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#1
Coral reefs have fuelled severe global warming in Earth's past
#1 out of 2
20h ago

Coral reefs have fuelled severe global warming in Earth's past

  • New research shows coral reefs may have increased atmospheric CO2 by producing calcium carbonate in Earth's past.
  • The study models coral–plankton balance over 250 million years to explain past climate shifts.
  • Periods of extensive reef growth may have disrupted the carbon cycle and warmed oceans in the deep past.
  • When reef coverage declines, deeper-sea carbonate burial can lower CO2 and cool the climate over long timescales.
  • The researchers caution that deep-time feedbacks operate over long timescales and may not apply to today’s rapid changes.
  • Experts say reef–plankton interactions illustrate a co-evolving feedback between life and climate.
  • The study highlights potential reef contributions to climate feedbacks beyond corals, including ancient microbial communities.
  • The research emphasizes the need to consider historical carbon-cycle dynamics when modeling future climate.
  • Carbon cycling disruptions in the past were linked to shifts in reef extent and nutrient dynamics.
  • The article notes the implications for understanding how life interacts with climate over geological timescales.
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#2
Coral reefs kept Earth's carbon cycle stable for 250 million years - Oceanographic
#2 out of 2
7h ago

Coral reefs kept Earth's carbon cycle stable for 250 million years - Oceanographic

  • New research shows coral reefs shifted Earth’s carbon cycle for over 250 million years, affecting climate recovery.
  • Shallow-water reef growth reduced deep-ocean exchange, slowing the planet’s CO₂ rebound after disturbances.
  • When reef space collapsed, deep-sea carbonate burial rose, boosting plankton productivity and speeding recovery.
  • Study portrays reefs as active climate modulators, not just passive recorders of change.
  • Researchers used plate tectonics, climate simulations, and ecological modeling to trace past carbonate production.
  • Today’s reefs face rapid decline from warming and acidification, potentially limiting stabilizing effects on carbon.
  • The study warns that ecological losses would delay any geological-scale recovery.
  • Shallow-reef dynamics influenced marine plankton evolution and long-term ocean chemistry.
  • Researchers emphasize learning from the deep past to understand modern carbon dynamics.
  • Authors warn that stabilizing effects depend on preserving reef ecosystems.
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