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As we enter the final two weeks of JOIDES Resolution Expedition 401, we figured it was time to check in with our science team on their expedition highlights to date.

So, we checked in with some of them asking…

What’s the most interesting thing you’ve found in these cores so far?

“That we can correlate individual sedimentary beds (cycles) 100s of miles between our drill sites. It’s an essential step in finding how the Mediterranean overflow behaved and changed through time.”

-Trevor Williams, EPM

Image of the surface of a sediment core, and an X-ray image of the same core showing pyritized burrows. Credit: IODP

“I think the most interesting thing I’ve seen in our cores so far are pyritized burrows. The thing is you can’t really see what they look like under the sediment unless they show up on the X-ray scan. So, when we look at a core, we might see some nodules of pyrite and some spots indicating a trace fossil, but the X-ray will show the actual burrow network if the trace fossil has been infilled with pyrite or a different sediment than the host material. If the infill is denser than the surrounding sediment (like pyrite), it shows up dark on the X-ray scan. Chondrite is usually visible as spots on the split surface of the core, and occasionally you can see a branch in the trace fossil, but seeing the entire network of the burrow is really cool.”

-Patty Standring, Sedimentologist

“As a geophysicist that has a moderate experience with drilling and coring, what surprised me in the cores overall is how homogeneous and unchanging the sediments look to the eyes. On seismic profiles and other measured physical properties data we see a lot of boundaries and variations that are, most of the time, impossible to detect by the naked eye.”

-Fadl Raad, Physical Properties

Image of core showing turbidite sands. Credit: IODP

“Turbidite sands in U1609, that record the movement of coarse grain material from shallower water into deeper water, by gravity flows.”

-Simon George, Sedimentologist

“The most interesting/exciting thing for me is the cross lamination in the mud.

Conventionally, people generally presumed that for fine-grained (e.g., < 20 micrometer) sediments, due to their rather small size, can be deposited only under rather quiet environments through suspension settling. However, about 15 years ago, flume experiments (the flume lab from which I got my Ph.D.) revealed that fine-grained sediments can also be deposited under running water conditions and that they form the same sedimentary structure (ripples) as sands. In ancient sediments, the mud ripples are expressed as cross lamination, which not only tells us that these fine-grained sediments were deposited under relatively energetic flowing conditions, but this is also the first time (I believe) that mud ripples are documented in the deepwater deposits in the cores.”

-Zhiyang Li, Sedimentologist

“The most interesting thing for me is evidence for an outflow during the salinity crisis – there’s been a lot of debate on this over the past few decades.”

-Udara Amarathunga, Micropaleontologist

“We found a dolostone in the core catcher at the bottom of Hole U1610A! This was our deepest recovered sample and the most different lithology of all the cores. Dolomite might be my favorite rock/mineral. We do not yet fully understand how it forms, even though people have been studying it for over a hundred years. There is a hilarious (but actually good) paper title on the topic: “Failure to Precipitate Dolomite at 25 degrees C from Dilute Solution Despite 1000-Fold Oversaturation after 32 Years”.”

-Clara Blättler, Inorganic Geochemist

“Void space gas. Watching some cores fizz like champagne was spectacular.”

-Sarah Feakins, Organic Geochemist

Interesting Finds for Expedition 401

Ocean Acidification

Where the sky meets the ocean

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By Leonie Jaeger (ICBM Oldenburg)

The ocean is the dominant climate regulator of our Earth. I am on board the RV Meteor to conduct measurements that helps us better understand the critical processes at the interface between the atmosphere and the ocean. The focus of these measurements is heat and freshwater fluxes, two key drivers that both influence and regulate Earth’s climate.

The ocean stores and transports vast amounts of heat across the whole globe. The exchange of heat between the atmosphere and the ocean is controlled by different surface heat fluxes. The sun emits shortwave radiation, which warms the surface ocean, though part of this radiation is reflected at the water surface. At the same time, the ocean emits longwave radiation towards the sky due to its temperature, some of which is reflected and absorbed by water vapor and clouds. To quantify these fluxes, I use radiometers: sets of upward- and downward-looking sensors that measure radiation coming from the sky and from the ocean. Specifically, pyranometers measure shortwave radiation, while pyrgeometers measure longwave radiation.

Radiometers to capture short- and longwave radiation coming from the sky and from the ocean to quantify radiative heat fluxes between the atmosphere and the ocean. Photo: Leonie Jaeger.

Over the open ocean, freshwater fluxes result from two processes: evaporation and precipitation. Approximately 80% of the global freshwater flux occurs over the ocean, underscoring the ocean’s dominance in the global water cycle and its influence on climate over land. In a warming climate, evaporation is expected to intensify as temperatures rise and the atmosphere’s capacity to hold moisture increases. That makes is very important to better understand these fluxes. However, high-quality measurements of precipitation and evaporation using remote techniques remain challenging. On this cruise, I am using a disdrometer, an instrument that measures rain in high resolution. It allows us to investigate not only the total amount of rain but also the velocity and size of individual raindrops, enabling a detailed characterization of rain events.  

A distant heavy rainfall event in the ITCZ over the central Atlantic Ocean. Photo: Leonie Jaeger.

Our cruise track crosses the Atlantic Ocean from South to North, passing the equator. This transect will provide a valuable dataset. Importantly, we will cross the Inter-Tropical Convergence Zone (ITCZ), a region near the equator characterized by heavy rain and thunderstorms. These storms originate from warm, moist air that rises continuously. As the air rises, it cools and condenses, forming thick clouds and intense precipitation. Because the ITCZ is driven by the convergence of trade winds from both hemispheres, it maintains persistent bands of convection. In this zone, these convective systems can trigger even more convection in the atmosphere driving the tropical climate. Together with warm surface temperatures, these high-energy processes can lead to the genesis of tropical cyclones. Thus, the atmosphere influences the ocean, and the ocean influences the atmosphere. Direct measurements at their interface are essential to better understand these processes shaping our climate. My responsibilities include installing and maintaining the measurements systems, as well as data validation and data storage. Maintaining sensors close to the ocean requires frequent cleaning, because sea spray leaves salt deposits everywhere, leading to corrosion. Together with ship-based measurements such as air temperature, wind speed and humidity, and oceanographic underway measurements including continuous observation of the water temperature, salinity, turbidity and chlorophyll, our data will provide a comprehensive dataset to study fresh and heat water fluxes between the ocean and the atmosphere.

Where the sky meets the ocean

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Ocean Acidification

METEOR Sets Sail on Its Final Voyage

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Welcome to the M219 ocean blog!

Here, we will share updates and stories about the scientific work taking place during this research expedition. We also hope to offer a glimpse into daily life and work at sea.

For many members of the scientific party, this is their first time aboard METEOR. It will also be their last, as METEOR is embarking on its final voyage before retiring from service as a German research vessel after more than 40 years at sea. Over the course of its distinguished career, METEOR has travelled more than 1.7 million nautical miles, which is equivalent to more than 8 times the distance between the Earth and the Moon. Throughout those decades the vessel has supported countless scientific discoveries and generations of marine scientists. We are very grateful and honored to be part of the final chapter of this remarkable ship’s history and to accompany her on the last few thousand miles of her legendary journey.

Planned cruise track for the research expedition M219.

The scientific program of this cruise focuses on long-term observations of ocean currents off the coast of Brazil and at the equator, as well as interdisciplinary measurements near the Cape Verde Islands. At all these sites, GEOMAR has maintained observational programs for the past 10 to 20 years. Over the next four weeks, we will introduce these regions and the measurements carried out there in more detail. But first, let’s look at what happened in Brazil before the cruise began.

On Thursday, May 28, many of the scientists and students left the hotel early in the morning to attend a seminar at the Universidade Federal de Pernambuco (UFPE), celebrating the long-standing scientific collaboration between Brazil and Germany.

The seminar was opened by Prof. Dr. Marius Müller, a former student at GEOMAR and now a professor for biological oceanography at UFPE. These meetings have become a valued tradition, having been organized for more than 20 years by now. This year marked the 9th edition of the seminar since its inception over 20 years ago.

A total of 8 scientists and students from Brazil, Germany, and the U.S. presented their research on various aspects of the tropical Atlantic Ocean. We would like to thank Marius Müller, Doris Veleda and all the Brazilian scientists and students who helped organize the seminar and provided such a warm welcome. We greatly enjoyed the exchange of ideas and look forward to celebrating the 10th seminar in the years to come.

Group picture at the 9th Brazil-German seminar at the Universidade Federal de Pernambuco (UFPE). Photo: Nadja Baumann

After the seminar we returned to the hotel, but there was little time to rest. Later that same day, the captain of METEOR and the German Consul General in Recife hosted a reception aboard METEOR in the Port of Recife.

The event brought together members of the scientific party, representatives of local institutions, and guests from the Brazilian and German scientific communities. It provided an excellent opportunity to celebrate the long-standing partnership between the two countries.

Reception onboard of R/V METEOR to celebrate the German-Brazilian collaboration. Photo: Nadja Baumann

On Friday, May 29, the scientific party finally boarded METEOR. There was little time to settle into our cabins and workspaces, as preparations for departure were already in full swing. We left the Port of Recife as soon as possible and at around 1pm METEOR set sail and began the final voyage of her remarkable career.

About 12 hours after leaving port, we arrived at our first station. Thanks to the dedicated efforts of technical and scientific teams, all instruments had been installed and prepared in time for the start of operations. This station marked the beginning of our observational program off the coast of Brazil, which includes the deployment and recovery of tall moorings as well as CTD measurements. An intensive first week lies ahead, with a demanding schedule of measurements and mooring operations. After months of planning and preparation, everyone is excited to finally begin the scientific work and make the most of the final weeks aboard METEOR.

Leaving the port of Recife on May 29th, 2026. Photo: Peter Brandt

METEOR Sets Sail on Its Final Voyage

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Ocean Acidification

All About Gobies

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There are more than 2,000 species of gobies (Gobiidae) known to science today, making them the largest family of fish in the ocean. But these small creatures are far more complex and essential to marine ecosystems than first meets the eye. Found all around the world in brackish, fresh and salt water in tropical and subtropical regions, they are an astonishingly diverse group of fish with several curious characteristics that set them apart.

Most gobies are quite small and don’t usually measure more than six inches long. Measuring just about eight millimeters long, the dwarf pygmy goby (Trimmatom nanus) is not only the tiniest goby known to science but also one of the smallest of all fish species in the world.

Primarily bottom-dwellers, gobies are known to be excellent foragers and have evolved expert burrowing behaviors over time. As they sift around looking for food like copepods, seaworms and tiny crustaceans, their movement helps to aerate sediment and keep algae in check. Some are even known to be “cleaner fish,” snacking on parasites they remove off larger creatures. It’s like a spa day for the animal being cleaned and a choose-your-own-adventure buffet for the gobies. Studies also show that cleaner goby activity is largely tied to the microbial health of coral reefs, showcasing that even the tiniest of species are essential to functioning marine ecosystems.

Gobies have some unique aspects to their anatomy, too. First, their fused pelvic fins are designed to help them form a strong suction cup to perch on coral reefs, rocks and other ocean terrain amidst turbulent currents. Some freshwater species are even known to use this suction to climb waterfalls. It may come as no surprise then that gobies are cousins to mudskippers, animals known to “walk” through mud. There are more species-specific features that set certain gobies apart. From the use of bioluminescence to symbiotic relationships with shrimp, the adaptations within the goby family are truly wide-ranging. Some species have even been found to use marine terrain memorization to navigate back to the tide pools where they were born. Isn’t nature mind-blowing sometimes?

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Gobies have equally complex and varied behaviors. Male gobies are infamous for being territorial protectors of their nests. Many larger males are known as “guarders;” these hopeful fish make careful nests to attract a mate, and once fertilization occurs, guarders will remain diligently near the nests to keep eggs safe. However, there’s another type of male goby that complicates this dynamic. These other males are known as “sneaker gobies” and are called that for one reason: They’re sneaky! If guarder gobies aren’t careful, sneakers can creep into the nest, fertilize some of the eggs and quickly escape. As if on an underwater episode of Maury, guarder males who aren’t careful could end up unknowingly babysitting little gobies that aren’t their actual offspring.

Gobies serve as indicators of ecological health and are essential to keeping delicate food webs in check. Unfortunately, many changes in our ocean threaten their ability to survive and thrive today. Coral bleaching and degradation endanger the health of one of their key habitats, and a combination of warming waters and coastal development can make it difficult for both juvenile and adult gobies to survive and thrive.

Healthy gobies mean a healthy ocean. Their essential role in marine ecosystems demonstrates that even the tiniest creatures play a major role in helping hold together the beautiful yet fragile habitats that make up our beloved ocean. Visit Ocean Conservancy’s Action Center and join the movement to protect our blue planet today and for years to come—from the tiniest goby to the largest whales, our ocean is counting on us.

Lemon Gobies Inhabit an old bottle

The post All About Gobies appeared first on Ocean Conservancy.

All About Gobies

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