Rising sea temperatures due to climate change are causing tropical marine species to move from the equator towards the poles, according to a study. The research, published in the journal Trends in Ecology and Evolution, also shows that temperate species are receding as it gets too warm, they face increased competition for habitat, and new predators arrive on the scene.
Climate Change Cause Tropicalisation as per the Study
Tropicalisation
- Climate change is causing a marine phenomenon known as tropicalisation, where tropical species expand their range while temperate species retract.
- Temperate species are receding as it gets too warm, they face increased competition for habitat, and new predators arrive on the scene.
- This global shift is altering ocean ecosystems, biodiversity, and could impact the global economy.
- The first instance of this process was identified in the Mediterranean Sea.
- The Mediterranean Sea is considered as a “tropicalisation hotspot” due to an increase in tropical species.
Species Dispersal due to Climate change
- Climate change has altered the physical factors that affect species dispersal, such as ocean currents in areas that separate tropical/subtropical and temperate regions.
- These warm-water boundary currents are heating faster than the global seawater average, facilitating the poleward movement of species, and reinforcing the retraction of temperate species.
- Example: Range-expanding tropical damselfishes and temperate reef fishes have been documented altering their feeding and social behaviors to allow for coexistence,
Evolution of New Traits
- Changes in how species interact can result in the evolution of new traits or behaviors due to the close connection between ecology and evolution.
Ocean Warming
- The ocean absorbs most of the excess heat from greenhouse gas emissions, leading to rising ocean temperatures.
Reason
- Greenhouse Gas Emissions: The burning of fossil fuels (coal, oil, and natural gas) for energy, deforestation, and industrial processes releases significant amounts of greenhouse gasses, including carbon dioxide (CO2), methane (CH4), and nitrous oxide (N2O), into the atmosphere. These gases trap heat, leading to a warming effect on both the atmosphere and the oceans.
- Carbon Dioxide Absorption: Oceans act as a vast reservoir that absorbs a significant portion of the excess carbon dioxide from human activities. While this absorption helps mitigate climate change on land, it also results in the warming of the ocean itself.
- Solar Radiation: Changes in solar radiation, though a minor contributor compared to human-induced factors, can influence ocean temperatures over long periods.
Impact
- Coral Bleaching: Elevated temperatures can cause corals to expel the symbiotic algae living in their tissues, leading to coral bleaching. Prolonged bleaching weakens corals and makes them more susceptible to diseases, posing a significant threat to coral reef ecosystems.
- Sea Level Rise: Warmer ocean temperatures contribute to the thermal expansion of seawater. This, along with the melting of polar ice caps and glaciers, leads to rising sea levels, which can result in coastal erosion and increased vulnerability of coastal communities.
- Disruption of Marine Food Webs: Changes in ocean temperatures can alter the distribution and abundance of marine species, affecting the structure of marine food webs. This can have cascading effects on fisheries and the livelihoods of communities dependent on them.
- Ocean Acidification: The absorption of excess carbon dioxide by the oceans leads to ocean acidification. Acidification can harm marine organisms with calcium carbonate skeletons or shells, including corals, mollusks, and some plankton, affecting the entire marine food chain.