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by Dr. Birgit Quack, GEOMAR Helmholtz Centre for Ocean Research Kiel

There are two regions of our atmosphere where the trace gas ozone is especially important: in the stratosphere and in the surface boundary layer. In the upper region of our atmosphere, the stratosphere ozone is produced from the sunlit decay of oxygen and acts as an important UV radiation protector for life on earth. It is rapidly destroyed by radical reactions of halogens, such as chlorine, bromine, and iodine, which occur in various forms in our atmosphere. A severe ozone hole occurred in the 1980s and could be related to long-lived fluorochlorocarbons, which were banned by the Montreal Protocol in the 1990s. Because of this, the ozone hole over Antarctica is closing and ozone in the upper stratosphere is generally increasing again. However, in the lower stratosphere of the tropics, it is still declining. Surface ozone, on the other hand, is increasing due to air pollution, especially when fossil fuel is combusted.

Surface ozone on Sunday, 12th of May, at 2 pm local time (7 am UTC). (Photo from windy.com)

Under windy.com, anyone who has internet access can find a global map for ozone and local values for every place in the world (Figure 1). Surface ozone, which is also a greenhouse gas, is produced naturally to a background of 10-40 µg/m3. As it is a strong oxidant, it can irritate eyes and lungs in higher concentrations. Therefore, legal thresholds and warning systems are established for cities where ambient concentrations increase in summer >100µg/m3 and can harm sensitive people.

Figure 1 shows the ozone surface ozone concentrations in the area where our cruise SO305 operated in the Bay of Bengal. It is very high over the entire India during the day, and it is also apparent that the ozone concentrations sharply decline at the coastlines and towards the open oceans. This is mainly due to an active halogen chemistry, which destroys ozone over the oceans, caused by natural halogenated volatile compounds. They are formed in the oceans by sunlight, phytoplankton, and chemical reactions and are partly released into the atmosphere. Those compounds comprise bromoform (CHBr3), dibromo¬methane (CH2Br2), methyl iodide (CH3I), diiodomethane (CH2I2) iodochloromethane (CH2CII), dichlorobromomethane (CHBrCl2) and all have short atmospheric lifetimes of minutes to six months. The anthropogenic industrial solvent dichloromethane (CH2Cl2) and chloroform (CHCl3) from freshwater chlorination are also short-lived and contribute to ozone depletion in the atmosphere as well. The compounds lifted up into the stratosphere by deep convection in the tropics release their halogens in the lower stratosphere while moving to the North and South poles. Thus, the tropical processes exert their effects globally.
During the last month, we were on board RV Sonne in the tropical Bay of Bengal, discovered in 2001 as a major source of some natural halogenated volatile compounds to the atmosphere. We measured the compounds in water on board, with a Gas-chromatographic Mass-spectrometric (GC/MS) Purge-system (Figure 2), in order to understand their source strengths and learn about their biogeochemical cycling in the oxygen minimum zone of the Bay of Bengal.

Gas-chromatographic Mass-spectrometric (GC/MS) Purge-system for measuring halogenated compounds in ocean and atmosphere. Jule Ploschke, Julia Mickenbecker, and Birgit Quack with water and air-sampling devices (Photo by: Hendrik Feil).

Jule, doing her master thesis on the topic, Julia, joining R/V Sonne for the second time as a student helper, and I, traveling the oceans for 30 years for halocarbons, brought our analytical system on board, which ran smoothly since the beginning of the cruise 24/7 in shifts of each 8 hours, where the instrument gets a new sample every hour. We have taken water from the deep ocean and the surface waters in brown glass bottles and pumped air into stainless steel canisters (Figure 3). The gases in the water samples were extracted with helium, frozen in liquid nitrogen, separated on a gas-chromatographic column, and detected with a Mass-spectrometer. The air samples will be analysed using a similar method for approximately 50 compounds by Elliot Atlas at the National Center for Atmospheric Research in Boulder, Colorado, US. From the concentrations in the ocean and atmosphere, we calculate the air-sea gas exchange of the compounds, try to understand their distribution in the region related to physical and biogeochemical parameters, and estimate how the oceanic source and sink may develop in the future and what this means for ozone as a greenhouse gas and as UV-shield.

The last air sample during SO305 (Photo by: Hermann Bange).

During every ship expedition in my 30 years of travelling the oceans, a team of scientists and crew on board different research vessels explored the ocean as an ancient interplay of water, chemicals, trillions of bacteria, and higher organisms, influenced by gravity, the rotation of the earth as well as by sunlight and the moon. The biota responds to the distribution of nutritious chemicals, while the waters interact closely with the atmosphere, from the sea surface to the stratosphere. Every time, a bit of the myriad of global and regional secret interactions, which determine the basis of our life, was discovered and published. The old interplay is now influenced by human activities, which I hope do not tip the evolving equilibrium so that future generations have the chance to further unravel it to sustainably live with it.

I was able to conduct my last cruise on RV Sonne, a starship of the German research fleet, with a professional crew, which enabled again very good data sets, by the smooth operation of the ship until Singapore harbour. During the next years, I will likely mainly explore my 30-year data sets with AI for the benefit of extracting the most knowledge about halocarbons out of them. Jule and Julia will hopefully find more opportunities to conduct their career with ocean voyages of discovery, as those not only promote knowledge, but also evolve social skills of team effort, discipline, endurance, considerateness and tolerance. I will miss the daily challenges of a successful research cruise.

Birgit Quack, Singapore 18.05.2024

Hallo halos in and over the Bay of Bengal

Ocean Acidification

What is Coral Bleaching and Why is it Bad News for Coral Reefs?

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Coral reefs are beautiful, vibrant ecosystems and a cornerstone of a healthy ocean. Often called the “rainforests of the sea,” they support an extraordinary diversity of marine life from fish and crustaceans to mollusks, sea turtles and more. Although reefs cover less than 1% of the ocean floor, they provide critical habitat for roughly 25% of all ocean species.

Coral reefs are also essential to human wellbeing. These structures reduce the force of waves before they reach shore, providing communities with vital protection from extreme weather such as hurricanes and cyclones. It is estimated that reefs safeguard hundreds of millions of people in more than 100 countries. 

What is coral bleaching?

A key component of coral reefs are coral polyps—tiny soft bodied animals related to jellyfish and anemones. What we think of as coral reefs are actually colonies of hundreds to thousands of individual polyps. In hard corals, these tiny animals produce a rigid skeleton made of calcium carbonate (CaCO3). The calcium carbonate provides a hard outer structure that protects the soft parts of the coral. These hard corals are the primary building blocks of coral reefs, unlike their soft coral relatives that don’t secrete any calcium carbonate.

Coral reefs get their bright colors from tiny algae called zooxanthellae. The coral polyps themselves are transparent, and they depend on zooxanthellae for food. In return, the coral polyp provides the zooxanethellae with shelter and protection, a symbiotic relationship that keeps the greater reefs healthy and thriving.

When corals experience stress, like pollution and ocean warming, they can expel their zooxanthellae. Without the zooxanthellae, corals lose their color and turn white, a process known as coral bleaching. If bleaching continues for too long, the coral reef can starve and die.


Ocean warming and coral bleaching

Human-driven stressors, especially ocean warming, threaten the long-term survival of coral reefs. An alarming 77% of the world’s reef areas are already affected by bleaching-level heat stress.

The Great Barrier Reef is a stark example of the catastrophic impacts of coral bleaching. The Great Barrier Reef is made up of 3,000 reefs and is home to thousands of species of marine life. In 2025, the Great Barrier Reef experienced its sixth mass bleaching since 2016. It should also be noted that coral bleaching events are a new thing because of ocean warming, with the first documented in 1998.

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How you can help

The planet is changing rapidly, and the stakes have never been higher. The ocean has absorbed roughly 90% of the excess heat caused by anthropogenic greenhouse gas emissions, and the consequences, including coral die-offs, are already visible. With just 2℃ of planetary warming, global coral reef losses are estimated to be up to 99% — and without significant change, the world is on track for 2.8°C of warming by century’s end.

To stop coral bleaching, we need to address the climate crisis head on. A recent study from Scripps Institution of Oceanography was the first of its kind to include damage to ocean ecosystems into the economic cost of climate change – resulting in nearly a doubling in the social cost of carbon. This is the first time the ocean was considered in terms of economic harm caused by greenhouse gas emissions, despite the widespread degradation to ocean ecosystems like coral reefs and the millions of people impacted globally.

This is why Ocean Conservancy advocates for phasing out harmful offshore oil and gas and transitioning to clean ocean energy. In this endeavor, Ocean Conservancy also leads international efforts to eliminate emissions from the global shipping industry—responsible for roughly 1 billion tons of carbon dioxide every year.

But we cannot do this work without your help. We need leaders at every level to recognize that the ocean must be part of the solution to the climate crisis. Reach out to your elected officials and demand ocean-climate action now.

The post What is Coral Bleaching and Why is it Bad News for Coral Reefs? appeared first on Ocean Conservancy.

What is Coral Bleaching and Why is it Bad News for Coral Reefs?

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Ocean Acidification

What is a Snipe Eel?

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From the chilly corners of the polar seas to the warm waters of the tropics, our ocean is bursting with spectacular creatures. This abundance of biodiversity can be seen throughout every depth of the sea: Wildlife at every ocean zone have developed adaptations to thrive in their unique environments, and in the deep sea, these adaptations are truly fascinating.

Enter: the snipe eel.

What Does a Snipe Eel Look Like?

These deep-sea eels have a unique appearance. Snipe eels have long, slim bodies like other eels, but boast the distinction of having 700 vertebrae—the most of any animal on Earth. While this is quite a stunning feature, their heads set them apart in even more dramatic fashion. Their elongated, beak-like snouts earned them their namesake, strongly resembling that of a snipe (a type of wading shorebird). For similar reasons, these eels are also sometimes called deep-sea ducks or thread fish.

Close up of a snipe eel profile in turbid water

How Many Species of Snipe Eel are There?

There are nine documented species of snipe eels currently known to science, with the slender snipe eel (Nemichthys scolopaceus) being the most studied. They are most commonly found 1,000 to 2,000 feet beneath the surface in tropical to temperate areas around the world, but sightings of the species have been documented at depths exceeding 14,000 feet (that’s more than two miles underwater)!

How Do Snipe Eels Hunt and Eat?

A snipe eel’s anatomy enables them to be highly efficient predators. While their exact feeding mechanisms aren’t fully understood, it’s thought that they wiggle through the water while slinging their beak-like heads back and forth with their mouths wide open, catching prey from within the water column (usually small invertebrates like shrimp) on their hook-shaped teeth.

How Can Snipe Eels Thrive So Well in Dark Depths of the Sea?

Snipe eels’ jaws aren’t the only adaptation that allows them to thrive in the deep, either. They also have notably large eyes designed to help them see nearby prey or escape potential predators as efficiently as possible. Their bodies are also pigmented a dark grey to brown color, a coloring that helps them stay stealthy and blend into dark, dim waters. Juveniles are even harder to spot than adults; like other eel species, young snipe eels begin their lives as see-through and flat, keeping them more easily hidden from predators as they mature.

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How Much Do Scientists Really Know About Snipe Eels?

Residence in the deep sea makes for a fascinating appearance, but it also makes studying animals like snipe eels challenging. Scientists are still learning much about the biology of these eels, including specifics about their breeding behaviors. While we know snipe eels are broadcast spawners (females release eggs into the water columns at the same time as males release sperm) and they are thought to only spawn once, researchers are still working to understand if they spawn in groups or pairs. Beyond reproduction, there’s much that science has yet to learn about these eels.

Are Snipe Eels Endangered?

While the slender snipe eel is currently classified as “Least Concern” on the International Union for the Conservation of Nature’s Red List of Threatened Species, what isn’t currently known is whether worldwide populations are growing or decreasing. And in order to know how to best protect these peculiar yet equally precious creatures, it’s essential we continue to study them while simultaneously working to protect the deep-sea ecosystems they depend on.

How Can We Help Protect Deep-Sea Species Like Snipe Eels?

One thing we can do to protect the deep sea and the wildlife that thrive within it is to advocate against deep-sea mining and the dangers that accompany it. This type of mining extracts mineral deposits from the ocean floor and has the potential to result in disastrous environmental consequences. Take action with Ocean Conservancy today and urge your congressional representative to act to stop deep-sea mining—animals like snipe eels and all the amazing creatures of the deep are counting on us to act before it’s too late.

The post What is a Snipe Eel? appeared first on Ocean Conservancy.

What is a Snipe Eel?

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Ocean Acidification

5 Animals That Need Sea Ice to Thrive

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Today, we’re getting in the winter spirit by spotlighting five remarkable marine animals that depend on cold and icy environments to thrive.

1. Narwhals

Narwhals are often called the “unicorns of the sea” because of their long, spiraled tusk. Here are a few more fascinating facts about them:

  • Believe it or not, their tusk is actually a tooth used for sensing their environment and sometimes for sparring.
  • Narwhals are whales. While many whale species migrate south in the winter, narwhals spend their entire lives in the frigid waters of the circumpolar Arctic near Canada, Greenland and Russia.
  • Sea ice provides narwhals with protection as they travel through unfamiliar waters.

2. Walruses

Walruses are another beloved Arctic species with remarkable adaptations for surviving the cold:

  • Walruses stay warm with a thick layer of blubber that insulates their bodies from icy air and water.
  • Walruses can slow their heart rate to conserve energy and withstand freezing temperatures both in and out of the water.
  • Walruses use sea ice to rest between foraging dives. It also provides a vital and safe platform for mothers to nurse and care for their young.

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3. Polar Bears

Polar bears possess several unique traits that help them thrive in the icy Arctic:

4. Penguins

Penguins are highly adapted swimmers that thrive in icy waters, but they are not Arctic animals:

  • Penguins live exclusively in the Southern Hemisphere, mainly Antarctica, meaning they do not share the frigid northern waters with narwhals, walruses and polar bears.
  • Penguins spend up to 75% of their lives in the water and are built for efficient aquatic movement.
  • Sea ice provides a stable platform for nesting and incubation, particularly for species like the Emperor penguin, which relies on sea ice remaining intact until chicks are old enough to fledge.

5. Seals

Seals are a diverse group of carnivorous marine mammals found in both polar regions:

  • There are 33 seal species worldwide, with some living in the Arctic and others in the Antarctic.
  • There are two groups of seals: Phocidae (true seals) and Otariidae (sea lions and fur seals). The easiest way to tell seals and sea lions apart is by their ears: true seals have ear holes with no external flaps, while sea lions and fur seals have small external ear flaps.
  • Seals need sea ice for critical life functions including pupping, nursing and resting. They also use ice for molting—a process in which they shed their fur in the late spring or early summer.

Defend the Central Arctic Ocean Action

Some of these cold-loving animals call the North Pole home, while others thrive in the polar south. No matter where they live, these marine marvels rely on sea ice for food, safety, movement and survival.

Unfortunately, a rapidly changing climate is putting critical polar ecosystems, like the Central Arctic Ocean, at risk. That is why Ocean Conservancy is fighting to protect the Central Arctic Ocean from threats like carbon shipping emissions, deep-sea mining and more. Take action now to help us defend the Central Arctic Ocean.

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The post 5 Animals That Need Sea Ice to Thrive appeared first on Ocean Conservancy.

5 Animals That Need Sea Ice to Thrive

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