Tropical Ecosystems
- Created by: rosieevie
- Created on: 28-05-17 18:01
Early History of Tropical Research
Alfred Russell Wallace
- Early Indo-West Pacific explorer
- Father of biogeography
- Independently theorized evolution by natural selection
Charles Darwin
Alexander Von Humboldt
- Nearer approach the tropics - greater increase in variety of structure, grace or form,
Diversity Gradients - Hypotheses on Origin and Mai
Biodiversity highest in tropics - many hypotheses as to why
Early ecological hypotheses - related to area effects (larger and more connected), species coexistence (nich partitioning) and temperature effects
Later evolutionary (geographic differences between speciation and extinction rates) and historical hypothesis (tropics older than temperature latitudes)
More likely, latitudinal gradient best described as intergration of ecological, evolutionary and historical factors
HIGHEST SPECIES RICHNESS AT THE EQUATOR
Why Marine Islands are Farther Apart in the Tropic
James Brown - hypothesised marine species diversity gradients explained by combining metabolic theory with biogeography
Tropical areas warmer than temperate areas = increased evolutionary speed and:
- Increased metabolic rate
- Reduced life span
- More/shorter generation times = higher DNA mutation rates
- Speeds up growth rates
- Shorter larval development = shorter dispersal distances
Larval dispersal + high temperature = difficulty for marine species to disperse between island in tropics
= Islands metaphorically 'father' away (larval development faster and dispersal lower)
Explains Indo-West Pacific marine biodiversity hotspot
Over large timescales - big efffect on evolution of new species = allopatric speciation
Models of Biodiversification
In order to discuss factors driving diversity gradients - conceptual models of geographic scenarios of bio-diversification. 5 scenarios:
- Cradles - extinction constant, speciation highest in tropics
- Museums - extinction low in tropics, speciation constant
- Out of the tropics - high speciation, low extinction, dispersal out of tropics
- Casino - high speciation, high extinction, dispersal in tropics
- Intro the tropical museum - low extinction, speciation constant, dispersal into tropics
In general, regional or global patterns of biodiversity are function of geographical differences between speciation, extinction and dispersal rates over space and time.
Data needs to be tested - which geographical scenario applicable to study system
Use fossils or moden records
Eastern Pacific rocky intertidal gastropod latitudinal diversity gradient and worldwide diversity of marin bivalves examples - high diversities, well known taxonomy/ecology and excellent fossil record
Eastern Pacific Rocky Shore Gastropod Case Study
Latitudinal diversity gradient = into the tropical museum hypothesis
Low extinction in tropics, constant speciation rates and dispersal into the tropics
Study restricted to gastropods from one habitat type - rocky shores - very few of these habitats in tropics = difficulty to immigrate
Species originating in rocky shore 'islands' in temperate regions:
- Short distances between habitats
- Longer dispersal distances
- Evolved in highly seasonal environments
- Capable of dispersal into tropics over time
Species originating in tropics:
- Long distances between habitats
- Shorter dispersal times
- Evolved in warm environments
- Less capable of dispersing out of tropics
Worldwide Marine Bivalves Case Study
Bivalve species pooled across depths
= Out of tropics scenario = high speciation rates, low extinction rates and net dispersal of larvae out of tropics
Study included many different habitat types
Pooling across habitats erases distance between islands - affect results
Controlling for habitat is key
Coral Reefs - Hermatypic Corals
Hermatypic corals = reef building corals
Phylum Cnidaria, class Anthozoa, order Scleractina - hard, stony corals
Contain zooxanthellae - limited to photic zone
Ahermatypic corals - non-reef building with no zooxanthellae
Environmental limits - shallow water tropic regions;
- Temperature - 18-36C, optimum 26-28C
- Light - <10m but can be <30m - light for zooxanthellae photosynthesis
- Salinity - high salinity 33-35
- Wave action - high wave energy but constant risk of storms/hurricanes = growth/erosion cycle
- Sediment load - no sediments, causes smothering, shading and abrasion (no estuaries)
Earliest fossils - Triassic Period (~240mya), after late Permian mass extinction
Scleractina not first reef-building animals - rugrose corals, stromatolites and bivalves can also build reefs
Coral-Zooxanthellae Symbiosis
Hermatypic corals have symbiotic dinoflagellates - only in photic zone
Transfered via reproduction or direct from water
Benefits for both organisms - mutualism
Zooxanthellae
- Provide growth energy in form of carbohydrates, lipids, oxygen during photosynethsis
- Rapid uptake of CO2 - enhanced CaCO3 deposition at coral base = reef building
- Remove organic waste
Algae obtain nutrients from host and direct seawater upyake
Coral hosts:
- Give access to sunlight for photosynthesis
- Give stable,protected environment
- Provide coral metabolic waste
Stress and Coral Bleaching
Bleaching - generalised response to stress = zooxanthellae ejected from polyp
= decreased growth and reproduction = death
If temperature of water too high, bleaching occurs - during El Nino and climate change
Warm water temperatures higher than average summer for 4 weeks = bleaching
Excessive sunlight, calm seas and low tides also = bleaching
Now in 3rd coral bleaching event (lasted since 2014) - longest bleaching event ever recorded
Reef Types and Zonation
Fringing reef - close to shore
Barrier reef - often surrounds tropical islands and seperated from land by 1-10km wide lagoon
Atoll reef - form around volcanic islands - start off as volcanic island with fringing reef as island subsides/sea level rises, coral grow rapidly on outer edge = barrier reef. Eventually island is lost but outer ring-shaped atoll remains
Patch reefs (bommies) - smalls areas of reef in shallow lagoon area
Divisions of a reef:
- Shore - sandy beach
- Back reef - shallow lagoon areas - 10sm to 1000m (small patch reefs and seagrass beds)
- Reef flat - strong wave action w/ smooth coral free-area of encrusting coarline algae
- Fore reef - building most rapid (ideal conditions), dominated by elkhorn coral or staghorn if calm
- Drop off - plate corals catch more light due to less wave action and more sediment
Reef Ecology
Coral reefs - extremely diverse systems - large variety of primary producers with high biomass
Species richness not uniform - divided into 3 major global regions
- Indo-west pacific - biggest area/most diverse
- Eastern Pacific - smallest area
- Western Atlantic - impoverished fauna
Most nutrients cycle internally - close coupling of plants and animals (inc. symbiosis) = low f-ratio (little regenerated nutrients) and low net production (respiration)
Space limiting - competition for space and light
- Expoitative competition = corals shading out others
- Interference competition = coral extrude gastric filaments and sweeper tentacles kill of polyps of neighbour (branching corals)
- Massive corals counter by being shade tolerant = competitive hierarchies with depth
Predatory pressure constant
Corallivorous, herbivorous and omnivorous fish influence community structure
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