English version below
Die letzte Woche unserer Expedition ist angebrochen und wir haben die Labradorsee in Richtung Osten verlassen. Die verbleibenden Tage werden wir mit Messungen der CTD-Rosette verbringen. Sie besteht aus einem Kranz von Flaschen, mit denen wir Wasserproben nehmen können und zusätzlichen Messgeräten, die darunter angebracht sind. Die eigentliche CTD (die Abkürzung steht für: Conductivity = Leitfähigkeit, Temperature = Temperatur, Depth = Tiefe) ist ein Messgerät an der Unterseite der Rosette. Zusätzlich gibt es noch eine kleine Kamera, die Bilder aufnehmen kann und ein Messgerät, das Fluoreszenz misst. An bestimmten Positionen müssen wir dann das Schiff anhalten und lassen die Rosette an einem Kabel bis zum Boden hinab. Bei Wassertiefen, die teilweise über 3000m betragen, kann es bis zu 2 Stunden dauern, bis die CTD-Rosette nach unten und wieder nach oben gefahren ist.
Die geplanten CTD-Stationen sollten uns Stück für Stück Richtung Grönländischer Küste führen. Die küstennahen Messungen sind dabei besonders interessant, um ähnlich wie in der Labradorsee den tiefen Randstrom zu untersuchen. Doch bei diesem Plan machte uns das Eis einen Strich durch die Rechnung. Auf der einen Seite freuten wir uns über die Schönheit der zahlreichen Eisschollen um uns herum, auf der anderen Seite verhinderten sie leider auch unser Vorankommen zu den küstennahen CTD-Stationen.

Aus dem Film Titanic haben wir alle gelernt: So ein Eisberg kann zum fatalen Problem für ein Schiff werden. Aber ist das eigentlich noch aktuell? Laut Kapitän Björn Maaß, können Eisberge heutzutage durchaus noch Schiffe versenken. Wir haben allerdings einen Vorteil, gegenüber der Titanic: das Radar, auf dem man Eisberge sehr gut erkennen kann. Nicht so gut erkennbar sind allerdings die von Eisbergen abgebrochene kleinere Eisstücke, Growler genannt. Growler (wortwörtlich übersetzt Brummer) sind nach dem Geräusch benannt, das sie beim Aus- und Abtauchen in der See verursachen. Teilweise sind sie schon mehrere Jahre unterwegs, weshalb sie häufig aus härterem Eis bestehen und nicht so weit aus dem Wasser schauen, da sie schon rundgewaschen sind. Um auch die Growler im Blick zu behalten, ist es deshalb wichtig zusätzlich zur Radarbeobachtung auch aus dem Fenster zu schauen, um alles im Blick zu behalten.
Damit kommen wir zu dem Problem, das unsere CTD-Messungen verhinderte. Es ist nämlich nicht nur das Eis, sondern die Kombination aus Eis und schlechten Sichtverhältnissen, die zur Gefahr wird. Zu Beginn der Stationsarbeit hatten wir Nebel aber nur wenig Eis. Später klarte es auf und das Eis wurde mehr. Solange die Sicht gut ist, sind bis zu 70-80% Bedeckung der Wasseroberfläche mit Eis noch in Ordnung, so der Kapitän. Doch der erneut aufziehende Nebel verringerte die Sicht drastisch. Solange die CTD-Rosette im Wasser ist, ist das Schiff in der Manövrierfähigkeit eingeschränkt und könnte damit einem auf das Schiff zutreibenden Eisberg schlecht ausweichen. Selbst nah am Schiff vorbei treibende Eisberge können zur Gefahr werden. Wie allgemein bekannt, befindet sich der Großteil eines Eisberges unter Wasser. Durch Abtauen des Eises kann es zur Verlagerung der Gewichtsverteilung und damit zum Drehen oder Kippen des Eisberges führen. Sollte das in der Nähe des Schiffes passieren, kann es zu einer Kollision kommen.

Vielleicht fragt sich an diesem Punkt der ein oder andere: ist die Maria S. Merian nicht ein Eisbrecher? Wieso ist das Eis dann überhaupt ein Problem? In der Nord- und Ostsee, wo man es nur mit einjährigem Eis zu tun hat, kann sie tatsächlich bis zu 80cm Eis brechen. In dem Gebiet, in dem wir uns jetzt befinden, kann es aber durchaus sein, dass sich eingeschlossen im einjährigen Eis auch ältere Stücke befinden. Diese haben bereits einen oder mehrere Sommer überstanden und sind dadurch schon mehr verdichtet und damit härter. Versucht man dieses dann zu brechen, kann das Schiff beschädigt werden. Das führte mutmaßlich zum Untergang des Kreuzfahrtschiff Explorer 2007 in der Antarktis. Die Besatzung des Schiffes war auf der Nord- und Ostsee ausgebildet und damit nur im Umgang mit einjährigem Eis geschult.
Fassen wir also kurz zusammen: Eisberge sind auch heutzutage noch eine Gefahr für die Seefahrt. Dank Radar kann man das Eis zwar sehr gut beobachten, doch die Sichtverhältnisse sollten trotzdem möglichst gut sein, wenn man sich in einem Eisfeld befindet. Außerdem ist nicht jedes Eis gleich und muss auf Grund des Alters, der Form und der Größe differenziert betrachtet werden.

Bleibt nur noch die Frage, was passieren würde, sollte unser Schiff die Maria S. Merian doch einmal mit einem Eisberg zusammenstoßen. Das kann auch der Kapitän nicht so leicht beantworten. Zuerst einmal ist die Geschwindigkeit des Schiffes ein wichtiger Faktor. Bei einer Kollision mit 2 Knoten Fahrt, würden die Eisstücke höchstwahrscheinlich nur zur Seite geschoben werden, während ein Zusammenstoß bei 10 Knoten Geschwindigkeit gefährlicher wäre. Außerdem hängen die Auswirkungen eines Zusammenstoßes noch von einigen weiteren Kriterien ab, zum Beispiel wie groß der Schaden ist und wo sich das Loch befindet. Da das Schiff in mehrere Sektionen unterteilt ist, die sie sich wasserdicht voneinander abschotten lassen, kommt es darauf an wie viele und welche Abteilungen volllaufen. Solange nicht Maschinenraum und Windenraum oder nur zwei Sektionen geflutet werden, bleibt die Maria S. Merian schwimmfähig. Für uns bleibt das eine hypothetische Überlegung. Am Ende hatten wir einen atemberaubenden Ausblick, der uns über die verpassten CTD-Stationen hinweggetröstet hat und wurden von der Brücke sicher wieder aus dem Eis herausmanövriert.
The downside of icebergs
The last week of our expedition has dawned and we have left the Labrador Sea towards the east. The remaining days will be spent with measurements of the CTD rosette. It consists of a wreath of bottles with which we can take water samples and additional measuring instruments attached underneath. The actual CTD (abbreviation stands for Conductivity, Temperature, Depth) is a measuring device on the underside of the rosette. In addition, there is a small camera that can take pictures and a meter that measures fluorescence. At certain locations we then have to stop the ship and drop the rosette on a cable down to the ground. At water depths, some of which are over 3000m, it can take up to 2 hours for the CTD rosette to go down and back up.
The planned CTD stations should lead us step by step towards the Greenland coast. The measurements near the shore are particularly interesting to study the deep margin current, as in the Labrador Sea. But with this plan, the ice broke our hearts. On the one hand we enjoyed the beauty of the numerous ice floes around us, on the other hand they unfortunately prevented our progress to the coastal CTD stations.

We all learned from the movie Titanic: an iceberg like this can become a fatal problem for a ship. But is this really still relevant? According to Captain Bjorn Maas, icebergs can still sink ships today. However, we have one advantage over the Titanic: the radar, on which you can see icebergs very well. However, smaller pieces of ice broken off by icebergs, called growlers, are not so well visible. Growlers are named for the noise they make when they go out and dive in the sea. Some of them have been floating around for several years, which is why they often consist of harder ice and do not look as far out of the water as they have already washed around. In order to keep an eye on the growlers, it is therefore important to look out the window in addition to radar observation to keep an eye on everything.
This brings us to the problem that prevented our CTD measurements. It is not just the ice, but the combination of ice and poor visibility that becomes the danger. At the beginning of the station work we had fog but only a little ice. Later, it cleared up and the ice became bigger. As long as visibility is good, up to 70-80% coverage of the water surface with ice is still fine, according to the captain. But the re-emerging fog drastically reduced visibility. As long as the CTD rosette is in the water, the ship is limited in maneuverability and could thus badly dodge an iceberg drifting towards the ship. Even icebergs drifting close to the ship can become a hazard. As is common knowledge, most of an iceberg is underwater. By thawing the ice, it can shift the weight distribution and thus turn or tip the iceberg. If this happens close to the ship, there may be a collision.

At this point, some may wonder: isn’t the Maria S. Merian an icebreaker? Why is ice a problem? In the North and Baltic Seas, where you only have to deal with one year old ice, it can actually break up to 80cm of ice. In the area in which we are now, however, it may well be that there are older pieces trapped in the one-year ice. These have already survived one or more summers and are therefore already more compacted and thus harder. If you try to break it, the ship can be damaged. This led to the sinking of the cruise ship Explorer in Antarctica in 2007. The crew of the ship was trained in the North and Baltic Seas and thus trained only in handling one year’s worth of ice.
So let’s summarize briefly: icebergs are still a danger to shipping today. Thanks to radar you can observe the ice very well, but the visibility should still be as good as possible when you are in an ice field. In addition, not all ice cream is the same and needs to be considered differentiated based on age, shape and size.

The only question left is what would happen if our ship, the Maria S. Merian, collided with an iceberg. The captain can’t answer that easily. First of all, the speed of the ship is an important factor. In a collision at 2 knots, the pieces of ice would most likely only be pushed aside, while a collision at 10 knots speed would be more dangerous. In addition, the impact of a collision depends on a number of other criteria, such as the size of the damage and where the hole is located. Since the ship is divided into several sections, they are sealed off watertight from each other, it depends on how many and which sections are full. As long as engine room and windroom are not flooded or only two sections are flooded, the Maria S. Merian will remain floating. For us, this remains a hypothetical consideration. In the end, we had a breathtaking view that consoled us over the missed CTD stations and were safely maneuvered out of the ice again from the bridge.
Ocean Acidification
The jellyfish we see are only half the story
When moon jellyfish gather in large numbers, the bloom is impossible to ignore. Hundreds or thousands of medusae can suddenly fill a bay or fjord. Because this swimming stage is so visible, it is often the focus of monitoring and research. But the familiar jellyfish is only one chapter in a much more complex life cycle. Before entering the open water, moon jellyfish can spend years as tiny polyps attached to rocks, algae or other hard surfaces on the seafloor. These polyps reproduce asexually and release young jellyfish when conditions are suitable. Our new study in Trondheimsfjorden, Norway, shows why this hidden stage deserves much more attention. The central finding is that the stage that moves the least may be the stage that gives a jellyfish population its greatest stability.
Image courtesy: https://sciencedigest.org/facts-about-jellyfish/
One animal two worlds
Moon jellyfish (Aurelia aurita) alternate between two contrasting habitats. Polyps remain attached to the seabed and can persist locally for years. Medusae live in the water column for a much shorter time and can be transported by currents across the fjord.
This creates an ecological puzzle. If medusae can travel widely, should populations throughout a fjord become genetically well mixed? Or can local structure survive because the stationary polyp stage retains diversity in particular places? Our new study in Trondheimsfjorden, Norway, shows that these hidden polyps may be crucial for maintaining genetic diversity. We combined field observations, genetic analyses of 572 samples and a model of movement through fjord currents. We found 70 genetic variants—and a striking difference between life stages.Polyps consistently held high genetic diversity. Medusae varied much more between places and years and were sometimes dominated by only a few variants. The polyps therefore appear to act like a biological seed bank: many possibilities remain stored out of sight, while each year’s conditions determine which ones emerge.

Currents alone could not explain the genetic patterns: the model predicted more mixing than was observed among medusae. Transport is therefore only part of the story. Local retention, temperature, food, survival and reproductive timing can filter which variants reach the visible stage.
This matters because jellyfish blooms affect food webs, fisheries, tourism and coastal infrastructure. Better forecasts will require more than counting medusae or following currents. We must also monitor polyp habitats and understand what controls transitions between life stages.
The wider lesson is simple: to understand the connectivity and resilience of marine organisms, we cannot study only the most visible, or most mobile part of their lives.
Paper: Majaneva, S., Ellingsen, I., Javidpour, J. and Aberle, N. (2026). Benthic life stages retain fjord-scale population structure despite pelagic dispersal. Frontiers in Marine Science, 13:1895768. https://doi.org/10.3389/fmars.2026.1895768
Ocean Acidification
What are Tire Wear Particles?
What do you think about when you hear the words “microplastic pollution?” Your mind may immediately go to imagery of colorful fragmented plastics broken off from bottles, buckets and other items we use in our everyday lives. Or, perhaps, you imagine a pile of microplastic fibers—the tiny, squiggly, spaghetti-shaped plastics that shed from our synthetic clothing. You may be surprised to hear there is another major source of microplastic pollution that’s hiding in plain sight, quite literally under our feet, that might change how you think about microplastics: tire particles.
We all know tires wear down over time—that’s why we have to replace them on our cars roughly every 60,000 miles or so. Every time a vehicle accelerates, brakes or simply drives down the road, the friction between its tires and the pavement creates tiny fragments of rubber, known as tire wear particles.
Driving a car or even riding in a bus is a bit like dragging an eraser across the planet, except the crumbs are microplastics. Toxic microplastics.
Tires are made from a complex mix of natural and synthetic rubber along with a range of additives, fillers and chemical compounds—some of which, like the preservative 6PPD, have been shown to be highly toxic to coho salmon when they break down into derivative product 6PPD-Q in the environment—even in tiny concentrations.
Some studies have shown that a single vehicle’s tires can emit more than two trillion particles per mile driven—and that the average person generates nearly two pounds of tire particles per year! Once these particles are shed from tires, they don’t just disappear. Some are small and light enough to become airborne, drifting away from roadways as dust. Others settle on road surfaces, where they accumulate until the next heavy rain washes them into storm drains and from there, into streams, rivers and eventually the ocean.
That’s why tire wear particles are now considered one of the top sources of microplastics to the environment. In fact, until recent developments in analytical methods, scientists weren’t reliably able to detect tire wear particles in microplastic counts—thus, these pesky microplastics may have been evading our detection for years.
Why green infrastructure may be one of our best near-term solutions
Unlike some sources of plastic pollution, we can’t simply stop driving overnight. Reformulating tire rubber to be less toxic or shed less material, while promising, will take time to develop, test and scale across the global vehicle fleet. So, what can we do about tire wear particle pollution right now?
This is where green infrastructure comes in. Green infrastructure refers to engineered natural systems (things like bioswales, rain gardens, roadside buffers and permeable pavement) that are designed to slow down, filter and treat stormwater before it reaches rivers, lakes and coastlines. Instead of routing runoff directly into storm drains and out to sea, green infrastructure gives contaminated water a chance to percolate through soil, plants and other natural filtration media, which helps trap microplastics, including tire wear particles, preventing them moving further downstream.
Early research on green infrastructure has been promising, showing that these systems are quite effective at capturing microplastics and other contaminants carried in road runoff. But there’s a critical piece we still don’t fully understand: What would it take to scale up green infrastructure across an entire city, and how much of a dent would that actually make in long-term tire wear particle pollution?
Our research on green infrastructure capture of tire wear particles
Funded by the Tire Industry Project, our plastics science and policy teams at Ocean Conservancy have partnered with the University of Toronto on a new study evaluating the costs and benefits of scaling up green infrastructure at the city level specifically to capture tire wear particles.
If you happen to be driving on the roadways of Portland, Oregon, you may spot our scientists crouched over, precariously scooping dirt with spoons from a sample area on the roadside. Don’t be alarmed—that’s just us doing science! Feel free to give us a wave.
Ocean Conservancy is currently working to:
- Quantify the scale of pollution: Collect road dust samples from 30 cities globally to measure both total microplastic and tire wear particle concentrations and determine how different variables (population density, road size, rainfall) might influence those values.
- Assess feasibility: Determine what it would take realistically—logistically, financially and spatially—to scale up green infrastructure across an entire city.
- Model positive impacts: Estimate how much city-scale green infrastructure could reduce tire wear particle pollution entering aquatic ecosystems.
- Compare across cities: Understand how well these solutions might translate across different urban contexts, focusing on Portland, Oregon; Toronto, Canada; and London, England as case-study cities.
- Make our findings accessible: Produce a public-facing toolkit to help city planners, engineers and advocates guide real-world implementation of infrastructure that captures tire-wire particles.
By pairing rigorous science with practical guidance, we hope to help cities move from asking “Could this work?” to confidently building solutions that we know can be effective.
Give today and make a difference!
How can I help?
Tire wear particle pollution can feel like an overwhelming problem. After all, it’s tied to transportation, which most of us rely on every day. But that’s exactly why research like this matters: It gives us a real, near-term path forward that doesn’t require waiting for the entire global transportation system to change first.
You can help by staying engaged with Ocean Conservancy as we continue to dig into solutions for the plastic pollution crisis—one roadway, one storm drain and one city at a time. Together, we can keep working toward a world and ocean free of plastic pollution, forever and for everyone.
The post What are Tire Wear Particles? appeared first on Ocean Conservancy.
Ocean Acidification
A tiny but remarkable visitor in Vejle Fjord-Denmark?
A small jellyfish-like animal recently reported from Vejle Fjord has attracted attention. Clear photographs suggest that it belongs to the genus Gonionemus and may possibly be the clinging jellyfish, Gonionemus vertens (Picture courtesy to Jonas Bøgelund Poulsen)

Unlike the large jellyfish commonly encountered along Danish coasts, Gonionemus vertens is a small hydromedusa, usually only around 1.5–2.5 centimetres across. Its transparent bell reveals four coloured reproductive structures arranged like a cross. Numerous fine tentacles surround the bell, often appearing bent or angled. Small adhesive pads near the ends of the tentacles allow the animal to attach itself to eelgrass, seaweed and other submerged vegetation.
This unusual behaviour explains its English name: the clinging jellyfish. During the day, it often remains attached to vegetation rather than drifting freely with the current. At night, it becomes more active and swims into the water column to feed on zooplankton and small crustaceans. Consequently, it can easily remain unnoticed even in places where it is already established. Another reason the species can be difficult to detect is its life cycle. The visible medusa is only one stage. For much of its life, the animal may persist as a minute polyp attached to a hard surface, shell or vegetation. These inconspicuous polyps can reproduce asexually and later release new medusae when environmental conditions become favourable.
Gonionemus vertens is generally considered native to the northern Pacific but has been introduced into several parts of Europe and the Atlantic. Transport on ship hulls, in ballast water or with movements of oysters and other marine organisms has been suggested as possible pathways, although the pathway responsible for any particular occurrence is rarely known with certainty.
Despite its delicate appearance, the animal should not be touched. Some populations possess powerful stinging cells and have caused intense pain, swelling, muscle cramps and, in rare cases, serious allergic reactions. Sting severity differs considerably among regions, which is one reason researchers suspect that animals currently grouped under the name G. vertens may represent a complex of closely related forms.
The Vejle Fjord observation is therefore scientifically interesting, but it should not yet be presented as a confirmed record of G. vertens. Anyone encountering a similar animal should photograph it without handling it and record the date, exact location, approximate size, number observed and surrounding habitat. Observations can be submitted to Denmark’s national species portal, Arter, where they can be evaluated and contribute to tracking changes in Danish marine biodiversity. Please use either my App: GoJelly JellySpotter or reprot to the Arter.dk: Gonionemus taxon page and Danish species-reporting portal.
References:
Edwards, C. (1977). A study in erratic distribution: The occurrence of the medusa Gonionemus in relation to the distribution of oysters. Advances in Marine Biology, 14, 251–284. DOI: 10.1016/S0065-2881(08)60448-4.
Govindarajan, A. F., Källström, B., Selander, E., Östman, C., & Dahlgren, T. G. (2019). The highly toxic and cryptogenic clinging jellyfish Gonionemus sp. (Hydrozoa, Limnomedusae) on the Swedish west coast. PeerJ, 7, e6883. DOI: 10.7717/peerj.6883.
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