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When I think of worms, I think of going for a walk on a rainy day and seeing (and smelling) the earthworms on the sidewalk exploring their aboveground surroundings. Did you know that worms also live in our ocean? Yes, it’s true. Sometimes, I have a hard time grappling with that fact. Yes, worms do live in the ocean. Marine worms live in nearly all areas of the ocean and are a part of the larger ocean ecosystem. One type of marine worm is the bearded fireworm. It’s brightly colored, which in the wild often means—danger! Let’s learn all about the fireworm.

Bearded Fireworm

Hermodice carunculata

The bearded fireworm is a type of marine bristleworm that belongs to the Amphinomidae family.

Physical appearance

Due to their beautiful, bright red-orange coloring, fireworms are often a favorite for marine photographers. In addition to the red-orange color, fireworms can also be green, yellow or gray in color. Their shape and size look a bit like a centipede. The average size of fireworms is usually between 5-10 centimeters in length, but can reach up to 35 centimeters. Their body has between 60 and 150 separate segments.

Apart from the head and last (or end) body segment, all the other segments are completely identical. Each segment contains two paddles or “legs” called parapodia for swimming, moving around or burrowing. Each segment also has clusters of stinging white bristles and red or orange gills. The mouth is on the bottom side of their second segment. Their head, containing eyes and sensory organs, is on their first segment.

Look, but don’t touch!

Fireworms produce a stinging sensation if touched. Fireworms are covered with fine, white, brittle bristles that break if touched. They are used as a defense mechanism—easily embedding into the skin of whatever predator has come into contact with it.

The bearded fireworm “toxins” produce an intense burning irritation in the area of contact. The sting can also lead to nausea and dizziness. A painful sensation can last up to a few hours after contact. 

Fireworm close-up

Scientists have not yet concluded about what chemical substance is part of the stinging process. Research suggest that they are venomous and use a series of toxins to defend themselves Only time (and more research) will reveal the specifics.

Not a dragon

Fireworm is also a type of dragon from the animated movie and tv show How to Train Your Dragon. The ocean fireworm is not the same as the dragon.

Diet and reproduction

Bearded fireworms are predators. They feed on soft and hard corals, anemones and small crustaceans. They “crawl” on the tip of coral reef branches and feed on the coral tissue, removing it from the coral skeleton. You can tell where a fireworm has been dining because the coral will have a lack of color on the eaten area.

Bearded fireworms are nocturnal, which means they are active during the night and usually hidden during daytime.

Did you know?

Bearded fireworms emit bioluminescence during their mating ritual.

The bearded fireworm can reproduce through both asexual and sexual means. Asexual—their bodies divide into separate parts and regenerate to become new individuals. Sexual—they can reproduce through regular spawning—this typically occurs two to five days after a full moon. Females emit a bioluminscent glow, attracting males to the surface, where they flash their colors as well. As they move toward each other, they shed and combine their sex cells.

Habitat and range

Bearded fireworms can be found near ocean reefs and at depths of up to 500 feet. They are common throughout the tropical western Atlantic as well as the mid-Atlantic. On the eastern side they are found from Algeria to Liberia, and on the western side from the southeast coast of the United States to Guyana, including the Gulf of Mexico and the Caribbean Sea. 

Bearded Fireworm on Vase Sponge

Don’t count on seeing the bearded fireworms at your local aquarium—since they are so hostile, they are usually not held in aquariums.  

Age and population status

Bearded fireworms live between two and three years.

The conservation status of the bearded fireworm is not listed in the International Union for Conservation of Nature database. Their status and population size are unknown. Not enough research has been conducted on this species to know what threatens them.

Part of a healthy ocean ecosystem

Fireworms, like other segmented worms, help in the decomposition process. They convert organic ocean debris into carbon dioxide, which is then used by the plankton to help with photosynthesis.

How you can help coral reefs and the animals who depend on them

It’s up to all of us to help protect marine fireworms, coral reefs and all the animals living in the sea. Ocean Conservancy is working with you to protect the ocean from today’s greatest global challenges. Together, we create evidence-based solutions for a healthy ocean and the wildlife and communities that depend on it.

Please make a donation to Ocean Conservancy—give today and make a difference for the future of our ocean!

The post What is a Bearded Fireworm? appeared first on Ocean Conservancy.

What is a Bearded Fireworm?

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Ocean Acidification

Between Storms and Science: Easter in the Labrador Sea (04.04.26–13.04.26)

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Between all the scientific work, we celebrated Easter on board, although the weather had other plans for us. Due to rough conditions, we weren’t able to carry out any CTD casts.

Photo: Sarah Tomae

Easter itself was spent in a mix of rest and small celebrations. Some of us enjoyed a long Easter breakfast with traditional Easter bread, while others took the opportunity to sleep in. In the evening, we gathered with both crew and scientists for a small celebration. The ship’s cook even organized a quiz, and those who answered correctly were rewarded with Easter chocolate.

The next day, the weather improved, and we began early with the recovery of K1, a 3,495-meter-long mooring in the middle of the Labrador Sea.

We joined the nautical officers on the bridge before sunrise to search for it. Fortunately, K1 has a floating buoy with a light, so we were able to spot it even in the dark. The actual recovery started at first light, and it began to snow while we were working.

Photo: Sarah Tomae, GEOMAR

Amid all the CTDs and mooring operations, there was also a personal highlight: my (Sarah’s) birthday. Although I’ve spent birthdays away from home before, this one felt especially unique, being so far out at sea, with only limited internet contact.

Normally, I work the 4-8 shift, but my incredibly kind shift team gave me the morning off. That meant I could sleep in and even find time to call family and friends back home. In the afternoon, I was surprised with my favourite cake, baked by Julia.

Our work continued with the mooring array at 53°N, which consists of seven moorings. So far, we have recovered five (K7, K8, K9, DSOW1 and DSOW2), and three of them have already been redeployed (K7, K8 and DSOW1,).

Deploying K7 turned out to be particularly tricky. On our first attempt, sea ice drifted toward us faster than expected, forcing us to recover nearly half of the mooring again. While the ship itself can handle drifting ice, deploying a mooring is much more delicate: a long cable with instruments and floats is released behind the ship before the anchor is dropped, allowing the system to sink into place.

Two days later, we tried again and this time, the deployment was successful.

Photo: Sarah Tomae

Afterwards, we moved closer to the sea ice, which was a highlight for many of us. Seeing the ice up close and even spotting a seal swimming nearby, made the experience unforgettable.

Photo: Sarah Tomae
Photo: Sascha Gniosdorz

Due to the continuing harsh weather, the decision was made to return to K1 and make use of an upcoming weather window for deployment the following day.

German:

Zwischen Stürmen und Wissenschaft: Ostern in der Labradorsee (04.04.26 – 13.04.26)

Zwischen all der wissenschaftlichen Arbeit haben wir Ostern an Bord gefeiert, auch wenn das Wetter andere Pläne für uns hatte. Aufgrund der rauen Bedingungen konnten wir keine CTD-Messungen durchführen (Messungen von Leitfähigkeit, Temperatur und Tiefe im Ozean).

Foto: Sarah Tomae

Ostern selbst war eine Mischung aus Erholung und kleinen Feierlichkeiten. Einige von uns genossen ein ausgedehntes Osterfrühstück mit traditionellem Osterbrot, während andere die Gelegenheit nutzten, etwas länger zu schlafen. Am Abend kamen Crew und Wissenschaftler*innen zu einer kleinen Feier zusammen. Der Koch organisierte sogar ein Quiz, und wer die Fragen richtig beantwortete, wurde mit Oster-Schokolade belohnt.

Am nächsten Tag besserte sich das Wetter, und wir begannen früh mit der Bergung von K1, einer 3.495 Meter langen Verankerung mitten in der Labradorsee. (Eine Verankerung ist eine lange, am Meeresboden befestigter Draht, der mit Instrumenten ausgestattet ist, um über längere Zeit Ozeandaten zu messen.)

Noch vor Sonnenaufgang gingen wir mit den nautischen Offizieren auf die Brücke, um nach ihr Ausschau zu halten. Glücklicherweise verfügt K1 über eine schwimmende Boje mit Licht, sodass wir sie bereits im Dunkeln entdecken konnten. Die eigentliche Bergung begann bei Tagesanbruch und es begann sogar zu schneien.

Foto: Sarah Tomae

Zwischen all den CTD-Einsätzen und Verankerungsarbeiten gab es auch ein persönliches Highlight: meinen (Sarahs) Geburtstag. Obwohl ich schon öfter Geburtstage fernab von zu Hause verbracht habe, war dieser besonders, so weit draußen auf dem Meer und mit nur eingeschränktem Internetkontakt.

Normalerweise arbeite ich in der 4-8 Uhr Schicht, aber mein unglaublich nettes Schichtteam hat mir den Morgendienst freigegeben. So konnte ich etwas länger schlafen und hatte sogar Zeit, mit Familie und Freunden zu Hause zu telefonieren. Am Nachmittag wurde ich dann noch mit meinem Lieblingskuchen überrascht, den Julia für mich gebacken hat.

Unsere Arbeit ging weiter mit dem Verankerungs-Array bei 53°, das aus sieben Verankerungen besteht. Bisher haben wir fünf geborgen (DSOW1, DSOW2, K7, K8 und K9), von denen drei bereits wieder ausgebracht wurden (DSOW1, K7 und K8).

Das Ausbringen von K7 erwies sich als besonders schwierig. Beim ersten Versuch trieb das Meereis schneller auf uns zu als erwartet, sodass wir fast die Hälfte der Verankerung wieder einholen mussten. Obwohl das Schiff selbst gut durch treibendes Eis navigieren kann, ist das Ausbringen einer Verankerung deutlich anspruchsvoller: Dabei wird ein langer Draht mit Messinstrumenten und Auftriebskörpern hinter dem Schiff ausgesetzt, bevor am Ende der Anker gelöst wird und das gesamte System absinkt.

Zwei Tage später versuchten wir es erneut, diesmal mit Erfolg.

Foto: Sarah Tomae

Anschließend fuhren wir näher an das Meereis heran, was für viele von uns ein besonderes Highlight war. Das Eis aus nächster Nähe zu sehen und sogar eine Robbe in der Nähe schwimmen zu beobachten, machte das Erlebnis unvergesslich.

Foto: Sarah Tomae
Foto: Sascha Gniosdorz

Aufgrund der weiterhin rauen Wetterbedingungen wurde schließlich entschieden, zu K1 zurückzukehren, um ein bevorstehendes Wetterfenster für die Ausbringung am nächsten Tag zu nutzen.

Between Storms and Science: Easter in the Labrador Sea (04.04.26–13.04.26)

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Humans Just Flew Around the Moon This Week. But Would Babies Born There Ever Truly Feel Gravity? Ask Jellyfish Babies.

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This week, NASA’s Artemis II crew made history by flying around the Moon and returning safely to Earth, the first human journey to the Moon’s vicinity in more than 50 years. It was a stunning reminder that humanity is no longer just dreaming about living beyond Earth. We are actively rehearsing for it.

And that leads to a much stranger, deeper question: even if one day we build skyscrapers on the Moon, raise families there, and turn space into a place to live, will babies born away from Earth develop a normal sense of gravity? Or will their bodies learn the universe differently?

To explore that question, NASA once turned to an unexpected stand-in for human babies: jellyfish babies. On the STS-40 mission, scientists sent thousands of tiny jellyfish polyps into space because jellyfish, like humans, rely on gravity-sensing structures to orient themselves. The experiment asked a simple but profound question: if a living body develops in microgravity, will it still know how to handle gravity later?

The answer was both fascinating and unsettling. The jellyfish developed in space in large numbers, but once back under Earth’s gravity, the ones that had developed in microgravity showed far more pulsing abnormalities than the Earth-grown controls. In other words, their bodies formed, but their sense of balance did not seem to work quite the same way.

That is why this old jellyfish experiment still matters today. Before we imagine lunar cities, schools, nurseries, and generations born off-world, we need to ask not only whether humans can survive in space, but whether developing there changes how the body understands something as basic as up, down, and movement. Jellyfish babies cannot tell us everything about human children, but they may have given us one of the first clues that life born beyond Earth might not come home unchanged.

Reference: https://nlsp.nasa.gov/view/lsdapub/lsda_experiment/0c10d660-6b12-573d-8c3b-e20e071aed3b

Image: GEOMAR, Sarah Uphoff

Humans Just Flew Around the Moon This Week. But Would Babies Born There Ever Truly Feel Gravity? Ask Jellyfish Babies.

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First Week of Cruise MSM142 – Into the Labrador Sea

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After a slight delay of the Maria S. Merian caused by late-arriving containers our research cruise MSM142 finally got underway. By last Tuesday (24.03.2026), the full scientific team had arrived in Nuuk, the capital of Greenland, and the ship reached port on Wednesday (25.03.2026) morning. That same day, scientists and technicians moved on board and immediately began preparations, assembling and testing our instruments. Although the mornings on Wednesday and Thursday were grey and overcast, the afternoons cleared up beautifully. This gave us valuable time to organize equipment on deck and store empty boxes back into the containers before departure.

Foto: Julia Pelle

Given the forecast of harsh conditions outside the fjord, we carried out the mandatory safety drill while still in harbour. This included practicing emergency procedures and boarding the lifeboat. After completing border control, we were finally ready to leave Nuuk. We set sail on March 27th, heading into the Labrador Sea to begin our mission. Even before starting scientific operations, we tested the setup for deploying our gliders without releasing them during the transit out of the fjord. Once we reached open waters, we were met by high waves the following morning. For some on board, this was their first experience under such rough sea conditions. Seasickness quickly became a challenge for a few, while scientific work had to be temporarily postponed due to the strong winds and sea conditions. Together with the crew, we discussed how best to adapt our measurement plans to the given weather conditions. On March 29th, we were finally able to begin our scientific program with the first CTD deployment. A CTD is an instrument used to measure conductivity, temperature, and depth, which are key parameters for understanding ocean structure.  

Foto: Julia Pelle

During the following night, we continued with additional CTD stations and successfully recovered two moorings: DSOW 3 and DSOW 4, located south of Greenland. These moorings carry instruments at various depths that measure velocity, temperature, and salinity. DSOW 4 was redeployed on the same day, while DSOW 3 followed the next day. In addition, the bottles attached to the CTD’s rosette can be used to collect water samples from any desired depth. These samples can be used, for example, to determine the oxygen content, nutrient levels, and organic matter.

Foto: Julia Pelle

Both are part of the OSNAP array, a network of moorings spanning the subpolar North Atlantic. On these moorings are a few instruments, for example microcats which measure temperature, pressure and salinity.

We then conducted around 25 CTD stations spaced approximately 3 nautical miles apart across an Irminger ring identified from satellite data. This high-resolution sampling was necessary to capture the structure of an Irminger Ring, which had a radius of about 12 km wide.

Foto: Julia Pelle

The days leading up to April 2nd were marked by very rough weather conditions. Life on board became both challenging and, at times, unintentionally entertaining sliding chairs were not uncommon. During the night from April 1st to April 2nd, winds reached 11 Beaufort with gusts up to 65 knots, forcing us to pause our measurements. Fortunately, conditions improved by morning, allowing us to resume our work. As well as with the help of the crew we had to adapt to the harsh weather conditions to continue our scientific work. On the 3rd of April, we were able to deploy a few gliders and one float. An ocean glider is an autonomous underwater Vehicle, which you can steer remotely and send to different locations, while it is measuring oceanographic key parameters.

Foto: Julia Pelle

This research cruise focuses on understanding small-scale processes in the ocean and their connection to the spring bloom, an essential phase in marine ecosystem in subpolar regions. Despite the challenging start, we have already gathered valuable data and look forward to the weeks ahead in the Labrador Sea. 

First Week of Cruise MSM142 – Into the Labrador Sea

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