Geht man auf eine Wanderung in den Bergen, so schaut man sich meistens als ersten Schritt eine Karte an. Genauso ist es auch auf dem Ozean wichtig eine Karte zu haben. Nicht nur eine Karte, in der die Küsten und Inseln verzeichnet sind, sondern vor allem eine detaillierte Karte der Topografie des Meeresbodens. Während Mitte des 19. Jahrhunderts bis Anfang des 20. Jahrhunderts Tiefenmessung noch mit einem Gewicht am Ende eines langen Seils durchgeführt wurde, wird heute in den meisten Fällen das vom Kieler Dr. Alexander Behm 1913 patentierte Echolot genutzt.
Die beste und auch wissenschaftlich anerkannte bathymetrische Daten-Zusammenstellung erstellt GEBCO (englisch: General Bathymetric Chart of the Oceans). Der Datensatz basiert auf zusammengetragenen Daten aus Schiffs-Tiefenmessungen und wurde erstmals vor 120 Jahren der Öffentlichkeit vorgestellt. Heutzutage besteht dieser Datensatz weitestgehend aus so genannter prädizierter Bathymetrie. Das bedeutet, dass Satellitenmessungen gemacht werden, die im Anschluss mit von Schiffen gemessener Bathymetrie verifiziert und ergänzt werden können. Die Satelliten können über verschiedene physikalische Zusammenhänge aus der gemessenen Meeresspiegelhöhe ableiten, ob sich unter Wasser ein Seamount befindet. Dieses Verfahren ermöglicht zwar den gesamten Ozean abzubilden, ist aber sehr ungenau. Seamounts mit einer Größe unter 2 km können zum Beispiel nicht gemessen werden. Der GEBCO Datensatz wird mittlerweile jedes Jahr erneuert. Der einzige Nachteil ist, dass es ihn an detaillierten Metadaten mangelt. Metadaten sind Hintergrundinformationen, die zum Beispiel angeben, von welchem Institut oder auf welchem Schiff die zur Verfügung gestellten Daten gemessen wurden.
Da der Datensatz in großen Teilen auf Schiffsmessungen basiert, ist er stark abhängig von Schiffsrouten, zwischen denen sich teilweise sehr große Lücken befinden. Es sind erst circa 20% des Meeresbodens auf diese Weise vermessen (Mayer et. al 2018). Auf dieser Reise wollen wir einige dieser Lücken kartieren. Genauer gesagt, wollen wir sogenannte Seamounts kartieren.
Seamounts sind unter Wasser liegende Berge meist vulkanischen Ursprungs. Sie sind typischerweise kegelförmig, haben oft Krater, lineare Kämme oder flache Gipfel. Die Form ist häufig abhängig von der Entstehung des Seamounts. Geformt werden sie an Orten, an denen es tektonische Aktivitäten gibt, so zum Beispiel in der Nähe von ozeanischen Rücken, Inselbögen oder an Stellen, wo unter der tektonischen Platte heißes Material aus dem Erdmantel aufsteigt. Seamounts, die in der Nähe von Plattengrenzen entstehen, also dort, wo die Lithosphäre (die Erdkruste und der äußerste Teil des Erdmantels) noch frisch entstanden und dünn ist, sind meistens eher klein. Klein heißt in diesem Fall weniger als 2.5 km Höhe. Größere Seamounts mit 3-10 km Höhe entstehen häufig an Stellen, wo die Lithosphäre schon älter und dicker ist. Obwohl nicht genau bekannt ist, wie viele Seamounts es gibt, ist eines sicher: es sind sehr viele!
Aufgrund ihres vulkanischen Ursprungs sind Seamounts aus geologischer Sicht sehr interessant, da sie einen Einblick in die Zusammensetzung und die Temperatur des Erdmantels geben können. Auch für ozeanographische Betrachtungen sind Seamounts wichtig, da die Bathymetrie Einfluss auf Strömungen und Vermischungsprozesse hat. So können Seamounts als Barrieren fungieren, die verhindern, dass kaltes Tiefenwasser sich mit dem warmen Oberflächenwasser mischen kann. Zu guter Letzt sind sie auch Mittelpunkt eines diversen Ökosystems. Das liegt daran, dass nährstoffreiches Tiefenwasser an ihnen aufsteigt (diesen Prozess nennt man Upwelling) und somit die perfekte Grundlage für Fische und eine vielfältige Flora und Fauna bildet.
Jetzt wissen wir also, warum wir uns für Seamounts interessieren sollten, dass es unglaublich viele von ihnen gibt und, dass viele noch nicht kartiert sind.

Auf unserer geplanten Reiseroute kommen wir an einigen Stellen vorbei, wo Seamounts vermutet werden. Durch nur leichte Kursänderung ist es möglich über einige dieser Seamounts hinweg zu fahren und sie so mit dem Schiffsecholot zu vermessen. Dabei wird ein akustisches Signal zum Meeresboden gesendet, das am Boden reflektiert und dann bei Rückkehr zum Schiff wieder empfangen wird. So kann man durch die gemessene Zeit zwischen Senden und Empfangen den Abstand zwischen Schiff und Meeresboden messen. Dieses Prinzip wird auch hier auf der Maria S. Merian genutzt, mit dem Unterschied, dass nicht nur ein Signal, sondern ein ganzer Fächer von Signalen ausgesendet wird. Damit kann ein Streifen mit einer Breite sechs Mal so groß wie die Wassertiefe vermessen werden. In unserem derzeitigen Messgebiet beträgt die Wassertiefe 2500-3000 m was einem kartierten Streifen von 15 bis 18 km Breite entspricht.
Wir befinden uns im Moment in der Nähe des Mittelozeanischen Rückens, also an einem Ort, wo neue Lithosphäre entsteht. Wie wir bereits gelernt haben, werden die hier zu findenden Seamounts eher kleiner sein. In diesem Gebiet ist auch die Anzahl und Dichte der vorhergesagten Seamounts deutlich größer. Unser erster „überfahrende“ kleine Seamount, noch weit entfernt von dem Mittelozeanischen Rückens, zeigte einen flachen Gipfel mit einer ungefähren Höhe von 450 m. Mit 7.5 km breite sowie 8 km Länge war er fast rund und äußerst sehenswert. In wie weit dieser Seamount in Zukunft weiter erforscht wird, wird sich zeigen.

Auf dieser Fahrt kümmert sich Daniel und Marianne vom „Unterwegs“-Forschungsdaten Projektes der Deutschen Allianz Meeresforschung (DAM) um alles, was mit den Seamounts und dem Fächerecholot zu tun hat. Häufig werden Fächerecholot Daten auch nebenbei erhoben, wenn der Schwerpunkt der Ausfahrt nicht in der Vermessung des Meeresbodens liegt. Im Rahmen des Projekts arbeiteten beide daran, dass diese Daten erhoben und nach der Forschungsfahrt für die Wissenschaft verfügbar gemacht werden. Beide arbeiten für PANGAEA einem Datenrepositorium für Erd- und Umweltdaten.
English version:
If you go on a hike in the mountains, you usually look at a map as the first step. It is also important to have a map being on the ocean. Not only a map listing the coasts and islands, but above all a detailed map of the topography of the seabed. During the middle of the 19th century to the beginning of the 20th century, depth measurement was still carried out with a weight at the end of a long rope, but today the echo sounder patented by Dr. Alexander Behm from Kiel in 1913 is used in most cases.
The most accurate and scientifically recognized bathymetric data collection is produced by GEBCO (General Bathymetric Chart of the Oceans). The dataset is based on collected data from vessel depth measurements and was first presented to the public 120 years ago. Today, this data set consists largely of so-called predicated bathymetry. This means that satellite measurements are made, which can then be verified and supplemented with bathymetry measured by ships. The satellites can derive from the measured sea level via various physical relationships whether a seamount is underwater. This method allows us to map the entire ocean, but it is very inaccurate. Seamounts less than 2 km in size, for example, cannot be measured. The GEBCO dataset is now renewed every year. The only drawback is that it lacks detailed metadata. Metadata are background information indicating, for example, by which institute or on which vessel the data provided were measured.
Since the data set is largely based on ship measurements, it is highly dependent on ship routes, some of which have very large gaps. Only about 20% of the seabed have been measured in this way (Mayer et. al 2018). On this journey we want to map some of these gaps. More specifically, we want to map so-called seamounts.
Seamounts are submerged mountains of volcanic origin. They are typically conical, often with craters, linear ridges or shallow peaks. The shape often depends on the origin of the seamount. They are formed in places where tectonic activity occurs, such as near oceanic ridges, arch islands, or at places where hot material rises from the Earth’s mantle beneath the tectonic plate. Seamounts that form near plate boundaries, i. e. where the lithosphere (the Earth’s crust and the outer part of the Earth’s mantle) is still fresh and thin, tend to be rather small. Small in this case means less than 2. 5 km altitude. Larger seamounts with a height of 3-10 km often form in places where the lithosphere is older and thicker. Although it is not known exactly how many seamounts there are, one thing is certain: there are many!
Due to their volcanic origin, seamounts are very interesting from a geological point of view, as they can provide insight into the composition and temperature of the Earth’s mantle. Seamounts are also important for oceanographic observations, as bathymetry influences currents and mixing processes. Seamounts can act as barriers that prevent cold deep water from mixing with warm surface water. Finally, they are also the centre of a diverse ecosystem. This is because nutrient-rich deep water rises at their flanks (a process called upwelling) and thus forms the perfect basis for fish and a diverse flora and fauna.
So now we know why we should be interested in seamounts, that there are many of them out there, and that a lot of them have not yet been mapped.

On our planned itinerary we pass some places where seamounts are suspected. By only slight course changes it is possible to drive over some of these seamounts and to measure them with the ship echo sounder. An acoustic signal is sent to the seabed, which is reflected on the ground and then received when returning to the ship. Thus, the measured time between sending and receiving can be used to measure the distance between the ship and the seabed. This principle is also used here on the Maria S. Merian, with the difference that not only one signal, but a whole range of signals is emitted. This allows a strip with a width of six times as large as the water depth to be measured. In our current measuring area the water depth is 2500-3000 m which corresponds to a mapped strip of 15 to 18 km wide.
We are at the moment near the Mid-Oceanic Ridge, a place where new lithosphere is forming. As we have already learned, the seamounts to be found here will tend to be smaller. In this area, the number and density of predicted seamounts is also significantly higher. Our first mapped small seamount, still far from the Mid-Oceanic Ridge, showed a shallow peak with an approximate height of 450 m. With 7. 5 km wide and 8 km long, it was almost round and extremely worth seeing.

On this trip, Daniel and Marianne from the “Underway” research data project of the German Marine Research Alliance (DAM) will take care of everything that has to do with the seamounts and the Multibeam Echo Sounder. Frequently, Multibeam data is collected even if the focus of the research is not in the measurement of the seabed. As part of the project, Daniel and Marianne worked to collect these data and make them available to scientists after the research trip. Both are part of PANGAEA, a data repository for earth and environmental data.
Quellen/Sources:
- Gevorgian, J., Sandwell, D. T., Yu, Y., Kim, S.-S., & Wessel, P. (2023). Global distribution and morphology of small seamounts. Earth and Space Science, 10, e2022EA002331. https://doi.org/10.1029/2022EA002331
- Mayer, L.; Jakobsson, M.; Allen, G.; Dorschel, B.; Falconer, R.; Ferrini, V.; Lamarche, G.; Snaith, H.; Weatherall, P. The Nippon Foundation—GEBCO Seabed 2030 Project: The Quest to See the World’s Oceans Completely Mapped by 2030. Geosciences 2018, 8, 63. https://doi.org/10.3390/geosciences8020063
- Damaske, D. (2013): Bathymetry and short term changes of submarine seafloor structures in the area of the former Larsen ice shelf, north west Weddel Sea, Master thesis, http://hdl.handle.net/10013/epic.67a7bbd6-5ada-4764-a961-519e334d5c56
- https://oceanexplorer.noaa.gov/facts/seamounts.html
Ocean Acidification
Soundscapes in the pearl of the orient seas: The Philippines!
Intro
At the western tip of Luzon, which is the biggest island of the Philippines, lies the small coastal town of Bolinao. Tourists seldom find their way here as it takes around seven hours to get here by bus from Manila. Still, you can spot foreigners walking around every now and then, but they really stand out among the Filipinos. A reason for their presence is often that they study or work at the Bolinao Marine Laboratory (BML), which belongs to the University of the Philippines (UP). It is one of the seven research institutions participating in the GAME project 2026. Every year, GAME brings together Master’s students from all over the world to experience different cultures and conduct globally replicated experiments in marine ecology.

This year’s Team Philippines consists of Jona, a Filipino master student of Marine Biology at the University of the Philippines, and Konstantin, a German student who is enrolled in the Master programme „Ecology and Evolution“ at Freiburg University. As part of GAME 2026, we are currently staying at BML for 6 months to run experiments about the influence of underwater soundscapes on the colonization of marine hardbottoms.

Where are we?
At the BML, we live in a dormitory together with many other students and scientists mostly from the Philippines and a few international interns. At almost any time of the day there is someone in the kitchen to hang out with, eat together, or simply have a chat. It is easy to make friends in this little community. The way to work is just a short walk along a forest path, where we can pick mangos for a snack and spot butterflies, birds, or even wild macaques climbing through the trees. After crossing a street, we reach the institute. But instead of enjoying the cool temperatures of the laboratories, we spend most of our working days outside, doing fieldwork in or near the water.


On Fridays, Konstantin experiences real Filipino culture during an almost weekly party at the institute with karaoke and lots of food and drinks. And Jona even brought some German culture to the Philippines by baking German bread for everyone.

What do we do?
Even though Bolinao is a remote place, it can get quite loud. Tricycles and jeepneys pass by, children play basketball in the streets, and karaoke can be heard almost everywhere and at any time. But just a few meters offshore, the soundscape changes. Beneath the surface of the ocean, you enter a world filled with sounds that are not so familiar to humans. When you dive down, alongside the rhythm of your own breathing, you might hear the crackling snaps of shrimp, the grunts of fish, or the rumble of waves rolling overhead. Together, these sounds form a natural underwater symphony which, however, can easily be interrupted by the noise of passing boats.

Marine organisms use sounds to communicate and to gather information about their environment, and there is growing evidence that this also applies to the larvae of sessile invertebrates such as mussels, barnacles and tunicates. During their pelagic life they are presumably able to use sounds for finding their way to suitable habitats, in which the sessile adult life stage can survive and reproduce. But what happens when these natural soundscapes are disturbed by anthropogenic noise? And what is the effect when the soundscape in a degraded reef gets enriched with sounds of a healthy coral reef?
In our experiments, which we just finished a few days ago, we investigated how different underwater soundscapes influence the colonization of hard substrata by the larvae of marine invertebrates. For this, we placed PVC settlement panels in the water and exposed them to playbacks of either boat noise, or amplified recordings from healthy coral reefs. A further group of panels was not exposed to any playbacks. By comparing the communities that establish under these different acoustic conditions, we can determine whether soundscapes affect the settlement of larvae.
Challenges
In contrast to the other GAME teams of this year’s project, we don’t have a jetty at BML. So, our first challenge was to build a setup that could carry an MP3 player for the soundscape playbacks, an amplifier, and an underwater speaker, which all need electricity supply, and position it about 30 to 50 meters away from the beach.
We ended up building a floating frame that carries the settlement panels as well as the underwater speaker, and combined it with a waterproof box, which was above the waterline and contained all the sensitive technical equipment. The box was firmly sealed so that it withstood waves and heavy monsoon rains, while its interior remained dry. At the same time, it was protected with a reflective car cover to prevent the technical equipment from overheating, as the box was constantly exposed to the burning tropical sun. To supply the set up with electricity, we – with the help of technicians and divers – rammed long bamboo poles into the seafloor and attached a cable to them that was connected to an electrical outlet on land.

As a consequence of this particular set up, every time we want accessed it, we either went snorkeling or took a boat. Hence, we had to plan our work according to the tides. We also needed to avoid the hottest hours of the day, and sometimes we needed to hurry because a storm was approaching. In the end, you could say that we learned to live in the rhythm of Mother Nature.


After some test runs, everything was ready and we could finally start the experiments. From that moment on, we regularly inspected the frames to check whether everything was still in place and whether there were any damages or malfunctions. So, we still had to go into the water almost every day. It was beautiful to make a small detour while working to see some nudibranchs, octopus or pufferfish and get to know the local underwater environment better every day. Once a month we took all the settlement panels out of the water to collect data about the abundance of single species and to document the community composition. Already after a few weeks in the water, many barnacles had settled on the panels. At a later stage, they dominated the artificial substrates together with macroalgae and black mussels. Furthermore, we could detect different species of ascidians, polychaetas, and hydrozoans, which, however, only occurred in very low abundances.


Alongside with the preparations of the experimental set up, every few weeks, Konstantin was able to join the coral research group during their fieldwork and went diving with them. This how we got our recordings of sounds from nearby healthy coral reefs. He deployed underwater microphones (hydrophones) while diving and since this task took only some minutes of the dive, he often still had enough air and time to enjoy the underwater world of the Philippines more closely.


Life in Bolinao
To put it in a nutshell, life here is a mix of relaxing beach vibes, lively markets in the city center and a wonderful community in and around the institute. A foundational value embedded in Filipino communities is Bayanihan, which embodies unity, cooperation, and collective volunteerism, where individuals work together toward a common goal without expecting personal gain or reward. This is something we feel and experience at the institute, as any individual is willing to provide help without asking for anything in return.

Science has a very strong application-oriented status here. Within the working groups at the institute, people often discuss the benefit of their research to the community. We also talked to local fishermen. They were very curious about our work and told us how they could already make use of previous research by the institute and increase their income at mussel farms.
Our experiment also could help these fishermen in the future. If we gain a better understanding of how soundscapes affect marine life, we could use that knowledge to prevent the decline of biodiversity in these waters. This would enable the community to secure stable access to the natural marine resources that serve as an important source of food and income here.

The end of our experiments
The Philippines experience 20 typhoons in a year on average and most of them hit the country during the northwest monsoon between July through October, which is overlapping with the last phase of our experiments. The frames we deployed were built to go along with the waves, but strong waves with heavy rains inflicted some damage on them. Because of that and since further storms were about to come, we decided to terminate the experiments some weeks earlier than planned.
We didn’t do much analysis of the data that we collected yet, but the first results are already fascinating. When comparing the communities that established under the influence of boat noise with those that developed in the absence of playbacks, it seems that the noise decreased the communities‘ biomass and biodiversity while it also altered their composition.
For assessing the dry weight of the organisms that colonized the panels, we scraped off everything that grew on their surfaces and dried this material in an electric dryer. After this work, the whole laboratory building smelled like a fish market. On the next day, we could already see that people took notice as many fans appeared on the hallway to blow away that smell. Luckily, everyone has been very kind and patient, helping us with ventilation and cleaning and simply putting up with the smell. Soon, our time here will come to an end, and we will head back to Kiel, Germany, to work on our data. We will be sad to say goodbye to all our colleagues and friends here, and we hope that the smell of fish will not be the only impression we leave behind!
Soundscapes in the pearl of the orient seas: The Philippines!
Ocean Acidification
Team Madeira – At least one of us is thinking
It all started with a bang – several million years ago. Beneath the Atlantic, successive eruptions raised an enormous volcanic mountain from the ocean floor, and its very tip now forms rugged cliffsides, deep red canyons and fertile ground for hotel chains. How land was formed here, in the middle of the ocean, is still plainly evident in the red and black banded mountainsides of Madeira, in pools of volcanic rock frozen mid-flow and in cliffs sculpted by magma, wind and water. Life clings to this volcanic ground with stubbornness: Cacti climb sheer ridges, while sage-green, brown and vibrant yellow shrubs crouch against the rugged terrain.
Today, Madeira is known as the Island of Flowers, an image that echoes across postcards, signs and souvenirs. Indeed, many of the winding mountain roads are lined by eucalyptus trees from Australia, tall white and lilac lilies from South Africa, and hydrangeas from Asia. Fitting for an island that lives from tourism, while also beginning to buckle under its strain.

Our own project looks, at least partly, at another, less visible invader: human-made sound. Beneath the ocean’s surface, boat engines add to the island’s natural underwater soundscape, and during the six months we spend here we want to find out whether sound changes where the larvae of marine sessile animals, such as bryozoans, tunicates or polychaetes, choose to settle. Those animals are sessile in their adult life, but as larvae they are free floating. In this stadium, they are influenced by a wide variety of environmental factors—including noise—while they seek out a suitable habitat in which they could settle and survive.
And with that “Óla” from Team Madeira. We are Elin and Jana, two German students who have come to Madeira for half a year to take part in this year’s GAME (Global Approach in Marine Ecology) project.
Jana studies biology at the Ruhr-University in Bochum. “I was always interested in marine biology and had already worked in this field for my bachelor’s thesis. When I decided that I didn’t want to move away from Bochum for my Masters, I was a little bit sad, deep down, thinking that I couldn’t continue to pursue marine biology. So, I was thrilled to return to the ocean and to fieldwork when I got accepted for GAME”.

Elin studies biological oceanography in Kiel “This year’s GAME topic of The influence of soundscapes on hard bottom community colonization seemed made for me, since I had already written my bachelors thesis about the colonization of hard substrates and if I could’ve picked any field, sound would have been it.”
This year is the first time that GAMIEs are working with sound, which made the planning phase in Kiel in March extra exciting for us. We tested underwater microphones, so called hydrophones, tried out speakers and had many, many, many discussions about scientific literature and the experimental setup. In the end all teams agreed on one basic concept: One student in each country would analyze the effects of boat noise and the other the influence of natural soundscapes on the formation of invertebrate communities. Natural soundscapes will be captured by deploying thydrophones in underwater habitats that are typical for the marine region a team is working in. In Madeira, the underwater world is strongly shaped by the past volcanic activity, and features steeply sloping rock faces and rocky areas that are overgrown with algae and sessile animals. These form the most typical habitat of the region. Furthermore, here and there they give way to sandy bottoms at greater depths.
We are investigating the settlement under the influence of natural sounds, because more and more marine habitats have been destroyed by human activity. In the past, several studies have been conducted on marine mammals, fish, shellfish and coral species, which found that when sound was used to simulate healthy habitats in otherwise disturbed environments, it led to the successful re-establishment of populations. A concept that is known as acoustic restoration.
In our experiments, both, the natural sounds and the boat noise, will be played back from speakers and will be directed onto plastic plates hanging in the water, to which the larvae of sessile animals can attach.
So much for the theory.
After arriving on Madeira in early April, we got to work and realized quickly that reality is lots of planning, glue, trips to the hardware store and starting over. Luckily, we have kind and helpful supervisors at MARE, the research institute here in Madeira, many of which are former GAMIEs. They contributed their experience, advice and occasional emotional first aid. But most of the time we’re trying to do as much as we can on our own – with special support from Jana’s electronics-technician-husband, Niklas, who also came along to Madeira and is of great help with all the equipment. Even though we had many long and a few frustrating days, it was nice to plan and build everything on our own. Actually, it’s incredibly rewarding to see the finished results of our work running smoothly while the experiments are going on.

Our workplace here in Madeira is the marina in Quinta do Lorde, which is almost on the eastern tip of the island. It’s a beautiful workplace, because most days the water is calm and clear and we get to see sepias, triggerfishes and a school of barracudas swimming in the shallow waters. This makes it all the more frustrating that it is forbidden to go in, due to the ship traffic – you can imagine how hard it is for two marine scientists to follow this rule, and how often we stare into the water longingly.

The ideal way for us to run the two experiments was conducting them both at the same time. But of course, the playbacks of the natural soundscape and the boat noise shouldn’t mask or overlay each other. And they should not reach those panels that we have to study invertebrate settlement in the absence of any playbacks. This prerequisite is called acoustic isolation: whatever happens near one speaker shouldn’t affect the other settlement plates. Since sound can travel far under water, we choose the two opposite ends of the marina and two jetties in between for the deployment of the settlement panels.
Unfortunately, our workplace is in a busy marina and to check if the play-backed boat noise doesn’t affect the other locations where we placed settlement plates, we need silence throughout the entire area. So, we had to stop and redo the measurements many, many times, because of incoming and departing boats, loud wind, cracking noise from the jetties or technical difficulties with our hydrophones.
We had one truly frustrating Friday afternoon when we wanted to test acoustic isolation but couldn’t get even five minutes of silence without a boat engine in the background for hours! And then, shortly before we had to catch the last bus home, we finally managed to do the test- and it was perfect. We had recordings without any disturbances and we had acoustic isolation- which meant we could run both experiments in parallel.
Then the wind blew the hydrophone from the jetty into the water, while we were packing up. Jana was over it and ready to give up, but Elin declared it the best thing that had happened that day. She had in the morning naively predicted a short workday with plenty of time to go snorkeling. Instead, she got special permission to go into the marina just this once – and gleefully fished out the hydrophone. Everything was done just in time before the last bus came and we decided never to test acoustic isolation on a Friday afternoon again.

Since Jana studies the effects of natural soundscapes on larvae settlement, she needs to record the marine ecosystems of Madeira. The team at MARE helped her to choose a few promising locations, which best reflect Madeira’s rocky underwater landscape. They are in protected areas and have little boat traffic.We built six hydrophone stands, of which one was placed at each location with the help of a technical diver. The stands were constructed in a way that the hydrophone could be attached and detached by freediving from the surface, and this allows us to work independently of the diver. And, of course, to have the opportunity to go snorkeling for work :). For the first month it was just Elin who could hold her breath long enough to reach the hydrophone stand, which was in 5 to 8 meters water depth, because she had years of experience. But after training freediving while snorkeling in beautiful locations all over the island, first Niklas and then Jana figured it out and now we can divide this very popular task among the three of us.

Even when the project is running smoothly, there are always a million little things to think of, to plan and to organize. Our motto became ‘at least one of us is thinking’ – because of how often one of us forgot something or didn’t think ahead and the other one caught it just in time. And there is something to it. Even though we will write separate Master theses, we share the work and the responsibility, and it is amazing to work in a team in which you can truly rely on the fact that the other person cares just as much and is right there with you.

When we’re not in the workshop building our frames or glued to the binocular during long sampling days, we love to be in the water for snorkeling trips or go hiking in the beautiful mountains. The island’s nature is fascinatingly versatile, and after almost 5 months have passed now, we’re sure that we’ll never grow tired of the amazing views. There are so many Levada trails with waterfalls, hidden paths through the mountains and small towns to visit. Levadas are man-made irrigation channels on Madeira. They carry the water from the mountains from the north to the south. The network, which spans a total of 2,000 to 3,000 kilometers, is used today not only for agriculture but primarily as a world-famous hiking trail. We make a point to go exploring new places, but the joy of staying for half a year is that you get to find your favorites and come back to them.

We are really happy to have worked and lived here on Madeira, and we can’t believe that half a year has almost come to an end; we’d do it all over again in a heartbeat.
Ocean Acidification
Do Sea Turtles Get Lost?
Did you know some female sea turtles can travel hundreds—or even thousands—of miles through open ocean before returning to nest on or near the very beaches where they hatched? In fact, Leatherback sea turtles take this long-distance travel to an extraordinary level. Pacific leatherbacks nesting in Indonesia have been documented migrating more than 10,000 kilometers to the West Coast of the United States. That’s the longest migration of any air-breathing marine vertebrate. So how do they accomplish this without Google Maps?
Scientists have found that sea turtles can sense magnetic information and use it as a navigational cue. Because the strength and angle of Earth’s magnetic field vary across the planet, these subtle differences can provide turtles with information about where they are and help guide their movements across the ocean. For turtles that return to their birthplace to nest (a behavior known as natal homing), these magnetic cues may be especially important. It’s an extraordinary system, but even the best navigation can take a turtle only so far.
Despite their great sense of direction, sea turtles don’t always make it where they’re going.
A sea turtle may be capable of navigating thousands of miles, but reaching the right destination is that much more of a challenge when human-caused obstacles lie in the way.
Artificial light is one example. Artificial lighting not only discourages nesting females from coming ashore but also has a harmful impact on hatchlings, which historically emerge from their nests at night and orient toward the brightest horizon. On a natural, undeveloped beach, that is generally the open ocean. But artificial light from coastal development can overwhelm the natural cue, drawing hatchlings inland away from the water and causing them to get lost on day one.
Coastal development not only brings more artificial light and human activity to the shoreline, but it also changes turtle habitats themselves. Buildings, roads and other development can alter or reduce areas sea turtles need for nesting. Shoreline armoring, such as seawalls, can eliminate the dry sand turtles need to successfully nest, while beach driving and other activities can further disrupt nesting habitats. And these challenges extend beyond the beach.
The ocean is getting noisier, too. Sea turtles have internal ears and can hear underwater sounds. Vessel traffic, oil and gas surveys, underwater construction and sonar all add noise to the marine environment. Human-generated sound can cause stress, disrupt normal behaviors or even force marine animals to move from preferred habitats or divert from migratory paths.
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Evolution never saw the plastic grocery bag coming.
Then there’s a threat sea turtles encounter almost everywhere they travel: plastic pollution. Sea turtles evolved over millions of years to spot drifting prey, like jellyfish. But plastic rapidly started to be used only around 60+ years ago.
Our plastic trash entered the ocean so quickly that animals haven’t had time to adapt. To a hungry sea turtle, a floating plastic bag still looks enough like dinner to trick even an experienced turtle. Plastic bags, balloons, soft plastic packaging and other plastics, once swallowed, can block a turtle’s digestive tract or puncture internal organs. And it doesn’t necessarily take much.
A recent Ocean Conservancy study of more than 10,000 marine animal autopsies found that nearly half of the sea turtles studied had ingested plastic. Even more alarming, researchers found that for adult loggerhead turtles, swallowing just one and a half times the plastic in a golf ball was enough to kill 50% of these creatures.
It’s a heartbreaking reminder that something we use for minutes can threaten an animal that’s been roaming Earth’s ocean for more than 100 million years.

Ancient animals still face very modern threats.
Sea turtles survived the extinction event that wiped out dinosaurs. They’ve outlasted shifting continents and dramatic changes to our planet. But surviving millions of years doesn’t make them invincible. Today, they’re facing threats that appeared in the blink of an evolutionary eye: plastic pollution, habitat loss, vessel strikes, fishing gear entanglement and climate change. The remarkable thing is that many of these challenges aren’t inevitable. They’re problems we can all help solve.
Together, we can reduce the amount of plastic that reaches the ocean. We can protect and restore nesting beaches. And we can support policies that protect healthy ocean ecosystems. Every action helps make our waters a safer place for animals that depend on it.
So, do sea turtles get lost? When left to their own devices, not often. Sea turtles have an extraordinary ability to navigate across vast stretches of open oceans. But there’s a bigger question worth asking: Can we help make the ocean a safe place while they make these incredible journeys? Navigation is only part of the challenge for sea turtles trying to find their way home. Sea turtles may know where they’re going, but it’s our job to ensure the ocean and coastlines they depend on are safe when they get there. That’s why Ocean Conservancy is committed to protecting our entire ocean—and all the creatures that dwell there.
We’re fortunate to share the planet with these amazing creatures. Their journeys are a remarkable feat of science and survival. To all the turtles out there: Here’s to finding your way—wherever you’re going!
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The post Do Sea Turtles Get Lost? appeared first on Ocean Conservancy.
https://oceanconservancy.org/blog/2026/08/27/do-sea-turtles-get-lost/
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