
On the morning of June 7th, the JOIDES Resolution threw off its mooring lines and set sail towards the North Sea. With the port of Amsterdam roughly 30km inland, Expedition 403 would begin with panoramic views of the Dutch countryside as it made its way towards the sea. Giant modern windmills towered over the ship as two tugboats led the way to Lock IJmuiden, which is used to control water height in the canals that lead into the densely populated city center. With Amsterdam sitting so far below sea level, the attention given to climate and rising oceans is out of necessity. The lock acting as a gate into the North Sea served as an oddly appropriate beginning for Expedition 403—the drilling destination can be considered a sort of “gate” into the Arctic, and a better understanding of it could have a direct effect on the predictions of rising sea levels.
The Fram Strait is a deep-water passage that connects the Arctic Ocean and the Northern Atlantic. Sitting between Greenland and Svalbard, the exchange of heat, moisture, and salt between the two oceans is a strong forcing mechanism for climate change both regionally and globally. A significant focus for many of the researchers onboard is the modality of decay of a former ice sheet that covered Svalbard and the Barents Sea roughly 21.000 years ago and shared many characteristics with the presently most vulnerable ice sheet on the planet, the Western Antarctic Ice Sheet (WAIS).

The lock slowly filled with water and opened its gates, leaving the tugboats behind and revealing open waters ahead. Still far from the first sampling site, the transit up along the coast of Norway would take seven days, with waves reaching as high as four meters. After onboarding and safety trainings the scientists would take the long transit to break into working groups and prepare for the arrival of samples. As the ship made the voyage further north the sun would hang higher and longer throughout the day. On the third day of transit, the faint glow of dusk would be the closest thing to night the crew would experience over the next two months. During the summer months, at higher latitudes, the sun will just run laps around the boat, never dipping below the horizon line.

The mix of sea ice movement and small window of seismic opportunity (seismic tests are only permitted in June due to vulnerable whale migration patterns in the region) would lead the expedition to settle on the eastern slope of the Vestnesa Ridge as the first sampling site. Exactly one week from departure, the crew would arrive on site. Greeted with a sea as calm as glass, drilling preparation would begin almost immediately. After the long transit the excitement of the science party was palpable in the labs as everyone huddled around the door to the catwalk waiting for the first core on deck. Friday evening at roughly 9:00pm, the first core would begin making its way up the drill pipe. In the last moments Lucinda Duxbury, a microbiologist from the University of Tasmania, had the brilliant idea to play “Ecstasy of the Gold” by Ennio Morricone over the lab’s sound system. In an appropriate pairing, the spaghetti western’s orchestral music played as the first core arrived onto to the catwalk, successful sample retrieved.
After the first core arrived on deck, the stream of samples was continuous. Deemed a high recovery expedition, the total amount of core recovered during Expedition 403 is anticipated to be over 5,000 meters. The flow of samples remained uninterrupted until challenges arrived midweek.

The indications of gas hydrates downhole posed a potential safety risk, and although not an unexpected complication for the region, evidence was showing a higher potential presence than anticipated. With the help of the trade knowledge of the drill crew and technical support staff, who constantly monitored gas safety measurements, operations proceeded with caution, ultimately leading to over one kilometer of core successfully retrieved.
Under the guidance of the onboard ice navigators Victor Gronmyr and Paul Ruzycki, the decision was made to head northwest to our next drill site. Thrusters will be raised shortly, and to the western slope of the Vestnesa ridge the team will go.
Ocean Acidification
All About False Killer Whales
Despite their dramatic name, false killer whales aren’t an orca species. These animals are dolphins—members of the same extended family as the iconic “killer whale” (Orcinus orca). Compared to their namesake counterparts, these marine mammals are far less well-known than our ocean’s iconic orcas.
Let’s dive in and take a closer look at false killer whales—one of the ocean’s most social, yet lesser-known dolphin species.
Appearance and anatomy
False killer whales (Pseudorca crassidens) are among the largest members of the dolphin family (Delphinidae). Adults can grow up to 20 feet long and weigh between 1,500 and 3,000 pounds, though some individuals have been recorded weighing even more. For comparison, that’s roughly double the size of a bottlenose dolphin—and slightly larger than a typical sedan.
These animals are incredibly powerful swimmers with long, torpedo-shaped bodies that help them move efficiently through the open ocean in search of prey. Their skull structure is what earned them their name, as their head shape closely resembles that of orcas. With broad, rounded heads, muscular jaws and large cone-shaped teeth, early scientists were fascinated by the similarities between these two marine mammal species.
Although their heads may look somewhat like those of orcas, there are several ways to distinguish false killer whales from their larger namesake counterparts.
One of the most noticeable differences has to do with their coloration. While orcas are known for their iconic black-and-white pattern with paler underbellies, alternatively, false killer whales are typically a uniform dark gray to black in color—almost as if a small orca decided to roll around in the dirt. If you’ve ever seen the animated Disney classic 101 Dalmatians, the difference is a bit like when the puppies roll in soot to disguise themselves as labradors instead of showing their usual black-and-white spots.
Their teeth also present a differentiator. The scientific name Pseudorca crassidens translates almost literally to “thick-toothed false orca,” a nod to their sturdy, cone-shaped teeth that help these animals capture prey. Orcas tend to have more robust, bulbous heads, while false killer whales appear slightly narrower and more streamlined.

Behavior and diet
False killer whales are both highly efficient hunters and deeply social animals. It’s not unusual to see them hunting together both in small pods and larger groups as they pursue prey like fish and squid.
Scientists have even observed false killer whales sharing food with each other, a behavior that is very unusual for marine mammals. While some dolphin and whale species work together to pursue prey, they rarely actively share food. The sharing of food among false killer whales spotlights the strong social bonds within their pods. Researchers believe these tight-knit social connections help false killer whales thrive in offshore environments where they’re always on the move.
Maintaining these close bonds and coordinating successful hunts requires constant effective communication, and this is where false killer whales excel. Like other dolphins, they produce a variety of sounds like whistles and clicks to stay connected with their pod and locate prey using echolocation. In the deep offshore waters where they live, sound often becomes more important than sight, since sound travels much farther underwater than light.
Where they live
False killer whales are highly migratory and travel long distances throughout tropical and subtropical waters around the world. They prefer deeper waters far offshore, and this pelagic lifestyle can make them more difficult for scientists to study than many coastal dolphin species.
However, there are a few places where researchers have been able to learn more about them—including the waters surrounding the Hawaiian Islands.
Scientists have identified three distinct groups of false killer whales in and around Hawaii, but one well-studied group stays close to the main Hawaiian Islands year-round. Unfortunately, researchers estimate that only about 140 individuals remained in 2022, with populations expected to decline without action to protect them. This is exactly why this group is listed as endangered under the U.S. Endangered Species Act and is considered one of the most vulnerable marine mammal populations in U.S. waters.
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Current threats to survival
False killer whales are currently listed as Near Threatened on the IUCN Red List. From climate change-induced ocean acidification and harmful algal blooms to marine debris and fishing bycatch, false killer whales face the same mounting pressures that are impacting marine ecosystems around the world. As their prey becomes scarce due to increasing threats, populations of top predators like these decline, serving as a powerful signal that the ocean’s overall health is in critical need of protection.
Here at Ocean Conservancy, we’re working daily to confront these threats head-on and protect the ecosystems and wildlife we all cherish so dearly. But we can’t do it without you. Support from ocean lovers is what powers our work to protect our ocean, and right now, our planet needs all the help it can get. Visit Ocean Conservancy’s Action Center today and join our movement to create a better future for our ocean, forever and for everyone.
The post All About False Killer Whales appeared first on Ocean Conservancy.
https://oceanconservancy.org/blog/2026/03/31/false-killer-whales/
Ocean Acidification
It’s been a long time since I posted here!
A lot has happened in the meantime: I became an Associate Professor at the University of Southern Denmark, we all lived through the Corona period, then slowly adjusted to the post‑pandemic stability, only to find ourselves again in turbulent political times. I am now affiliated with the Marine Research Center in Kerteminde, a beautiful coastal town on the island of Fyn. My plan is to share small updates on my research and activities every now and then. So let’s start with yesterday’s sampling trip for benthic phytoplankton, carried out by my colleague, Prof. Kazumasa Oguri. The sampling will help prepare for the first‑semester bachelor students who will join his small but fascinating project. This project is all about the benthic diatoms that form dense, photosynthetic communities on tidal‑flat sediments. Their daytime oxygen production enriches the sediment surface and allows oxygen to penetrate deeper, supporting diverse organisms that rely on aerobic respiration. The project will explore how oxygen distribution and oxygen production/consumption in sediments change under different light conditions (day, night, sunrise/sunset). The team will incubate benthic diatom communities in jars and measure oxygen profiles using an oxygen imaging system under controlled light regimes.
Yesterday, we visited several potential sampling sites where students can carry out their fieldwork. I encourage all PIs in our group to define at least one small project related to Kerteminde Fjord, where our laboratories are located. Over time, I hope we can build a more integrated dataset describing the marine and coastal ecosystems of the area.
Another activity currently in preparation is a project on marine invasive species in Kerteminde, which will feed into a course I will run in July and a master’s thesis project. More will come later.
Let’s hope for a more continuous blog from here on, keeping track of our activities, with or without jellyfish!



Ocean Acidification
What is the High Seas Treaty and Why Does It Matter?
You may have seen headlines recently about a new global treaty that went into effect just as news broke that the United States would be withdrawing from a number of other international agreements. It’s a confusing time in the world of environmental policy, and Ocean Conservancy is here to help make it clearer while, of course, continuing to protect our ocean.
What is the High Seas Treaty?
The “High Seas Treaty,” formally known as the Agreement on the Conservation and Sustainable Use of Marine Biological Diversity of Areas Beyond National Jurisdiction (BBNJ) Agreement, went into effect on January 17, 2026. We celebrated this win last fall, when the agreement reached the 60 ratifications required for its entry into force. (Since then, an additional 23 countries have joined!) It is the first comprehensive international legal framework dedicated to addressing the conservation and sustainable use of the high seas (the area of the ocean that lies 200 miles beyond the shorelines of individual countries).
To “ensure the conservation and sustainable use of marine biological diversity” of these areas, the BBNJ addresses four core pillars of ocean governance:
- Marine genetic resources: The high seas contain genetic resources (genes of plants, animals and microbes) of great value for pharmaceuticals, cosmetics and food production. The treaty will ensure benefits accrued from the development of these resources are shared equitably amongst nations.
- Area-based management tools such as the establishment of marine protected areas (MPAs) in international waters. Protecting important areas of the ocean is essential for healthy and resilient ecosystems and marine biodiversity.
- Environmental impact assessments (EIA) will allow us to better understand the potential impacts of proposed activities that may harm the ocean so that they can be managed appropriately.
- Capacity-building and the transfer of marine technology with particular emphasis on supporting developing states. This section of the treaty is designed to ensure all nations benefit from the conservation and sustainable use of marine biodiversity through, for example, the sharing of scientific information.
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Why is the High Seas Treaty Important?
The BBNJ agreement is legally binding for the countries that have ratified it and is the culmination of nearly two decades of negotiations. Its enactment is a historic milestone for global ocean governance and a significant advancement in the collective protection of marine ecosystems.
The high seas represent about two-thirds of the global ocean, and yet less than 10% of this area is currently protected. This has meant that the high seas have been vulnerable to unregulated or illegal fishing activities and unregulated waste disposal. Recognizing a major governance gap for nearly half of the planet, the agreement puts in place a legal framework to conserve biodiversity.

As it promotes strengthened international cooperation and accountability, the agreement will establish safeguards aimed at preventing and reversing ocean degradation and promoting ecosystem restoration. Furthermore, it will mobilize the international community to develop new legal, scientific, financial and compliance mechanisms, while reinforcing coordination among existing treaties, institutions and organizations to address long-standing governance gaps.
How is Ocean Conservancy Supporting the BBNJ Agreement?
Addressing the global biodiversity crisis is a key focal area for Ocean Conservancy, and the BBNJ agreement adds important new tools to the marine conservation toolbox and a global commitment to better protect the ocean.
Ocean Conservancy’s efforts to protect the “ocean twilight zone”—an area of the ocean 200-1000m (600-3000 ft) below the surface—is a good example of why the BBNJ agreement is so important. The ocean twilight zone (also known as the mesopelagic zone) harbors incredible marine biodiversity, regulates the climate and supports the health of ocean ecosystems. By some estimates, more than 90% of the fish biomass in the ocean resides in the ocean twilight zone, attracting the interest of those eager to develop new sources of protein for use in aquaculture feed and pet foods.

Done poorly, such development could have major ramifications for the health of our planet, jeopardizing the critical role these species play in regulating the planet’s climate and sustaining commercially and ecologically significant marine species. Species such as tunas (the world’s most valuable fishery), swordfish, salmon, sharks and whales depend upon mesopelagic species as a source of food. Mesopelagic organisms would also be vulnerable to other proposed activities including deep-sea mining.
A significant portion of the ocean twilight zone is in the high seas, and science and policy experts have identified key gaps in ocean governance that make this area particularly vulnerable to future exploitation. The BBNJ agreement’s provisions to assess the impacts of new activities on the high seas before exploitation begins (via EIAs) as well as the ability to proactively protect this area can help ensure the important services the ocean twilight zone provides to our planet continue well into the future.
What’s Next?
Notably, the United States has not ratified the treaty, and, in fact, just a few days before it went into effect, the United States announced its withdrawal from several important international forums, including many focused on the environment. While we at Ocean Conservancy were disappointed by this announcement, there is no doubt that the work will continue.
With the agreement now in force, the first Conference of the Parties (COP1), also referred to as the BBNJ COP, will convene within the next year and will play a critical role in finalizing implementation, compliance and operational details under the agreement. Ocean Conservancy will work with partners to ensure implementation of the agreement is up to the challenge of the global biodiversity crisis.
The post What is the High Seas Treaty and Why Does It Matter? appeared first on Ocean Conservancy.
https://oceanconservancy.org/blog/2026/02/25/high-seas-treaty/
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