Projected changes to coral reefs, mangroves and seagrasses Solomon Islands Government Based on...... Outline • • • • Coastal habitats: roles and values Requirements for good coral growth Recent stresses on coral reefs Projected effects of climate change on: – coral reefs – mangroves – seagrasses • Key management measures Requirements for good coral growth • Warm water temperatures • Shallow well-lit waters • Low sediment and nutrients • Right ocean chemistry Coral reefs grow in the warmest parts of oceans & have a narrow temperature range Corals must build skeletons fast enough to withstand natural forces of erosion waves cyclones & storms bleaching predators coral eaters 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 Stresses – higher water temperatures • Stressed corals lose algae (and their pigments) • Coral bleaching • Corals living only ~1-2oC below upper thermal limit • Too much freshwater can also cause bleaching Healthy - unbleached Stressed - bleached Recently dead Stresses – ocean acidification • 30% extra CO2 entered ocean • Changes ocean chemistry • Harder to form skeletons • Greater coral erosion Ocean acidification: natural laboratory • High CO2 volcanic seeps, PNG • “Winners” = massive corals • “Losers” = branching, tabulate corals • Reduced coral diversity • Much simpler reef with lower pH Normal pH = now Mid pH = 2050 Lower pH = 2100 Fabricius et al 2011 Projected effects of climate change Projected climate change 1980–1999 average 2035 A2 2050 A2 2100 A2 Air temperature (°C) 27.4 +0.5 to +1.0 +1.0 to +1.5 +2.5 to +3.0 Sea surface temperature (°C) 27.3 +0.7 to +0.8 +1.2 to +1.6 +2.2 to +2.7 +5 to +20 +10 to +20 +10 to +20 -5 to -20 -5 to -20 -5 to -20 Rainfall: equatorial (%) Rainfall: subtropics (%) n/a Sea level (cm) +6a +20 to +30 Ocean pH (units) 8.1 -0.1 Cyclones & storms 9 a = since 1960 +70 to +110 -0.2 +90 to +140 -0.3 Number of cyclones/storms may decrease but likely to be more intense Warmer water temperatures • Reefs very high vulnerability • Increased bleaching, ~1% loss per year by 2035 More acidic ocean • Reefs have high vulnerability • Weaker reef frameworks Stronger storms and heavier rainfall • Moderate vulnerability of reefs • More disturbances = less time to recover Higher sea level • Some corals may keep up • Loss of deeper corals Opportunities for interventions Anthony & Maynard 2011 What climate change means for reefs • More bleaching and diseases • Weaker skeletons • Physical destruction • Less time to recover between disturbances • Healthy reefs better able to cope Coral reefs will not disappear entirely BUT likely to be MUCH SIMPLER ECOSYSTEMS Mangroves: role Vulnerability of mangroves • Most vulnerable to: – sea-level rise – increasing storm intensity • Ability to adapt by migrating landward as sea-level rises but human barriers may constrain movement • Overall moderate-high vulnerability to climate change Overall vulnerability of mangroves Sea surface Solar temperature radiation Ocean chemistry Cyclones & storms Rainfall patterns Sea level Nutrients Low High Low Mangroves 2035 A2 Very low Low Very low Moderate 2050 A2 Very low Low Very low Moderate Moderate Very high Low 2100 A2 Very low Low Very low Moderate Moderate Very high Low Projected loss of mangroves in Solomon Islands From 525 km2 today: Year Mangrove area (%) 2035 -10 2050 -50 2100 -60 Unlikely Somewhat likely Likely Very low Very likely Very likely 29% Low 66% Medium 90% 100% High Very high Confidence Likelihood 0% Very low Confidence Likely Likelihood 0% Unlikely Somewhat likely 29% Low 66% Medium 90% 100% High Very high 0% 5% 33% 66% 95% 100% Vulnerability of seagrasses • Most vulnerable to: – Warmer waters – Increased rainfall (turbidity) – Increasing storm intensity – Reduced light • Limited ability to adapt • Overall moderate vulnerability to climate change Overall vulnerability of seagrasses Sea surface Solar temperature radiation Seagrasses 2035 A2 2050 A2 2100 A2 Moderate Moderate Moderate Moderate High High Ocean chemistry Cyclones & storms Very low Very low Very low Rainfall patterns Sea level Nutrients Moderate Moderate Low Low Moderate Moderate Low Low Moderate Moderate High High Projected loss of seagrass in Solomon Islands From 66 km2 today: Year Seagrass area (%) 2035 -5 to -20 2050 -5 to -30 2100 -10 to -35 Unlikely Somewhat likely Likely Very low Very likely Very likely 29% Low 66% Medium 90% 100% High Very high Confidence Likelihood 0% Very low Confidence Likely Likelihood 0% Unlikely Somewhat likely 29% Low 66% Medium 90% 100% High Very high 0% 5% 33% 66% 95% 100% Key management measures 1. Build health of coral reefs, mangroves and seagrass by addressing existing threats: • Integrated catchment management • Foster the care of coastal fish habitats • Manage and restore coastal vegetation 2. New measures to allow future adaptation of mangroves: • Provide for landward migration Conclusions • Coral reefs, mangroves and seagrasses in Solomon Islands are expected to decline in area due to climate change • Acting now to manage existing threats and allow for future adaptation is vital for these habitats • Coastal fisheries that depend on these habitats will be affected as these habitats degrade Thank you j.johnson@c2o.net.au