The Oceanic Flux Program (OFP), one of the world’s longest-running time-series, has received continued funding to help the oceanographic community answer ongoing questions about the connections between climate and the particle debris that sinks through the ocean’s water column. This process, called the particle flux, is a major control on the global carbon cycle and provides the fuel to support most biological processes operating within the ocean’s deep interior.

Nine Bermuda College students participated in lectures, hands-on laboratory activities, and a plankton-collecting trip during a two-day climate change workshop earlier this month through a partnership between BIOS’s Ocean Academy and the United States Consulate General in Bermuda.

Since 2013, BIOS has hosted marine planning coordinator Kevin Mayall, who has assisted the Government of Bermuda with its investigation of marine planning policy options. The approach is the first of its kind for the island, and involves a multi-year process of working collaboratively with government departments, ocean stakeholders, local and overseas scientists, commercial interests, conservation groups, and the general public to look at ways to create a plan for maintaining a healthy and productive relationship between Bermuda and the marine environment.

Chloe Emerson initially came to BIOS in the fall of 2014 for the Research Experiences for Undergraduates (REU) internship program funded by the National Science Foundation.  As a Wellesley College senior working to complete her major in Biology and minor in Philosophy, Emerson already found developmental biology and stem cell research fascinating. At BIOS, these interests crystalized as she began to study sea urchins in Andrea Bodnar’s Molecular Discovery Laboratory, leading her down a path in regenerative biology that she hardly could have imagined two years ago.

In 1989, BIOS was still known as the Bermuda Biological Station for Research and its logo was an angelfish surrounded by a concentric ring of nautical rope. Back then, the Institute’s research vessel was Weatherbird II, acquired that year to support the increased use associated with the open-ocean research and equipment testing for which BIOS became known. And when biologist and educator Dr. Edward F. MacNichol, Jr. made a generous gift in memory of his parents, the MacNichol Fund was established, allowing the Institute to recruit talented young scientists to establish their own independent research programs. The first hire was Fred Lipschultz, then a postdoctoral student and biological oceanographer from Harvard University, who arrived in September 1989.

Perched near the shoreline on the southwest coast of Bermuda, the Tudor Hill Marine Atmospheric Observatory is one of BIOS’s lesser-known gems, and the source for data used in two scientific papers published last year in leading scientific journals. The publications – Atmospheric Chemistry and Physics and the Journal of Geophysical Research: Atmospheres – feature collaborations among multiple researchers in the U.S., Germany, and Bermuda, including BIOS environmental chemist and Tudor Hill observatory lead scientist Andrew Peters.

Not many people willingly sign up for a multi-week research cruise in freezing temperatures where fresh produce typically runs out after the second week at sea. But BIOS research specialist Becky Garley is excited at the prospect of returning to the Arctic for the third time next September 2022 as part of the Synoptic Arctic Survey (SAS).

When scientists study coral reefs, they are often interested in figuring out key components of reef health; specifically, primary production—or photosynthesis—and calcification, the rate at which new reef growth occurs. For decades this has meant time and labor-intensive fieldwork, with scientists documenting global reef condition and linking what they see underwater with lab-based experiments and measurements.

Five years of data collected on reefs and offshore in Bermuda shows that coral reef chemistry – and perhaps the future success of corals – is tied not only to the human carbon emissions causing systematic ocean acidification, but also to seasonal and decadal cycles in the open waters of the Atlantic, and the balance of biochemical processes in the coral reef community.

Elevated ocean temperatures have threatened coral reefs around the world for over a year, but this October marked a tipping point.  NOAA scientists declared the onset of a global coral reef bleaching event impacting coral reefs in every ocean basin, and projected the bleaching will only intensify in 2016. This is the third such global bleaching event in history.