Fish population dynamics P2
2. Today’s Focus: Rocky Reefs of California & Mexico
These temperate rocky reefs share key features with coral reefs:
High habitat complexity
High biomass and species diversity
Strong environmental forcing (especially upwelling)
Today’s lecture examines:
Larval production
Settlement
Post‑settlement processes (predation, competition)
How oceanography shapes recruitment
3. Reproductive Modes and Larval Duration
3.1 Pelagic vs Non‑Pelagic Larvae
Previous lecture assumed pelagic larvae transported by currents.
Many rocky‑reef fishes lay benthic eggs that hatch near the substrate.
These larvae:
Still have a larval phase
But are not fully pelagic
Are less influenced by currents
Show higher local retention
3.2 Larval Duration as a Driver of Dispersal
Larval duration = time larvae spend in the water column.
Longer duration → greater potential dispersal distance.
Otolith microstructure used to estimate larval age:
Daily growth rings (day/night feeding cycles)
Allows reconstruction of larval duration for each species.
3.3 Empirical Findings
Huge variation across species:
Garibaldi: ~20 days
Pacific rockfish: ~270 days
Implication:
Species differ dramatically in dispersal potential.
Oceanographic models treat larvae as particles to simulate dispersal distances.
3.4 General Patterns Across Taxa
Seaweeds: dispersal <5 km
Invertebrates: extremely variable
Fishes: typically 20–200 km, depending on larval duration
4. Two Functional Groups on Rocky Reefs
4.1 Mid‑Water Schooling Species
Live in kelp canopy/mid‑water
Larval duration: 3–4 months
Examples: olive rockfish, yellowtail rockfish, black rockfish
4.2 Benthic Solitary Species
Live near substrate, under kelp
Larval duration: 1–2 months
Examples: various benthic rockfish species
5. Upwelling Systems and Recruitment
Upwelling = deep, cold, nutrient‑rich water rising to the surface.
5.1 California Upwelling System
Strong but not as extreme as Peru/Chile
Drives:
Productivity
Larval transport
Recruitment success
5.2 Counterintuitive Larval Depth Patterns
Mid‑water adults → larvae found deep (90–100 m)
Benthic adults → larvae found shallow
Why?
Larval depth is an evolved strategy to exploit upwelling cycles.
6. ENSO (El Niño / La Niña) Effects on Recruitment
6.1 El Niño
Weak upwelling
Weak offshore winds
Weak offshore currents
Benthic species recruit better
Their shallow larvae are pushed onshore into correct habitat.
6.2 La Niña
Strong upwelling
Strong offshore currents
Mid‑water species recruit better
Deep larvae are brought upward and onshore by upwelling.
6.3 Neutral Years
Both groups recruit moderately well.
7. Within‑Year Variability
Upwelling is not constant even within a single ENSO phase.
7.1 Temperature as a Proxy
Upwelling pulses → sharp drops in temperature
Temperature record shows:
Highly stochastic fluctuations
No smooth seasonal pattern
7.2 Recruitment Tracking Temperature
Mid‑water species:
Recruit during cold pulses (upwelling events)
Benthic species:
Recruit during warm periods (weaker upwelling)
Even over 4 months, recruitment switches back and forth depending on oceanographic conditions.
8. Case Study: Sheephead Wrasse Recruitment
8.1 Geography
California + Baja California
Strong ENSO‑driven current reversals:
La Niña: north → south flow
El Niño: onshore → north flow
8.2 Findings
Northern sites show:
Low recruitment in normal/La Niña years
Huge recruitment spike during El Niño
Mechanism:
El Niño currents push larvae northward, enhancing recruitment at northern sites.
9. Habitat Effects on Settlement: Giant Kelp (Macrocystis) Forests
Macrocystis forests:
10–15 m tall
Extremely complex habitat
Support diverse fish assemblages
9.1 Classic Experimental Studies
Multiple studies manipulated kelp density to test:
Settlement preferences
Habitat dependence
Recruitment success
9.2 Key Findings Across Studies
Some species prefer dense kelp (mid‑water species)
Others prefer open rock (benthic species)
Kelp structure strongly influences settlement patterns
10. Detailed Example: Kelp Bass Recruitment
10.1 Experimental Manipulation
Increased kelp density → order‑of‑magnitude increase in kelp bass recruitment
No kelp → almost no recruitment
10.2 What Part of the Kelp Matters?
Two metrics tested:
Stipe density (kelp “trunks”)
Blade biomass (actual leaf area)
Findings:
Recruitment increases with stipe density up to ~50 stipes
But blade biomass explains recruitment far better
Relationship is asymptotic:
More kelp ≠ infinite recruitment
Plateau due to predation and habitat saturation
10.3 Spatial vs Temporal Variation
Spatial: denser forests ≠ always more fish
Temporal: year‑to‑year kelp density changes → recruitment changes
Blade biomass is the key driver, not stipe count
11. Post‑Settlement Processes
Once larvae settle, several processes shape survival:
11.1 Predation
Evidence
Higher recruit density → higher per capita mortality
Why?
More prey → more predators attracted
Predation scales non‑linearly with prey density
Experimental Predator Removal
With predators present:
Mortality increases with recruit density
With predators removed:
Mortality becomes flat (density‑independent)
Habitat Complexity
Complex rocky substrate → lower mortality
Flat substrate → high mortality
Mechanism: more hiding spaces reduce predation risk
11.2 Interspecific Competition
Case study: Striped vs Black Surfperch
Diet Preferences
Striped surfperch:
Dominant competitor
Prefers Gelidium robustum (high‑quality algae)
Black surfperch:
Subordinate competitor
Forced to eat turf algae when striped surfperch present
Experimental Removal
Remove striped surfperch:
Black surfperch expands diet to include Gelidium
Remove black surfperch:
Striped surfperch unaffected (dominant)
Depth Distribution
Striped surfperch dominate shallow areas (more algae)
Black surfperch pushed to deeper areas
Competition drives zonal habitat partitioning
Community‑Level Effects
Similar patterns seen across multiple rockfish species
Competition structures:
Vertical zonation
Habitat partitioning
Species coexistence
12. Synthesis and Conclusions
Temperate rocky reefs show that:
Recruitment is shaped by:
Larval behaviour (depth, duration)
Oceanography (upwelling, ENSO)
Habitat structure (kelp density, substrate complexity)
Post‑settlement survival is shaped by:
Predation
Competition
Habitat availability
Population dynamics emerge from the interaction of all these processes.
No single factor explains adult abundance
Multiple processes act simultaneously
Understanding these interactions is essential for:
Fisheries management
Marine protected area design
Predicting climate‑driven changes