Coral bleaching
node · earth · Global tropical reefs
The breakdown of the coral-algal symbiosis under stress, in which the host loses its symbionts, or the symbionts lose their pigments, and the white skeleton becomes visible through the transparent tissue. The dominant trigger on modern reefs is heat: sea temperature held roughly one degree Celsius above the local maximum monthly mean for a period of weeks, with high light making it worse and cloud or turbidity making it better. The mechanism is understood in outline as damage to photosystem II in the symbiont under combined heat and light stress, producing reactive oxygen species that the host expels the symbiont to escape. The crucial point for a reader is that bleaching is not death. A bleached colony is starving, not destroyed; if the heat abates within weeks it can re-acquire symbionts and survive, though often with reduced growth and no reproduction that year. If the heat persists, it starves. Cold shock, freshwater, sedimentation and disease can bleach coral too, which is why an individual bleached colony is not by itself evidence of a marine heatwave.
Read in · 1
Evidence · 3
Timeline
No dated observations are stored for this object. Atlas shows what was observed and when — it does not infer a history.
Connections · 2
- Reef-building corals (Scleractinia)affects
- Marine heatwavecaused_by
Assembled narrative · 1
Assembled from 43 blocks · 3 evidence · 22 related
- Story
- The breakdown of the coral-algal symbiosis under stress, in which the host loses its symbionts, or the symbionts lose their pigments, and the white skeleton becomes visible through the transparent tissue. The dominant trigger on modern reefs is heat: sea temperature held roughly one degree Celsius above the local maximum monthly mean for a period of weeks, with high light making it worse and cloud or turbidity making it better. The mechanism is understood in outline as damage to photosystem II in the symbiont under combined heat and light stress, producing reactive oxygen species that the host expels the symbiont to escape. The crucial point for a reader is that bleaching is not death. A bleached colony is starving, not destroyed; if the heat abates within weeks it can re-acquire symbionts and survive, though often with reduced growth and no reproduction that year. If the heat persists, it starves. Cold shock, freshwater, sedimentation and disease can bleach coral too, which is why an individual bleached colony is not by itself evidence of a marine heatwave.
- Knowledge
- Reef-building corals (Scleractinia)
- Coral bleaching
- Marine heatwave
- Connections
- Reef-building corals (Scleractinia)
- Marine heatwave
- Degree Heating Weeks (DHW)
- Symbiont shuffling and thermal tolerance
- The first global mass bleaching event
- A published projection that reefs would bleach faster than they could recover
- The second global bleaching event
- The third global bleaching event
- Mass bleaching on the Great Barrier Reef
- A second consecutive year of mass bleaching on the Great Barrier Reef
- The interval between severe bleaching events is measured, and it has collapsed
- Mass bleaching on the Great Barrier Reef during a La Nina
- The fourth global bleaching event is confirmed
- The fifth mass bleaching on the Great Barrier Reef since 2016
- The current state of the fourth global bleaching event is not established in this package
- Marine heatwave
- Zooxanthellae (Symbiodiniaceae)
- Zooxanthellae (Symbiodiniaceae)
- Coral bleaching
- Crown-of-thorns starfish (Acanthaster)
- Elkhorn coral (Acropora palmata)
- Darwin publishes The Structure and Distribution of Coral Reefs
- The first global mass bleaching event
- A published projection that reefs would bleach faster than they could recover
- Mass bleaching on the Great Barrier Reef
- The interval between severe bleaching events is measured, and it has collapsed
- Reef-building corals (Scleractinia)
- Coral bleaching
- Thermal refugia
- Coral restoration methods
- Mass bleaching on the Great Barrier Reef during a La Nina
- Extreme water temperatures in the Florida Keys kill nursery and wild coral
- Evidence
- On projected warming, the interval between bleaching events would fall below the interval corals need to recover, making event frequency rather than event severity the binding constraint on reefs. V55 verification basis: not consulted in this session; identified and summarised from the producing model's knowledge of the paper and its subsequent reception.
- Reef thermal stress is measured as HotSpot (sea surface temperature above the local maximum monthly mean) accumulated over a rolling twelve-week window into Degree Heating Weeks, with roughly four DHW indicating likely significant bleaching and roughly eight indicating likely widespread bleaching and mortality. V55 verification basis: the product documentation was NOT retrieved — coralreefwatch.noaa.gov was refused by the egress proxy — and these definitions and thresholds are stated from the producing model's working knowledge of the products. Any alert levels added above Level 2 are not described here.
- In the 2016 Great Barrier Reef bleaching event only a small minority of the more than eleven hundred reefs surveyed escaped bleaching, with the most severe bleaching in the northern third of the system, and water quality and past exposure did not protect reefs from it. V55 verification basis: not consulted; the survey design and headline result are stated from the producing model's knowledge, and the precise escaped-reef percentage is given as "around nine per cent" rather than to a decimal place.
Observed changes · 0
No public Signals are attached to this object. Signals show what changed and when it was observed — never a direction or a rank.
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