English version below
Wenn man an Chemie denkt, denkt man wahrscheinlich schnell an explodierende Gläser, ätzende Säuren und verrückte Professoren, aber nicht an den Ozean. Hier an Bord wird unsere Wissenschaftsteam auch von zwei chemischen Ozeanographen begleitet, Tobias Steinhoff und Kristin Kampen.
Den beiden habe ich die Frage gestellt, „Was findet ihr an der chemischen Ozeanografie spannend?“: Es ist unglaublich interessant, was es alles an unsichtbaren Prozessen im Meer gibt, die unser aller Leben beeinflussen: In der chemischen Ozeanographie untersuchen wir, wie sich chemische Bestandteile im Meer verhalten, z.B. wie sich gelöste Gase (wie CO₂ und Sauerstoff), Nährsalze (wie Nitrat und Phosphat), Spurenmetalle und organische Verbindungen im Meerwasser verhalten und verteilen. Der Ozean nimmt CO₂ auf, produziert Sauerstoff und transportiert Nährstoffe durch den Ozean und überall wirken chemische Prozesse mit. Diese Zusammenhänge zu verstehen ist Grundlage unserer Arbeit.
Auf unserer Ausfahrt in der Labradorsee nehmen sie Seewasserproben und extrahieren gelöstes organisches Material (DOM). Dies umfasst alle organischen Verbindungen, die im Meerwasser gelöst sind, also nicht als Partikel vorliegen. Das sind zum Beispiel Zucker, Aminosäuren, Fette und komplexere Moleküle, die aus abgestorbenen Organismen, Ausscheidungen von Meereslebewesen oder dem Abbau von Algen stammen. Als einer der größten Kohlenstoffspeicher spielt DOM eine zentrale Rolle im marinen Kohlenstoffkreislauf. Die Labradorsee ist eine der wichtigsten Regionen für die Bildung des North Atlantic Deep Water (NADW). Oberflächenwasser sinkt in die Tiefe und nimmt dabei DOM mit. Das NADW verteilt dieses Material dann über Jahrhunderte durch die Weltmeere und entzieht so der Atmosphäre langfristig Kohlenstoff. Zusätzlich werden kontinuierliche Messungen von pCO₂/O₂ im Oberflächenwasser während der Fahrt durchgeführt, um sich den Austausch von CO₂ zwischen Ozean und Atmosphäre anzuschauen. Viele Prozesse sind hierbei immer noch nicht vollständig verstanden, wie z.B. der Gasaustausch bei hohen Windgeschwindigkeiten.
Da es hier auf See, besonders in dieser Region, oft sehr stürmisch zugeht, ist kein Geheimnis und es geht natürlich besonders in einem Chemie Labor dann doch mal etwas zu Bruch. Wie läuft diese Arbeit also bei 11bft und 6 Meter Wellen ab. Wasserproben müssen meist innerhalb von 24 Stunden verarbeitet werden. Da kann man nicht immer Rücksicht auf die Wetterbedingungen nehmen. Einige Arbeiten werden immer noch nasschemisch gemacht und unter Einsatz von Glasmaterial. Sowohl das genaue Abmessen von Reagenzien als auch das Zusammenhalten der Glasware ist nicht immer einfach bei einem rollenden Schiff (und auch nicht immer erfolgreich). Man versucht zwar den doch dann plötzlichen Bewegungen des Schiffes entgegenzuwirken und alle Proben Behälter, Kisten und Flaschen zu sichern. Man wird aber dann doch mal von einem umkippenden Mülleimer überrascht und die noch neu verpackten Plastikröhrchen oder andere Fliegengewichte im Regal finden bei der einen oder anderen Welle ihren Weg auf die gegenüberliegende Seite im Labor. Dazu kommt, dass beim Arbeiten mit chemischen Stoffen und Proben doch des Öfteren beide Hände für die Arbeit gebraucht werden. Wird man dann allerdings von einer Welle überrascht, erfordert das Festhalten mit der dritten Hand (Fuß falls man schnell genug ist), einiges an Bauchmuskeln.
Foto: Julia Pelle
Das Besondere an der Arbeit auf See ist, dass man neben der alltäglichen Schreibtischarbeit auch praktisch arbeiten kann. Dabei ist man auf die enge Zusammenarbeit mit seinen Kollegen angewiesen und lernt sie dabei viel besser kennen. Zusätzlich sind auch viele andere Forschungsbereiche mit an Bord, wodurch es einen spannenden Austausch zwischen den einzelnen Gruppen gibt.
Zum Schluss hier noch ein kleiner Tipp am Rande von unseren Chemikern und für deine erste Forschungsseereise: Laschen, laschen, laschen und immer ein Ohr am Bordfunk: Der Arbeitsplan ist bei den Wetterbedingungen eher ein Vorschlag und kann sich stündlich ändern (die nächste CTD Station ist immer um die Ecke).
Chemistry: Making the Invisible Visible
When you think of chemistry, you probably quickly imagine exploding glassware, corrosive acids, and crazy professors, but not the ocean. Here on board, our scientific team is also accompanied by two chemical oceanographers, Tobias Steinhoff und Kristin Kampen.
I asked them the question: “What do you find exciting about chemical oceanography?”
“It is incredibly fascinating how many invisible processes exist in the ocean that influence all of our lives. In chemical oceanography, we study the fate of various chemical components in the ocean: for example, how dissolved gases (such as CO₂ and oxygen), nutrients (such as nitrate and phosphate), trace metals, and organic compounds behave and are distributed in seawater. The ocean absorbs CO₂, produces oxygen, and transports nutrients through complex cycles, including chemical processes. Understanding these relationships forms the basis of our work.”
During our expedition in the Labrador Sea, they collect seawater samples and extract dissolved organic material (DOM). This includes all compounds dissolved in seawater, meaning they are not present as particles. Examples include sugars, amino acids, fats, and more complex molecules that originate from dead organisms, excretions from marine life, or the breakdown of algae. As one of the largest carbon reservoirs, DOM plays a central role in the marine carbon cycle.
The Labrador Sea is one of the most important regions for the formation of North Atlantic Deep Water (NADW). Surface water sinks into the depths, carrying DOM with it. NADW then distributes this material throughout the world’s oceans over centuries, thereby removing carbon from the atmosphere over the long term. In addition, continuous measurements of pCO₂ and O₂ in surface water are taken during the voyage to study the exchange of CO₂ between the ocean and the atmosphere. Many processes involved are still not fully understood, such as gas exchange under high wind speeds.
It is no secret that conditions at sea especially in this region are often very stormy, and in a chemistry lab, things can occasionally break. So how does this work at 11 Beaufort and 6-meter waves? Water samples usually need to be processed within 24 hours, so you cannot always take weather conditions into account. Some work is still done using wet chemistry and glass equipment. Accurately measuring reagents and holding glassware steady is not always easy on a rolling ship (and not always successful). Although efforts are made to counteract sudden ship movements and to secure all sample containers, boxes, and bottles, you may still be caught off guard by a tipping trash bin, and newly packaged plastic tubes or other lightweight items can suddenly fly across the lab with the next wave.
On top of that, when working with chemicals and samples, both hands are often needed. If a wave hits unexpectedly, holding on with a “third hand” (your foot, if you are quick enough) requires quite a bit of core strength. What makes working at sea special is that, alongside everyday desk work, you can also do hands-on work. This requires close cooperation with colleagues, allowing you to get to know them much better. In addition, many other research disciplines are on board, which creates exciting exchanges between different groups.
Finally, here is a small tip from our chemists for your first research expedition: strap everything down, strap everything down, strap everything down and always keep one ear on the ship’s radio. The work schedule is more of a suggestion under these weather conditions and can change hourly (the next CTD station is always just around the corner).
Ocean Acidification
Dr Heidarzadeh’s TV interview with SkyNews on the massive M7.7 Panama earthquake on 9 October 2026
Dr Heidarzadeh’s TV interview with SkyNews on the massive M7.7 Panama earthquake on 9 October 2026. Click here for the full story.
Dr Heidarzadeh’s TV interview with SkyNews on the massive M7.7 Panama earthquake on 9 October 2026
Our ocean is an incredibly vast and mysterious place. And there is no place where that is more evident than the deepest ocean area in the world: the legendary Mariana Trench. Located east of the Philippines, the Mariana Trench lies in the Mariana Archipelago in the western portion of the North Pacific. The greater area of the Mariana Trench Marine National Monument is made up of more than 95,000 square miles of ocean. Beneath these waters lie incredibly complex aggregations of submerged islands and volcanoes … and of course, an astoundingly massive trench.
Dive in with us to have your biggest questions answered about the famed Mariana Trench.
How deep is the Mariana Trench?
The deepest part of the Mariana Trench, known as Challenger Deep, is almost 36,000 feet below the ocean’s surface. For context, Mount Everest is about 29,000 feet above sea level, so the Mariana Trench is about 7,000 feet deeper than Mount Everest is tall. For one more comparison, the RMS Titanic lies at a depth of about 12,500 feet below sea level. The Challenger Deep is in waters nearly three times deeper than this ship’s final resting place.
Due to its enormous size, the Mariana Trench has at times been affectionately nicknamed the Grand Canyon of the ocean. This is certainly a picturesque image, but don’t let the mammoth size of this U.S. national terrestrial park fool you into thinking the Mariana Trench matches its size. The trench’s footprint is estimated to be 120 times larger than the Grand Canyon’s, and to reach the bottom of Challenger Deep, you’d need to descend through almost six Grand Canyons stacked on top of each other before you’d reach the seafloor.
Oh … and did we mention it’s five times wider than it is deep? It’s about 43 miles wide!
What is Challenger Deep, and how long would it take to reach it?
Challenger Deep is the deepest point of the Mariana Trench. Fewer than 30 people have ever journeyed to this area. The trek below the surface is long, dark and time-consuming, and it’s not an expedition considered lightly by scientists and explorers.
The first people to descend into the depths of this area in 1960 were oceanographers Jacques Piccard and Don Walsh, and it took them close to five hours to reach Challenger Deep. Since then, more advanced submersibles have been created, but it still takes two to four hours for modern vessels to reach such depths. For example, explorer and filmmaker James Cameron reached the seafloor in a little more than 2.5 hours in the first documented solo submarine dive to the area, and it took oceanographer Dr. Dawn Wright about four hours in 2022. It is crucial that these submersibles descend slowly and steadily beneath the surface, as the immense water pressure compounds with every mile a submersible descends. Speaking of pressure …
Get Ocean Updates in Your Inbox
Sign up with your email and never miss an update.
What is the water pressure at the bottom of the Mariana Trench?
If you thought the depth of the Mariana Trench was its only jaw-dropping feature, think again. Water pressure is one of the most important factors affecting deep-sea life. In the ocean, pressure increases by one atmosphere for every 33 feet (10 meters) of depth. One atmosphere (a unit of measurement for pressure equivalent to average air pressure at sea level) is equal to about 14.7 pounds per square inch (PSI), which is the approximate standard atmospheric pressure at sea level. If you were to convert atmospheric pressure into weight, one atmosphere is about the weight of a bowling ball. Stay with me, friends.
If a vessel were to dive 2,000 feet below the surface, the pressure would equal that of 60 bowling balls stacked atop every square inch of that submersible. But 60 bowling balls is simply nothing compared to the pressure in the Mariana Trench. The atmospheric pressure at the depths of Challenger Deep is equal to about 16,000 PSI. That pressure is about the same as the weight of an entire full-grown elephant on every square inch of a submersible!
Need a more extreme comparison? If a human were to be placed at the bottom of the Mariana Trench, the pressure would be equal to that of 50 jumbo jets piled on top of a person!
Do any animals live in the Mariana Trench?
The depths of the Mariana Trench come with immense pressure and extreme darkness, but somehow, life finds a way to survive. Organisms that live at an extreme depth, like that of Challenger Deep, have to be highly adapted to low temperatures (typically just above freezing), high pressure and virtually no light at all.
Species found in the depths of the Mariana Trench might look vastly different from animals from other ocean depths because their anatomy has been refined to thrive in harsh conditions. At such great depths, these animals typically depend on chemosynthesis (using nutrient-rich waters being pumped out of hydrothermal vents) or descending detritus (dead matter that has fallen from higher parts of the ocean) for food, such as whale falls. Just a handful of these animals include species of octopuses and squids, sea cucumbers, amphipods, sea jellies, shrimp, sea worms and some wild-looking fish!
In 2025, more than 7,000 new species were discovered in the Mariana Trench, including the hadal snailfish (Pseudoliparis swirei). This is the deepest-dwelling fish currently known to science. Now, the fish has been dubbed “the Mariana snailfish.”
How was the Mariana Trench formed?
The process by which the Mariana Trench was created is a geologically fascinating one known as subduction. On the Earth’s surface, there are thin plates that cover the planet’s mantle, which is made of molten rock. If two of these plates collide, one pushes down into the Earth’s mantle while the other is pushed over the bottom plate. When this happens, a trench is formed from the drag of the bottom plate. This process can sometimes create incredibly strong earthquakes. The plates that forged the Mariana Trench’s creation are estimated to be up to approximately 180 million years old.
This trench was unknown to scientists until 1875. It was then that a team of explorers on the HMS Challenger measured the depth of the sea by simply lowering a weighted rope into the water. They were baffled when they measured that first portion of the seafloor to be five miles below the surface. And so was born the origin of some of the most daring deep-sea explorations known to mankind to date.
Is the Mariana Trench protected?
The Mariana Trench is in waters off Guam and the Mariana Islands. The region is protected from some human activities under its status as a marine monument. The creation of the Mariana Trench Marine National Monument signified that international, national and local leaders all recognize the importance of protecting this area.
However, just because the region is protected does not mean it’s not vulnerable to modern threats to ocean health. Plastic bags have been spotted in the Mariana Trench during several expeditions, highlighting the far-reaching impact of the marine debris problem. No corner of our ocean is safe from the ever-present threat of plastic pollution. The reality of a changing climate makes the future well-being of wondrous places like the Mariana Trench uncertain. What’s more: More than 70% of the global ocean has yet to be mapped. And what we don’t yet know about, we cannot wisely work to protect.
It’s up to us to work together to defend our ocean, from the sandy shores of our favorite beaches to the deepest, darkest parts of the sea. Together, we can work to protect our ocean as a whole, which ultimately helps protect treasured places like Challenger Deep.
Find out how you can join Ocean Conservancy’s wave of momentum to secure a healthy ocean and a thriving planet, forever and for everyone!
The post The Mysteries of the Mariana Trench appeared first on Ocean Conservancy.
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.