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Investigating California Current petrale sole spawning dynamics and oceanographic recruitment drivers Melissa A. Haltuch 1 , John Wallace 1 , Nick Tolimeri 1 , Lee Qi 2 , Michael G. Jacox 3 , and Carolina Parada 4 1 NOAA-Fisheries, NWFSC, Seattle,


  1. Investigating California Current petrale sole spawning dynamics and oceanographic recruitment drivers Melissa A. Haltuch 1 , John Wallace 1 , Nick Tolimeri 1 , Lee Qi 2 , Michael G. Jacox 3 , and Carolina Parada 4 1 NOAA-Fisheries, NWFSC, Seattle, WA, USA. 2 School of Aquatic and Fishery Sciences, University of December 13, 2017 Washington, USA 3 NOAA-Fisheries, SWFSC, Monterey, CA, USA 4 University of Concepcion, Department of Geophysics, Chile 10th International Flatfish Symposium

  2. Petrale Sole Widely distributed NE Pacific Seasonal migration Daniel W. Gotshall onshore – off shore Discrete winter spawning grounds High site fidelity Commercially valuable target fishery Photo: Wade D. Smith Photo: Wade D. Smith 2

  3. Petrale Sole Stock Status and Recruitment 1980s to 2000s Minimums in SB ≤ 10% of unexploited levels Few Above Average Recruitments Support fishery catch Followed by a lack of incoming recruits What does fishery data suggest about spawning dynamics? What is driving strong recruitments? What are potential impacts of spawning aggregation fishery on recruitment? 3

  4. US GLOBEC: The horizontal-advection bottom-up forcing paradigm Large-scale climate forcing drives regional changes in alongshore and cross- shelf ocean transport, directly impacting the transport of nutrients, water masses, and organisms. 4 Di Lorenzo, et al. 2013. Oceanography 26(4):22–33.

  5. US GLOBEC: The horizontal-advection bottom-up forcing paradigm Large-scale climate forcing drives regional changes in alongshore and cross- shelf ocean transport, directly impacting the transport of nutrients, water masses, and organisms. Goal Test the hypothesis that cross-shelf transport of pelagic petrale sole from deep water spawning grounds shoreward towards nursery areas on the continental shelf results in stronger recruitments than transport off-shore away from nursery areas. 5 Di Lorenzo, et al. 2013. Oceanography 26(4):22–33.

  6. Approach Spatio-temporal modeling of fishery trawl log-book data Spawning aggregation locations, biomass, and density Proportion of the stock occupying each spawning ground Conceptual life-history model Stage- and spatio-temporally specific Test hypotheses Physical variables that influence survival at each life stage Biophysical individual-based model driven by ROMS Which spawning grounds contribute to recruitment success? Do important spawning grounds change through time? 6

  7. Spatio-temporal modeling of fishery trawl log-book data Data 1981-2015 th Filters for data quality Top 20% biomass in at least 14 of the years Analysis Package VAST on GitHub (www.FishStats.org) Delta GLMM Linear predictors for 1) encounter probability 2) positive catch or catch rates Catch Weight ~Year + Lat + Lon + vessel Identify 520 unique fishing areas, Static over all years 7

  8. Winter Trawl Fishing (Spawning) Grounds Northern California Oregon Washington 8

  9. Spawning aggregation locations and biomass 127W 125W 123W • …. 48N 48N 5 46N 46N 4 3 44N 44N Latitude 1981 - 2015 Average 2 Biomass Average Biomass (mt) 42N 42N 1 0 40N 40N 127W 125W 123W Longitude 9 Year

  10. Spawning biomass over time 10

  11. Biomass During 2015 • …. 11

  12. Spawning aggregation densities 127W 125W 123W • …. 48N 48N Average Kg per Hectare 7 46N 46N 6 5 44N 44N 4 Latitude 3 1981 - 2015 2 Average 42N 42N kg/hectare 1 0 Year 40N 40N 127W 125W 123W Longitude 12

  13. Conceptual Life History Model: Oceanographic Recruitment Drivers Conceptual life-history Literature search ↓ Make hypotheses ↓ Fit a bunch of models (glms) ↓ ↓ Model selection with AICc ↓ Model testing 13

  14. Conceptual Life History Model: Oceanographic Recruitment Drivers Conceptual life-history Make stage specific & spatially specific hypotheses ↓ Make hypotheses • Do not use generalized climate indices like NOI or PDO ↓ Fit a bunch of models (glms) • Use ROMS output for oceanic ↓ drivers Residuals = Intercept + • NO Spawning stock biomass various predictors (SSB) ↓ Model selection with AICc ↓ Model testing 14

  15. Conceptual Life History Model: Lat: 39-48.5 o N Years: 1981-2015 Preconditioning to benthic juveniles Petrale Sole Life-history stage Time period Depth location 50-400m Preconditioning May - Oct (Yr 0) with highest occurrence Bottom between 50 - 200 m Spawning Nov (Yr 0)- Feb (Yr 1) 250-475 m Bottom MLD-475 m Nov (Yr 0)- Eggs temperatures 4-10 degrees C, Water Column Mid-Mar (Yr1) salinities 25-30 ppt Mid-Nov (Yr 0)- Early Development MLD-475 m Water Column Mar (Yr 1) Larvae (start Dec-April 0-50 m Water Column feeding) Pelagic juveniles April-August 0-150 m Water Column Benthic Juvenile May-September 10 - 100 m Bottom (Age-0) 15

  16. Conceptual Life History Model: Preconditioning to benthic juveniles Petrale Sole Life-history stage Time period Depth location 50-400m Preconditioning May - Oct (Yr 0) with highest occurrence Bottom between 50 - 200 m Spawning Nov (Yr 0)- Feb (Yr 1) 250-475 m Bottom MLD-475 m Nov (Yr 0)- Eggs temperatures 4-10 degrees C, Water Column Mid-Mar (Yr1) salinities 25-30 ppt Look at one stage Mid-Nov (Yr 0)- Early Development MLD-475 m Water Column Mar (Yr 1) Larvae (start Dec-April 0-50 m Water Column feeding) Pelagic juveniles April-August 0-150 m Water Colimn Benthic Juvenile May-September 10 - 100 m Bottom (Age-0) 16

  17. Conceptual Life History Model: Preconditioning to benthic juveniles Petrale Sole Life-history stage Time period Depth location Pelagic juveniles Apr-Aug 0 - 150 m Water Column Depth Hypothesis Covariates extent Longitudinal extent Data source Transport to settlement Net long-shore 0-150 m 80-120 km offshore ROMS habitat affects recruitment transport Transport to settlement Net cross-shelf 0-15 m 80-120 km offshore ROMS habitat affects recruitment transport Growth/Predation hypothesis: Growth rate is faster in Degree days 0-150 m 80-120 km offshore ROMS warm water leading to reduced time vulnerable to predators etc 17

  18. Conceptual Life History Model: Individual Based Model 18

  19. ROMS Coupled Individual Based Model ROMS Model Oceanographic Coupling processes Model output Settlement Connectivity zones matrices Transport pattern 19

  20. Logbook Modeling Summary: What does fishery data suggest about spawning dynamics? Identify 520 discrete spawning grounds Low stock size – low spawning biomass across all spawning grounds Increasing stock size - 13 spawning grounds show large increases in biomass relative to other areas (all off of OR coast) Biomass on spawning grounds - lowest in CA, followed by WA then OR Oregon has ~ 50% or more of the biomass during the time series. Since 2007 between 55% - 82% of the total spawning biomass is in OR. California - spawning aggregations are much less dense than those in OR and WA Spawning aggregation density - increased steadily with increasing stock size Peaks in spawning aggregation density track strong cohorts in WA. 20

  21. Current Work Test hypotheses Physical variables that influence survival at each life stage Biophysical individual-based model driven by ROMS Which spawning grounds contribute to recruitment success? Do important spawning grounds change through time? 21

  22. The End Thank You! 22

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