Coral Bleaching and the Carbon Cycle
Coral Bleaching and the Carbon Cycle Notes
Coral Bleaching Overview
Definition: Coral bleaching is a phenomenon where corals expel the symbiotic algae (zooxanthellae) living in their tissues, often due to stress factors such as temperature changes.
Causes of Bleaching:
Elevated water temperatures, often measured as 1°C above the Maximum Monthly Mean (MMM).
Other stress factors can include ocean acidification, pollution, and loss of water clarity.
Recent Events in Florida Keys
July 2023 Incident:
Southern Florida Keys experienced severe coral bleaching due to record high sea temperatures.
Record temperatures reached as high as 33.60°C on July 13, exceeding the bleaching threshold.
This has raised concerns for mass mortality events among the coral populations.
Temperature Measurements:
MMM for Florida Keys: 29.63°C
Bleaching Threshold: 30.63°C
Start of Bleaching: June 14, 2023 (crossed threshold).
Coral Reef Basics
Coral Location: Typically found within 23 degrees north and south of the equator.
Significance: These regions are known as biodiversity hotspots, often referred to as the "rainforests of the sea."
Important Facts About Corals
Classification:
Corals are marine animals belonging to the class Anthozoa (related to jellyfish and anemones).
Over 6,000 species exist.
Structure: Corals are colonial invertebrates that consist of numerous tiny animals called polyps.
Symbiosis:
Coral polyps engage in a symbiotic relationship with algae (zooxanthellae), which perform photosynthesis and provide essential nutrients.
Algae live within the coral's tissues offering glucose and oxygen, vital for coral health.
Effects of the Carbon Cycle on Coral Bleaching
Relationship Between Carbon Cycle and Coral: Elevated CO2 levels lead to ocean acidification, affecting coral growth and resilience to bleaching.
Importance of Monitoring: Understanding how carbon emissions impact coral reefs is crucial for mitigating risk and managing reefs effectively.
Coral Bleaching Activities: Research and Data Analysis
Task Overview: Identify coral bleaching trends across four different locations for insights and comparisons.
Locations: Asuncion Island, Abul Thama (Bahrain), Clipperton Island (France), Martin (Florida).
Data Collection and Analysis:
Temperature data and heat stress measurements for three periods: 2001-2002, 2009-2010, and 2013-2014.
Higher heat stress correlates with significant bleaching events.
Key Measurements:
Heat Stress is quantified as the area under the sea surface temperature curve exceeding the MMM line.
Trends over the given years should be assessed to compare how coral reef locations respond differently to temperature changes.
Conclusion
Ongoing monitoring and research are essential for understanding coral bleaching and developing strategies to protect these vital ecosystems amidst changing carbon levels and temperature extremes.