correlations: J F M A M J J A S O N D Mean abundance (no./10 m 2 ) positive tows 0 50 100 150 200 250 Larvae Sebastes spp. Standard length (mm) 0 5 10 15 Length frequency (%) 0 10 20 30 40 50 60 70 Apr (329) May (12051) Jun (3698) Jul (810) Aug (70) Sep (300) 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 Normalized mean abundance (no./10 m 2 ) -2 -1 0 1 2 3 4 Rockfish Starry flounder Southern rock sole Synchronous group (Correlations 0.11, 0.33, 0.40) 1GI86 Mar 30 - Apr 20 2006 Rockfish larvae Depth m 200 1000 No./10 m² 0 <10 <50 <100 <500 <1000 <10000 1TT05 April 28 - May 7 2005 Rockfish Depth m 200 1000 No./10 m² 0 <10 <50 <100 <500 <1000 <10000 Interannual Patterns: Late-Spring Shelikof Time-Series 1985 1990 1995 2000 2005 2010 Mean abundance (no./10 m 2 ) 0 50 100 150 200 250 Larval abundance gulfofalaska.nprb.org Building Early Ontogeny Pelagic Exposure Profiles for GOA-IERP Species based on Historical Ichthyoplankton Data—Rockfish 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

Building Early Ontogeny Pelagic Exposure Profiles for GOA ......c e (n o. / 1 0 m 2) 0 50 100 150 200 250 Larval abundance gulfofalaska.nprb.org Building Early Ontogeny Pelagic Exposure

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Page 1: Building Early Ontogeny Pelagic Exposure Profiles for GOA ......c e (n o. / 1 0 m 2) 0 50 100 150 200 250 Larval abundance gulfofalaska.nprb.org Building Early Ontogeny Pelagic Exposure

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

Eastern vs. Western GOA

Multispecies Perspective

Synthesis

• RockfishlarvaeoccurinplanktonsamplesfromAprilthroughNovemberwithapeakinabundanceduringJuneandJuly.Larvae>15mmarenotsampledefficientlyby60cmBongonets.

• Larvaearecommonintheupper100mofthewatercolumnbutaremostabundantabove50m.Afewrecentlyhatchedlarvaehavebeensampledbelow100m.

• Lengthfrequencydistributionsindicatetheexistenceofaseparateandsmallersizedcohortoflarvae(differentspecies)inthesummerrelativetospring.

• LarvaearecommonduringspringandsummermonthsthroughouttheWGOAbutaremostabundantoverthecontinentalslopeandparticularlyinassociationwithAmatuliTroughandouterShelikofSeaValleywhichseemtobesignificantregionsofcrossshelftransportoflarvae.TheappearanceoflarvaeinShelikofStraitseemstoresultfromingressoflarvaeintheselocations.

• Thelate-springGOAtime-seriesforrockfishlarvaeischaracterizedbylowlevelsofabundancethrough1996,andsubsequentdramaticfluctuationswithincreasingabundanceoverallandhighestpositiveanomaliesin1998,2001and2011.

• Doyleetal.(2009)haveidentifiedapositiveassociationbetweenlatespringlarvalabundanceandwarmspringtemperatures.

• Interannualvariationinlarvallengthfrequencydistributionsindicatestabilityintimingofreleaseoflarvaeintotheplanktonoverthetime-series.Theweaknegativerelationshipbetweenlarvallengthandtemperaturesuggeststhatlarvaetendtobeslightlylargeroverallduringcolderyears,whichseemscounter-intuitive.

• RockfishlarvaebelongtoaslopeassemblageoflarvalfishspeciesthatprevailsduringspringandsummerintheWGOA(Doyleetal.,2002).

• Rockfishbelongtoanearlylifehistorystrategy“Synchronous”(latespawning)groupthatischaracterizedbyproductionoflarvaethatissynchronizedwellwithpeakspringproductioninthezooplankton(DoyleandMier,2012).Othermembersofthisgroupincludestarryflounderandsouthernrocksole.

• Althoughinterannualvariationinlarvalabundanceforthesespeciesisnotastightlysynchronizedasforthe“Abundant”group,theyshareapatternofincreasingabundanceoverallacrossthetime-serieswithoccasionalhighanomaliesinlateryearsincludingashareddramatichighin2001.

• Duringspring,rockfishlarvaeareabundantovertheslopeandindeepwaterinboththeWGOAandtheEGOA.

• Temporal ExposureofrockfishlarvaeischaracterizedbylatespringtosummerpeaksinabundancethatissynchronizedwellwiththeannualpeakinzooplanktonproductionintheGOA.Bothethespringandsummercohortsoflarvaearelikelytoencounterplentifulzooplanktonprey.

• Spatial ExposureextendsthroughoutWGOAandEGOAwatersprimarilyalongthecontinentalslopeandindeepwater,withhighestdensitiesoflarvaeassociatedwithtroughsthatlikelyfacilitateon-shelftransportoflarvae.

• Vertical Distributionoflarvaeindicatesthatcirculationmodelsrepresentingtheupper100mofthewatercolumn(shelf)aresuitablefortrackinglarvaldrift,andthathighestdensitiesoflarvaeoccurintheupper50m.

• TheEarly Life History strategy(ELH)commontorockfish,starryflounderandsouthernrocksoleresultsinanearlyontogenypelagicphasethatiswellsynchronizedwithabundantlarvalfoodresourcesintheplankton.

• Pelagic exposure-response coupling:Thesharedpatternofspring-summerpelagic“exposure”ofthesespeciesmaybereflectedinthecommontrendofincreasinglarvalabundanceoverthetime-series(DoyleandMier,2012).Apositiveassociationbetweenlarvalabundanceandspringwatertemperaturesisalsosharedbyrockfishandsouthernrocksole(Doyleetal.,2009).

• OccurrenceandabundanceoflarvaeiscomparablebetweentheEGOAandWGOA.

• Gaps in ELH knowledge:

• Distinctionamongmultiplerockfishspeciesinthelarvalstage

◊ SpawningareasandELHhabitatintheEGOA

◊ Larvalfeedingecology

◊ Larvalpredation

◊ Habitatandecologyoflatestageandtransitioninglarvae

◊ Age-0throughjuvenilestageecology

ReferencesDoyle, 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

% Frequency of catch by larval length bins (mm): Rockfish3 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 68 5.32 5.611982 147 -1 53 4.82 22.56 6.691983 145.5 -2.5 83 5.59 24.15 8.631985 148 0 541 5.36 22.86 53.811987 142 -6 0 25.03 0.001988 150 2 103 5.25 24.43 1.901989 152.5 4.5 108 5.70 19.51 4.191990 152 4 83 6.62 20.91 6.341991 141.5 -6.5 107 6.01 19.67 12.011992 143.5 -4.5 191 5.91 23.22 11.651993 148.5 0.5 356 6.06 23.04 16.511994 148 0 182 6.14 23.58 12.481995 145 -3 191 6.40 20.99 19.831996 149 1 117 6.25 23.21 5.191997 147 -1 410 5.87 23.31 41.291998 146 -2 1484 5.87 28.53 206.791999 149 1 612 7.25 20.06 3.622000 151.5 3.5 207 5.47 23.25 15.202001 149 1 1000 5.72 25.31 149.242002 148 0 192 6.18 23.07 8.972003 149.5 1.5 743 5.46 27.56 55.272004 149.5 1.5 546 5.76 22.70 12.872005 148 0 1097 6.68 25.31 32.122006 147 -1 564 6.70 23.23 4.712007 144 -4 141 6.34 18.88 30.252008 147 -1 476 6.04 20.15 43.662009 152.5 4.5 569 6.42 18.69 49.312010 147 -1 1418 6.02 24.28 74.412011 156.5 8.5 518 6.37 22.56 178.71

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<75WML = 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: -0.01 WML vs Cum J-M SST: -0.35 WML vs. Mid-cruise Shift: -0.02WMA vs Cum J-M SST: 0.41 WMA vs. Mid-Cruise shift: 0.25

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

Interannual Variation in Larval Length DistributionsYear N WML

Mid-Cruise

Julian Day

Mid-Cruise

Shift (JD)

J-M SST Cumulative

mean

Correlations:

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

50

100

150

200

250Larvae

Sebastes spp.

Standard length (mm)0 5 10 15

Leng

th fr

eque

ncy

(%)

0

10

20

30

40

50

60

70Apr (329)May (12051)Jun (3698)Jul (810)Aug (70)Sep (300)

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 2010Nor

mal

ized

mea

n ab

unda

nce

(no.

/10

m2 )

-2

-1

0

1

2

3

4 Rockfish Starry flounderSouthern rock sole

Synchronous group (Correlations 0.11, 0.33, 0.40)

1GI86Mar 30 - Apr 20 2006

Rockfish larvae

Depth m

200

1000

No./10 m²

0

<10

<50

<100

<500

<1000

<10000

1TT05April 28 - May 7 2005

Rockfish

Depth m

200

1000

No./10 m²

0

<10

<50

<100

<500

<1000

<10000

Interannual Patterns: Late-Spring Shelikof Time-Series

1985 1990 1995 2000 2005 2010

Mea

n ab

unda

nce

(no.

/10

m2 )

0

50

100

150

200

250 Larval abundance

gulfofalaska.nprb.org

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

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