The study, published in the Proceedings of the Royal Society B, measured changes in the reef framework in several naturally high-carbon dioxide settings near Papua New Guinea. For the first time, scientists found increased activity of worms and other organisms that bore into the reef structure, resulting in a net loss of the framework that is the foundation of coral reef ecosystems.
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.
Corals live and thrive by maintaining a careful balance between their growth rate and the rate of erosion. Scientists already know the projected increases in carbon dioxide in our global oceans, known as ocean acidification, will slow the rate at which corals build the hard calcium carbonate skeletons that are the foundation of their habitat. A new study published online today in PLOS ONE demonstrates that in naturally highly acidified waters, these coral skeletons will also face increased erosion from microscopic organisms, called bioerosion. The result is accelerated breakdown and loss of reef structures, and potentially the loss of essential habitat.
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.
From March 1st through March 3rd, AOML coral scientists traveled to reefs in the Upper and Lower Florida Keys to swap out instruments being used for an ongoing coral bleaching study. Both pH and light loggers were collected and deployed at inshore and offshore study sites.
AOML coral researchers conducted a number of reef monitoring activities during the month of October at Cheeca Rocks off of Islamorada, Florida. Among the activities was the installation of new sensors to measure pH and photosynthetic light levels at the on-site MapCO2 buoy. The team also conducted benthic surveys and deployed a pH sensor at an inshore patch reef where they are conducting an experiment to examine the impacts of bleaching across Florida Keys reefs. They were also joined by a colleague from the University of Miami who conducted photo mosaic surveys of the reefs. A photo mosaic is a tool used by researchers to map reefscapes and involves the stitching together of hundreds of photos taken simultaneously across the reef to form one giant image. Photo mosaics provide coral researchers with an important tool to more accurately document community-wide changes in reef health.
AOML’s Coral Health and Monitoring Program (CHAMP) rolled out a new data source in October as part of its online data query tool. Optimally Interpolated Sea Surface Temperatures, or OISSTs, are data from microwave satellite observation platforms, products that are sourced from Remote Sensing Systems. Whereas other sea surface temperature sources might be missing data due to orbital gaps or non-ideal environmental conditions such as cloud cover or rainfall, the OISST platform corrects for these errors to provide a complete, daily sea surface temperature map that can benefit coral health and monitoring efforts worldwide.
AOML coral scientists participated in a NOAA National Marine Fisheries Service-led project to document coral spawning in the Florida Keys National Marine Sanctuary during August & September 2015. The project aims to measure spawning success for two imperiled Caribbean species, elkhorn coral (Acropora palmata) and mountainous star coral (Orbicella faveolata) in the Florida Keys. The team collected gametes from both species to be used in experiments that aim to improve the understanding of factors that may enhance the likelihood of coral larvae to survive and settle on the ocean floor. Experiments will also assess impacts of current and future global environmental changes, such as ocean acidification, on these vulnerable early life stages of corals. Click on the image below to view a video of a spawning mountainous star colony.
Photo and Video credit: NOAA
Members of AOML’s Acidification, Climate, and Coral Reef Ecosystems Team (ACCRETE) recently traveled to two remote reef locations to expand the National Coral Reef Monitoring Program’s (NCRMP) network of sentinel climate and ocean acidification monitoring sites. The newly established sites, located in the Flower Garden Banks and the Dry Tortugas, will provide researchers with additional data and insights into the ocean’s changing chemistry and the progression of ocean acidification, as well as the ecological impacts of these variables across the Caribbean basin and the Gulf of America.
