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Reef
A term reserved to describe just the mineral structure.
Reef Community
The organisms that live on a reef.
Coral
They are an animal, “plant,” and mineral.
Animal: small anthozoans (polyps)
Plant: Contain photosynthetic zooxanthellae (algae)
Mineral: Polyp takes up Ca and C atoms and secrete a hard mineral skeleton.
Defining Reef Traits
Topographic Relief
Rigidity
Form in-place
Framework of Skeletons
High Biodiversity
Reef Definition: Reef Tract (Ecosystem)
The suite of interconnected ecological zones around and including the structural reef and the associated high diversity biological community.
Includes the shore, back-reef lagoon, reef crest, and fore-reef.
Reef Definition: Structural Reef
The complex rigid structure built from the skeletons of organisms that forms in-place and rises above the sea floor.
Reef Definition: Classic Reef
The bright, vibrant, lively underwater ecosystem made of coral which is often used for snorkeling and diving.
Types of Reefs: Atolls
Donut-shaped
Often without a high island in the water
Out in the deep ocean
Types of Reefs: Fringing Reefs
Reefs located a short distance offshore and going around it.
Types of Reefs: Barrier Reefs
Reefs that follow the coastline of the shore, separated by a moderate distance by a deep lagoon
Types of Reefs: Bank Reefs
Categorizes all of the other reefs that don’t easily fall into other categories.
May or may not be associated with a coastline, islands, or a lagoon/barrier.
Types of Reefs: Patch Reefs
Small reefs
Many different scales
Some are just a few meters across while others are 1km across
Usually located within the lagoon of a bigger reef system
Reef Characteristics: Physical Environment
Includes:
Warm water (greater than 18C)
Supersaturated Water (CaCO3)
Low Turbidity
Nutrient Desert
Hardbottoms
Physical Characteristics: Warm Water
Reefs require a minimum average temperature of 18C
The average reef is greater than 20C
Water has different properties at different temperatures—it holds more CaCO3 and less CO2 at higher temps.
Physical Characteristics: Supersaturated in CaCO3
Corals, clams, and other organisms use CaCO3 to make skeletons.
Tropics are 3 to 4 times supersaturated in CaCO3.
Adding CO2 makes the water more acidic, lowering the CaCO3 saturation, making it harder to form skeletons.
Burning fossil fuels adds CO2 to oceans, decreasing saturation, and increasing ocean acidification.
Physical Characteristics: Low Turbidity
Low turbidity results from low photosynthetic plankton productivity.
Nutrients accumulate in the lower cold areas of the thermocline.
In tropics, there is no change in the thermocline, so nutrients and the plankton that eat them stay low under the water.
Physical Characteristics: Nutrient Desert
Too many nutrients allow algae to smother all the coral.
Low nutrients allow for a bustling area of biodiversity because of the large amount of competition (no algae or plankton smothering the whole area).
Physical Characteristics: Hardbottoms
Lots of CaCO3 precipitation leading to a very different sedimentation.
Much more 3D, vertical topography for organisms to inhabit.
Softbottoms don’t allow organisms to anchor, hardbottoms do.
Organisms rapidly build up structures forming inorganic cements.
Bioeroders erode cavities into structures.
Topography is built by organisms rather than gravity.
Results in a complex 3D structure that varies from place to place based on the present organisms.
Reef Characteristics: Biological
Mineralized Skeletons
Modular Organsims
Functional Plants
High Diversity
Area Zonation
Biological Characteristics: Mineralized Skeletons
Organisms create carbonate skeletons.
Making carbonate skeletons is very efficient for energy use in many organisms.
Biological Characteristics: Modular Organisms
Modular organisms have parts/modules that can replace each other.
Partial mortality, one part dying doesn’t mean the entire organism ceases to exist.
Quick replacement and building of each part from the rest of the organism.
Each module is a cloned individual (true corals, soft corals, anemones, sponges, algae).
Biological Characteristics: Functional Plants
Corals are endosymbionts, they contain zooxanthellae (single-celled algaae).
Algae is located within the cells of the coral, containing pigments that give corals their color.
Corals get most of their energy from their endosymbiont zooxanthellae (95 to 98 percent of their calories).
Biological Characteristics: High Diversity
“High” diversity is relative. High diversity compared to similar/proximate areas.
Large differences compared to non-reef areas.
Reefs support many different and unique ecological niches.
Biological Characteristics: Area Zonation.
Corals form differently based on depth and light exposure.
Low light leads to slow growth plates, high light leads to rapid branching.
Though small and fragile, branching corals grow the fastest, allowing them to recover quickly from storms and heavy waves destroying them at the surface.
Coldwater Reefs
Not a true reef zone, no access to light. Dead reefs.
Topographic relief
Rigidity to waves
Forms in-place
Made of biological skeletons
High diversity (versus surrounding area)
Worm Reefs
Not true reefs, don’t fit all characteristics.
Not modular, gregarious settlement.
Annelids secrete a calcareous tube creating rigidity and a 3D structure.
Reef framework is the biological skeletons, built on place on old skeletons.
High diversity
Reef Sections: Fore Reef
Aphotic (not a true reef zone)
Disphotic/Rariphotic
Deep Fore-Reef (Red Algae Zone)
Mesophotic Reef
Euphotic Fore-Reef
Wall/Drop Off
The Cryptos
Spur and Groove
Barren Zone
Reef Sections: Back-Reef/Lagoon
Reef Flat
Carbonate Shelf
Sand and Mud Bottoms
Seagrass and Algae Beds
Hardgrounds
Patchreef/Fringing Reefs
Mangroves
Cays (not a true reef zone)
Salt Turns (not a true reef zone)
Reef Sections: Reef Crest
Algal Pavement
Reef Crest/Algal Rim
Reef Sections: Aphotic
Hard to Research, requires a submersible
Very dark, zero light.
Reef Sections: Disphotic (Rariphotic)
Very little light, not enough for growth
Lower bounds of true reef zones.
Reef Sections: Deep Fore-Reef (Red Algae Zone)
Lowest photic zone
Some autotrophs can live deeper than others, depends on clarity.
The algae is red because red light is absorbed first, blue and green wavelengths reach the deepest, and the algae needs as much light as it can get.
Reef Sections: Mesophotic
Lowest level to support minimal coral/plant growth.
Too deep for divers, requires subs and rebreathers.
Contains tons of cavities and crevices for species to take refuge, supporting biodiversity.
Important for conservation of reefs—it is shielded from sedimentation and overfishing.
Reef Sections: Euphotic Fore-Reef
Platy Coral Zone
Massive Coral Zone
High Diversity Zone
Branching Coral Zone
Receives the most light.
Most diverse and active zone.
Reef Sections: Wall/Drop Off
Creates areas for species to take refuge and breed.
Absorbs many large waves that would otherwise damage the inner lagoons.
Prevents coastal erosion.
Reef Sections: Cryptos
All of the microhabitats hidden below coral (dark crevices, tunnels, and coral undersurfaces).
Created by accretion and bioerosion.
Extremely important and diverse as it provides tons of shelter for organisms.
Up to 8X the surface area hidden under in this zone compared to the visible surface.
Contains 40% of species and 60% of biomass contributed to higher trophic levels.
Reef Sections: Spur and Groove
Prominent in fairly shallow water.
Spurs shoot up from coral growth, grooves dip down between.
Creates tons of space for species to hide.
Reef Sections: Barren Zone
Absorbs full energy of waves.
Dominated by strong branching corals.
Relatively close to the reef crest.
Waves from storms will break in the barren zone before they can reach the reef crest.
Reef Sections: Algal Pavement
Contains tons of encrusting algae towards the shallow surface leading to the reef crest.
Made of a relatively flat, hard rock surface that prevents and absorbs heavy wave breaks.
Reef Sections: Algal Rim (Reef Crest)
Reef crest is often exposed at low tide.
Algal ridge surrounds reef crest and holds in water for the corals.
Reef Sections: Reef Flat
Landward of the crest.
Flat area, surface close to sea-level.
Can be a productive reef environment, best developed in fringing reefs.
Reef Sections: Carbonate Shelf
Lagoon, wide and shallow
Protected by barrier reef from surf, calm area.
Variety of islands and patch reefs
Produces a lot of carbonate
Reef Sections: Sand and Mud Bottoms
Loose carbonate sand, mud, and silt.
Home to many burrowing organisms.
Can be home to seagrass beds hosting many small fish.
Hunting grounds for larger marine predators.
Reef Sections: Seagrass and Algae Beds
Algae produce tons of carbonate.
Seagrass and associated invertebrates are a major energy source for the reef.
Fish will hide in the reef during the day and forage over grass beds at night.
Reef Sections: Hardgrounds
Allows organisms to anchor and grow relatively high.
Transition zone to the main coral zones.
Provides moderate shelter for many different organisms.
Reef Sections: Patch Reefs/Fringing Reefs
Fringing reefs occur around cays
Patch reefs occur on ancient high points
Reef Sections: Mangroves
Patches of trees, tiny shrubs, and plants that have adapted to grow directly in seawater.
Not a ton of diversity in the trees themselves, but they support a high diversity of aquatic life and nutrient production.
Protect islands from storms.
Provide tons of shelter and habitats for many different organisms.
Act as a nursery for many fish.
Reef Sections: Cays and Salt Turns
Help absorb waves.
Filter nutrients and salt.
Support biodiversity, serve as nursery grounds for fish.