The Vulnerability of Coral Reefs

 
Vulnerability of coral reefs
 
Janice Lough
 
Moving reefs out of comfort zone
 
Hoegh-Guldberg et al 2007
 
Outline Coral Reefs
 
key coastal ecosystem
many different reef types
narrow environmental limits
already shown impacts, e.g. bleaching
combined effects of disturbances
less time to recover
simpler reefs
healthy reefs will cope better
 
 
 
 
Many different types of reefs
 
13/22 PICTS have more
reef than land area
(e.g. ~Fiji 40%)
dominant coastal
habitat
majority are oceanic
great diversity of reef
types
 
With different levels of human use
 
support local
fisheries
differences in local
pressures
 
Location matters
 
fringing continental reefs
affected by river runoff
isolated oceanic reefs not
well connected e.g. larval
supplies
tropical cyclones> 10
o
from equator
El Niño/La Ni
ña impacts
 
Important environmental factors
 
 warmest parts of oceans
 narrow temperature range
 
warm water temperatures
shallow well-lit waters
low sediment and nutrients
right ocean chemistry 
Ω
 >3.3
 
Corals must build skeletons fast enough to
withstand natural forces of erosion
 
coral eaters
 
predators
 
waves
 
sunshine
 
tropical cyclones
 
A special relationship
 
symbiosis at heart of tropical coral reefs
photosynthetic algae live within coral animal
corals get enough energy for rapid calcification
form structurally complex reefs
home to thousands of other plants and animals
 
stressed corals lose algae (and their pigments)
coral bleaching
seen more frequently due to warmer temperatures
corals living only ~1-2
o
C below upper thermal limit
too much fresh water also causes bleaching
 
Relationship breaks down due to stress
Healthy - unbleached
Stressed - bleached
Recently dead
 
30% extra CO
2
 entered oceans
otherwise greater warming!
BUT changes ocean chemistry
harder to form skeletons &
shells
more erosion
 
Ocean acidification
 
Ocean acidification: natural laboratory
 
Fabricius et al 2011
 
high CO
2
 volcanic seeps, PNG
“winners” = massive corals
“losers” = branching, tabulate corals
reduced coral diversity
much simpler reef with lower pH
 
 
Warmer temperatures
 
 very high vulnerability
 already seen bleaching, diseases
 
More acidic ocean
 
 high vulnerability
 weaken reef framework
 
Stronger storms and heavier rainfall
 
 moderate vulnerability
 more disturbances = less time to recover
 
Higher sea level
 
 
 some corals may keep up
 loss of deeper corals
 
Opportunities for management
interventions
 
Anthony & Maynard 2011
 
Morris & Mackay (2008) Status
of coral reefs of the world 2008
 
value of monitoring – appears “stable” condition
tropical cyclones, bleaching, COTs
recovery after disturbance
localised pollution/overuse
34% of reefs classed at “low threat”
 
Reef status: Fiji
 
What it means for coral reefs
 
 
already shown vulnerability
 bleaching and diseases
 physical destruction
 weaker skeletons
 lower salinity
 connectivity between reefs
 direct & indirect effects on other reef organisms
 
Summary key issues
 
 
 
rates of change
 combined stressors
 less time to recover between disturbances
 can adaptation occur in decades rather than 1000’s years?
 healthy reefs better able to cope
 consequences for reef-dependent fisheries
 
Coral reefs will not disappear entirely BUT
likely to be
MUCH SIMPLER ECOSYSTEMS
 
Thank you
 
j.lough@aims.gov.au
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Coral reefs, key coastal ecosystems, face various stressors such as bleaching and human pressures, impacting their ability to recover. With diverse reef types and environmental factors at play, the delicate balance of these underwater marvels is crucial for their survival. The special symbiotic relationship between corals and algae forms the basis of these vibrant ecosystems, but increasing stressors like coral bleaching threaten this delicate harmony. Location, human use, and environmental conditions all play pivotal roles in determining the health and resilience of coral reefs.

  • Coral reefs
  • Ecosystems
  • Environmental factors
  • Human impact
  • Symbiotic relationship

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  1. Vulnerability of coral reefs Janice Lough

  2. Moving reefs out of comfort zone Hoegh-Guldberg et al 2007

  3. Outline Coral Reefs key coastal ecosystem many different reef types narrow environmental limits already shown impacts, e.g. bleaching combined effects of disturbances less time to recover simpler reefs healthy reefs will cope better

  4. Many different types of reefs 13/22 PICTS have more reef than land area (e.g. ~Fiji 40%) dominant coastal habitat majority are oceanic great diversity of reef types

  5. With different levels of human use support local fisheries differences in local pressures

  6. Location matters fringing continental reefs affected by river runoff isolated oceanic reefs not well connected e.g. larval supplies tropical cyclones> 10o from equator El Ni o/La Ni a impacts

  7. Important environmental factors warm water temperatures shallow well-lit waters low sediment and nutrients right ocean chemistry >3.3 warmest parts of oceans narrow temperature range

  8. Corals must build skeletons fast enough to withstand natural forces of erosion tropical cyclones waves sunshine predators coral eaters

  9. A special relationship symbiosis at heart of tropical coral reefs photosynthetic algae live within coral animal corals get enough energy for rapid calcification form structurally complex reefs home to thousands of other plants and animals

  10. Relationship breaks down due to stress stressed corals lose algae (and their pigments) coral bleaching seen more frequently due to warmer temperatures corals living only ~1-2oC below upper thermal limit too much fresh water also causes bleaching Healthy - unbleached Recently dead Stressed - bleached

  11. Ocean acidification 30% extra CO2entered oceans otherwise greater warming! BUT changes ocean chemistry harder to form skeletons & shells more erosion

  12. Ocean acidification: natural laboratory high CO2volcanic seeps, PNG winners = massive corals losers = branching, tabulate corals reduced coral diversity much simpler reef with lower pH Lower pH = 2100 Mid pH = 2050 Normal pH = now Fabricius et al 2011

  13. Warmer temperatures very high vulnerability already seen bleaching, diseases

  14. More acidic ocean high vulnerability weaken reef framework

  15. Stronger storms and heavier rainfall moderate vulnerability more disturbances = less time to recover

  16. Higher sea level some corals may keep up loss of deeper corals

  17. Opportunities for management interventions Anthony & Maynard 2011

  18. Reef status: Fiji value of monitoring appears stable condition tropical cyclones, bleaching, COTs recovery after disturbance localised pollution/overuse 34% of reefs classed at low threat Morris & Mackay (2008) Status of coral reefs of the world 2008

  19. What it means for coral reefs already shown vulnerability bleaching and diseases physical destruction weaker skeletons lower salinity connectivity between reefs direct & indirect effects on other reef organisms

  20. Summary key issues rates of change combined stressors less time to recover between disturbances can adaptation occur in decades rather than 1000 s years? healthy reefs better able to cope consequences for reef-dependent fisheries Coral reefs will not disappear entirely BUT likely to be MUCH SIMPLER ECOSYSTEMS

  21. Thank you j.lough@aims.gov.au

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