420 likes | 572 Views
Coral Bleaching. www.ogp.noaa.gov. Why Bleaching?. Sun exposed areas bleach first. Photosynthesis (normal conditions). Photosynthesis under thermal stress (Photoinhibition bleaching model). Thermal thresholds (Temperatures at which bleaching occurs). Hoegh-Guldberg 1999. La Niña. El Niño.
E N D
Coral Bleaching www.ogp.noaa.gov
Photosynthesis under thermal stress(Photoinhibition bleaching model)
Thermal thresholds(Temperatures at which bleaching occurs) Hoegh-Guldberg 1999
La Niña El Niño
Tahiti Sea Surface temperature Hoegh-Guldberg 1999
Number of reefs severely bleaching Hoegh-Guldberg 1999
Question 1: • Why are corals growing so close to their thermal limit?
Predicted evolution SST(Global coupled atmosphere-ocean-ice model) Hoegh-Guldberg 1999
Question 2: • Why are corals growing so close to their thermal limit? • Why are there few reports of coral bleaching before 1979?
Predicted evolution SST(Global coupled atmosphere-ocean-ice model) Hoegh-Guldberg 1999
Question 3: • Why are corals growing so close to their thermal limit? • Why are there few reports of coral bleaching before 1979? • Will coral bleaching increase in the future?
Possible scenarios of increasing SST • Strategy shift: • Hardy spp. replace sensitive spp. • Tolerance: Corals acclimate + evolve • spp. with highest genetic variability expected to survive • Phase shift: corals are replaced by algae • Already occurring in many regions!
Simple Model Model with interspecific differences in thermal thresholds Model with thermal threshold differences + acclimation & evolution Hughes et al. 2003
Interspecific bleaching Susceptibility Diverse Communities Monospecific communities
Interspecific Bleaching Susceptibility Raiatea, French Polynesia (May 2002) Hughes et al. 2003
Coral species boundaries(geographical differences) • 1- Local Temperature differences • 2- Genetic Variability differences • Low-Isolated endemic populations • High-Central and Mainland populations Hughes et al. 2003
Facts on the future of Coral Reefs due to Global warming • Few indications that coral acclimation / rapid evolution is occurring • Oceans warming 2oC / 100 years • Annual massive bleaching events by 2030-2070 • Phase shift away from coral dominated communities by 2050 • Economical impact of Trillions of $, affecting 100’s of million humans
Coral-Algae Phase Shift (Jamaica) Algae Coral (% cover) • 3% 53% 1995 92% 4%
Coral reef herbivores? • Green Turtles • Ecologically extinct • Manatees & Dugongs • Ecologically extinct • Parrotfish (& surgeonfish) • Generally overfished • Sea Urchins • Variable abundance (diseases & predation)
Jamaican History 101 • 1492: 16 million Green Turtles (Caribbean) • 1688-1730:13000 turtles/year (slave food) • 1730: 6.5 million Turtles (Caribbean) • 1800:Turtle fishery crashes, Fish fishery develops • 1881:Jamaica imports 85% of its fish (local overfishing) • 1962:Historicalhigh fishery catches (15% local origin) (local overfishing still) No Turtles, No manatees, Very few parrotfish ONLY SEA URCHINS LEFT (Diadema antillarum)
Jamaican History 102 • 1980: Hurricane Allen • 1983: Diadema die-off across Caribbean (99% mortal.) NO HERBIVORES LEFT! • Late 1980’s:Shift to Algal Domination • 1991: Hurricane Gilbert • Today: • Algae dominate reefs • Extensive overfishing of herbivore fish species • Slow and patchy recovery of Sea Urchins populations
Historical coral reef community changes % reef sites P = Prehuman H = Hunter Gatherer A = Agricultural CO+CD = Colonial M1 = Modern M2 = Present
Increase Coral Diseases Massive Bleaching OVERFISHING Historical coral reef degradation
Principle 15 of the Rio Declaration • “Where there are threats of serious or irreversible damage, lack of full scientific certainty shall not be used as a reason for postponing cost-effective measures to prevent environmental degradation.”