New research on stony coral tissue loss disease reveals similar “bacterial signatures” among sick corals and nearby water and sediments for the first time. Results hint at how this deadly disease might spread, and which bacteria are associated with it, on Florida’s Coral Reef.
A new study by coral researchers from the University of Miami’s Cooperative Institute for Marine and Atmospheric Studies (CIMAS) and NOAA’s Atlantic Oceanographic and Meteorological Laboratory suggests that the physical oceanographic habitat characteristics-such as, temperature, light availability, and water flow, of corals, may influence microbe communities and health of coral reefs. The results showed a link between physical habitat and coral microbiology in coral reefs in southeast Florida.
Warm ocean water can be a killer for coral reefs, and AOML recently developed a new inexpensive sensor to drastically improve our ability to measure and monitor changing temperatures on reefs at an unprecedented scale. The low cost sea temperature sensor, known as InSituSea, costs roughly $10 in parts to produce while providing high accuracy (0.05-0.1 C) in measurement. With a production cost that is 10% of an off-the-shelf temperature sensor, colleagues have expressed strong interest in deploying the InSituSea sea temperature sensor at coral reefs around the world.
Coral Health and Monitoring Program (CHAMP) researchers at AOML have worked cooperatively with the Caribbean Community Climate Change Centre (CCCCC), headquartered in Belize, over the past several years to install Coral Reef Early Warning System (CREWS) stations at key coral reef sites in countries throughout the Caribbean. CREWS stations monitor an array of atmospheric and oceanographic parameters to assess the health and integrity of coral reefs. The stations are part of the CCCCC’s efforts to strengthen the Caribbean region’s ability to respond to climate variability, extreme weather conditions, pollution, and habitat change.
The new research published online August 10 in Nature Climate Change provides a stark look into the future of ocean acidification – the absorption by the global oceans of increasing amounts of human-caused carbon dioxide emissions. Scientists predict that elevated carbon dioxide absorbed by the global oceans will drive similar ecosystem shifts, making it difficult for coral to build skeletons and easier for other plants and animals to erode them.
On May 13th, the White House Office of Science and Technology Policy introduced the National Microbiome Initiative, an effort to support multi-agency research to help sample and better understand communities of microorganisms that are critical to both human health and the world’s ecosystems. As the nation’s premier ocean science agency, NOAA is leading interdisciplinary research to improve observation and assessment of marine microbiomes. To support this national initiative, NOAA’s Atlantic Oceanographic and Meteorological Laboratory (AOML) received nearly $2 million in funding this year to conduct a number of projects that integrate genetic sampling techniques and technologies to help advance the understanding of the ocean’s microbiomes.
When Barack Obama becomes the first president to visit Cuba since Calvin Coolidge, his visit will highlight not only a new course in international relations, but showcase on-going scientific opportunities with the country only 90 miles off the Florida coast.
For the third time in recorded history, a massive coral bleaching event is unfolding throughout the world’s oceans, stretching from the Indian Ocean to the Caribbean. Above average sea surface temperatures exacerbated by a strong El Niño could result in the planet losing up to 4,500 square miles of coral this year alone, according to NOAA. The global event is predicted to continue to impact reefs into the spring of 2016.
Scientists from NOAA and the Cooperative Institute for Marine and Atmospheric Studies at the University of Miami have documented a dramatic shift from vibrant coral communities to carpets of algae in remote Pacific Ocean waters where an undersea volcano spews carbon dioxide.
