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Summary Marine Systems

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Summary of all exam material = modules/lectures, scientific articles & tutorials

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Exam: online modules + scientific articles + tutorials



Oceans cover 71%

Terrigenous => sediment eroded from land

Dominant elements dissolved in water = Na & Cl

Average salinity sea water = 35%o

(bi)carbonates  buffer the ocean



Poles

 High density, cold air sinks  high pressure zone forms



Rotation of Earth on its axis  Coriolis deflection



Diurnal tides = 1 high tide & 1 low tide each day

Spring tides occur at new & full moon

Intertidal zone => part of sea bottom that is regularly exposed to the atmosphere



Plankton => all floating & drifting organisms in the sea

Diatoms (algae) => most abundant plants in ocean



Salt wedge estuary

 Low tidal input
 High river input
 Low mixing of water



Primary production facilitated by sunlight & nutrients

~10% of energy transferred to next trophic level

Competitive exclusion => 1 species outcompetes other species & drives them extinct

Filter feeders live in place with high bottom energy + high bottom substrate

Upwelling areas & river outlets unsuitable for corals



Institution => social organization that is emerging, developing, functioning, and becoming structural

,  Main purpose: create order in (inter)actions of people
 E.g. UNCLOS (UN Convention Law Of the Seas)

Policy => range of decisions, that guide actions & assist in future decision-making

 E.g. Wadden Sea UNESCO World Heritage (policy arrangement)

Agency => capacity of individuals to construct the world around them, through day-to-day choices

 E.g. Marine Stewardship Council (actor)



Tragedy of the commons => users of a commons are caught in an inevitable process that leads to
destruction of the resources on which they depend



Key concepts
Module 1: ecological dynamics & resilience
 Social-ecological systems (SESs)
- Understand & manage change
 Key variables & interactions in SES  assess resilience
1. Interaction web: + & - interactions
2. Identify important feedback loops



Changes in marine systems
Shifting baselines => rapid change not noticed

 Fish are getting smaller over time



Causes

 Human activity
Coastal development
- Fishing
- Oil spillage
- Nutrient runoff from land
- Climate change



Effects

 Single stressor response
1. Proportional responses (linear)
2. Sudden responses (non-linear)  problematic for management (unpredictable)  shift to
alternative regime
 But: multiple drivers/causes of change (not 1 stressor)

,Ecological dynamics

 Important to understand dynamics of marine systems, not only ecosystem
 Anthropocene => time of (human driven) change
- Response to change?
- Systemic approach  also consider e.g. geology & sociology
 Complex dynamics  complex systems perspective



Role of interactions in marine systems
(socio)ecological interactions  key to understand emergent dynamics

 Interaction = effect of 1 population on the other



Direct interactions

o Biotic
o Intraspecies => within species
o Interspecies => between species
o Biotic-abiotic
o Humans – biota
o Humans – abiota



 Trophic (+/-)
- Predation & herbivory
 Interference competition (-/0)(-/-)
- Aggression & establishment
 Direct facilitation (+/+)(+/0)
- Substrate &barnacles on whales



Indirect interactions

 Trophic cascade

- Bottom up control => prey determines top predator population

- Top down control => top predator determines prey population




Negative and positive feedbacks: response to changes in marine environment
Feedback mechanisms => species has effect on itself through other species (circle)

,  Results in non-linear responses to change, important!



Negative feedback => species has indirect – effect on itself

 Dampen change



Positive feedback => species has indirect + effect on itself

 Accelerate change  potential to destabilize systems
- Facilitate regime shifts
- May lead to alternative regimes/traps
 Recognition can help understand emergent dynamics & potentially break them



Non-linear effects of change

 Trophic cascades
 Alternative stable states



Alternative stable states & critical transitions
Regime shift => relatively rapid change from 1 regime to a contrasting one

 Some shifts are difficult or impossible to reverse
 Examples
- Coral bleaching
- Shift from coral to macroalgae
 Causes
- Severe disturbance or permanent change (e.g. hurricanes, higher sea surface T=SST)
- Gradually changing conditions (internal dynamics, tipping point)
- Or a combination
- Tipping point = critical transition



Pulse disturbances

 Temporary
 Coral reefs:
- Hurricane
- Sea urchin disease

Press disturbances (drivers of change)

 Gradually changing environment, permanent
 Coral reefs:
- Increased fishing
- Increased nutrient runoff
- Increasing SST

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