A new study found that when red tides began in early summer and continued into the fall, low oxygen areas—or dead zones— were more likely to also occur. T
A new study found that when red tides began in early summer and continued into the fall, low oxygen areas—or dead zones— were more likely to also occur. This study by scientists at the University of Miami Rosenstiel School of Marine and Atmospheric Science, and NOAA collaborators is the first study to link low oxygen—or hypoxia—to red tides across the west coast of Florida and offers new information to better understand the conditions favorable for combined events as they are expected to increase as Earth continues to warm.
Red tides are becoming a near annual occurrence off the west coast of Florida, which are caused by massive blooms of the algae Karenia brevis fueled in part by excess nutrients in the ocean. These algae blooms turn the ocean surface red and produce toxins that are harmful to marine mammals, sharks, seabirds and humans causing a range of issues from respiratory irritation, localized fish kills to large-scale massive mortalities to marine life. Hypoxic areas are typically referred to as ‘dead zones’.
“These events are so disruptive they are being incorporated in population assessments of some grouper species for use in fishery management decisions. During the 2005 red tide that also had hypoxia, it was estimated that about 30% of the red grouper population was killed,” said Brendan Turley, an assistant scientist at the UM Rosenstiel School and NOAA’s Cooperative Institute of Marine and Atmospheric Studies. “There are also concerns that the conditions favorable for combined red tide and hypoxia events will increase with climate change projections into the future.”
Read more at: University of Miami
Red tides are becoming a near annual occurrence off the west coast of Florida, which are caused by massive blooms of the algae Karenia brevis fueled in part by excess nutrients in the ocean. (Photo Credit: P. Schmidt, Charlotte Sun)
