Marine Zoology & Ecosystems: Hard Sediment

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54 Terms

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Environmental factors

Substrate type

Sediment transport

Productivity regime

Hydrodynamics

Depth

Disturbance

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Substrate characteristics

Rock type, texture, complexity, stability & orientation

determine what organisms can attach/live there

Affect habitat suitability for marine organisms

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Hydrodynamic forces & light

Wave exposure, currents, tidal regimes & light availability

Influences species zonation & nutrient flow

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Abiotic factors:

Temp & salinity fluctuations

Affect species distribution & physiological tolerance in marine habitats

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Biotic factors:

Competition & predation

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Anthropogenic Impacts

Over harvesting, pollution/eutrophication

Alter community structure & biodiversity in marine ecosystems

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Submarine canyons:

Investigate Northwest Atlantic vulnerable marine ecosystems (VME)

To understand eco-hydrodynamic & sediment drivers of macrofaunal diversity

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Sediment regime

dynamics: turbidity currents & tidal flushing

turbidity- nepheloid layer

accumulation of organic matter in deposition zone within canyons

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community composition

246 taxa, 15 phyla

bimodal density distribution in canyons vs slopes

biomass decreases with depth in canyons, increases with depth on slopes

overall deep-sea pattern: abundance decreases with depth

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Hydrodynamics:

studies movement of water through waves, currents, tides, internal waves & turbulence

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Hydrodynamics: hard sediment

water movement- dominant environmental driver

influences nutrient delivery, O2 availability, larval supply & settlement, sediment transport, species distribution (zonation)

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Zonation

patterns of species distribution across depth or hydrodynamic gradients

species distribution

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How traits affect ecology: surface texture

rough, complex surfaces trap larvae & biofilms

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How traits affect ecology: chemistry

reactive minerals attract or deter settlers

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How traits affect ecology: stability

affects succession- unstable/eroding surfaces favour opportunists

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How traits affect ecology: Orientation

orientation changes desiccation & flow exposure

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Predicting ecological outcomes: Early colonisers: Natural rock

Bacterial biofilm → microalgae (diatoms) → sessile inverts

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Predicting ecological outcomes: Early colonisers: biogenic

Bacterial biofilm & crustose coralline algae/encrusting sponges

larvae of corals, oysters, calcifiers

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Predicting ecological outcomes: Early colonisers: artificial

bacterial biofilm → opportunistic fast colonisers

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Predicting ecological outcomes: long-term community: Natural rock

Macroalgae (kelp), grazing inverts (limpets), dense mussel beds

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Predicting ecological outcomes: long-term community: biogenic

complex 3D reef with epibionts, cryptic species, borers (spongers), symbionts

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Predicting ecological outcomes: long-term community: artificial

lower evenness & structural complexity unless intentionally textured

dominated by non-calcifying fouling species

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Predicting ecological outcomes: feedback process: natural rock

Rugosity/crevices retain moisture & reduce morality for later settlers

Canopy macroalgae alter light & flow- creating understorey microhabitats

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Predicting ecological outcomes: feedback process: biogenic

Calcification builds structure → promotes more settlement

simultaneously bioerosion & dissolution reduce structure (-ve feedback)

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Predicting ecological outcomes: feedback process: artificial

chemistry can alter biofilm

absence of natural microcrevices limits niche diversity

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Natural rock

promotes slow, stable succession

granite/basalt

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Biogenic

enables chemically mediated, fast colonisation but fragile

coral skeletons

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Artificial

simplify communities unless modified

concrete

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Foundation species

organisms that create, define & maintain habitat through physical structure

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Kelp forest: structural trait

holdfast: tall, flexible fronds, dense canopy

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Kelp forest: abiotic effect

reduces light & flow

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Kelp forest: Biotic outcome

creates shaded refuged for invers/fish; suppresses understorey algae

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Coral reef: Structural trait

rigid CaCo3 skeleton

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Coral reef: Abiotic effect

alters hydrodynamics: buffers wave energy

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Coral reef: biotic outcome

3D complexity supports fish/inverts; high biodiversity

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Mussel bed: Structural trait

Dense, byssally bound shell matrix

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Mussel bed: abiotic effect

traps sediment, retains moisture

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Mussel bed: biotic outcome

provides habitat for infauna; reduces desiccation; increases small-scale diversity

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Sponge garden: structural trait

vertical, porous bodies

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Sponge garden: abiotic effect

filter water, modifies nutrients

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Sponge garden: biotic outcome

increases microbial productivity; creates substrate for epibionts

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Layers of life: Surface dwellers role

Primary production (algae)

Suspension feeding/space competition (barnacles)

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Layers of life: Interstitial species role

Detritovores

Transferring energy as prey for larger predation

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Layers of life: infauna role

Bioturbation

Nutrient remineralisation

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Layers of life: borers

Bioerosion

Carbonate cycling

Creating microhabitats

Contributing to structural weakening

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How does vertical habitat partitioning increase biodiversity in hard substrates:

Different layers support distinct species

Each layer offer unique microhabitats & resources

Functional roles vary by layer

Reduces competition by spatial separation

Enhances overall ecosystem complexity & resilience

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Kelp canopy->function->service:

primary function → carbon storage & habitat

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Coral reef->function->service:

3D habitat & carbonate accretion → shoreline protection

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Mussel bed->function->service:

Filtration → water clarity & nutrient cycling

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sponge garden->function->service:

nutrient cycling → water quality & microbial food web

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artificial->function->service:

refuge → biodiversity enhancement

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What happens when foundation species lost/replaced

removal shifts structure-function networks → loss of microhabitat complexity & ecosystem services

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Can ecosystem functions recover without original structure:

partial recovery possible via opportunists

lacks 3D habitat or long term stability

Study→ removing dead coral= 5x great coral densities after marine heatwave

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How can humans intervene to enhance resilience/restoration

active restoration: coral gardening

eco-engineering: biodegradable reef blocks to mimic natural heterogeneity

assisted adaptation: selecting heat tolerant coral

management leverage: marine protected areas