Alvin, Please Deploy My Trap There

Guest blog post by postdoc Johanna Weston

Today, I am coming to you from the Central East Pacific near 9°50’ North. I am on board R/V Atlantis along the East Pacific Rise as part of an NSF-funded cruise to study the biodiversity of inactive sulfide vents. Or, as we are saying – Life After Vents.

The East Pacific Rise (EPR) is a mid-ocean rise at a divergent tectonic plate boundary and a fast-spreading mid-ocean ridge. Along this axis, there is a lot of hydrothermal venting activity. However, this venting is ultimately transient, leaving only the sulfide mineral-rich deposits after the fluid flow stops. These inactive sulfides are beautiful and distinct features on the seafloor. They aren't teeming with the iconic life present on active vents, but they are not devoid of life either.

I spent January and February on a team, led by Dr. Lauren Mullineaux from WHOI and Dr. Jason Sylvan from Texas A&M, exploring some inactive sulfides. We are using the human-occupied submersible (HOV) Alvin to image, collect animals living on the rocks, and retrieve rocks! This is my first experience working with Alvin or a vehicle with manipulator arms. From planning sample collection, sorting samples, diving in Alvin, and seeing the deep ocean with my own eyee, this experience has been formative as a deep-ocean scientist.

One element that has transformed my thinking is the ability to choose where and when samples are collected. This concept is novel because my PhD focused on the ocean's deepest zone – the hadal zone. The hadal zone is depths from 6,000 to nearly 11,000 m at Challenger Deep in the Mariana Trench. For reference, the depth of the EPR is ~2500 m. Studying the hadal zone is even more challenging than other parts of the deep ocean due to these extreme depths. Our primary tool for biological sampling is autonomous free-landers with traps baited with smelly fish, like mackerel, to attract andhopefully catch scavengers. The scavengers that I focused on were amphipods, a type of crustacean. We had a targeted depth. But they landed where they landed.

As part of this cruise, I used two baited traps to examine the scavenging amphipod community of the active and inactive vents. Both baited traps have a similar design – a PVC tube with a funnel and a cap and mesh on the other. One trap was mounted on a lander. This lander was deployed for 24 hours, carried a McLane Pump to sample live larvae in the water column for a pressure chamber experiment onboard, and was placed on the edge of a vent by Alvin. The second trap was deployed and recovered by Alvin – and has lovingly been named the Amphipod Handbag. The Handbag is the same tube and funnel design but modified with weights on the horizontal side to keep it weighted down and a rope handle for Alvin's manipulator arm to set it down and pick it up. While the design is simple, plenty of thought went into making sure the Handbag fit into a biobox with the lid closed, it laid down nicely, and the trap was vertical when picked up. Also, the exciting part was deciding where precisely to place the Handbag – like on the edge of a Riftia bush and mussel bed and at the top of Lucky's Mound – to capture a different niche than the trap on the lander. Excitingly and primarily, I spotted differences across deployments and potentially even a new species.

My highlight happened on January 26, 2024, when I was the starboard observer on Alvin Dive 5224 to an inactive vent called Lucky's Mound. I got to see with my own eyes the deep ocean and deploy and recover the Handbag. Seeing the deep seafloor after many years of thinking about it was utterly magical, profound, and nearly indescribable. Beautiful, alive, and so complex. Truly, it was a privilege to see this small part of the deep ocean in person. This experience's mark on me will likely propel the questions I ask for the rest of my career.

As the cruise winds down and we steam to Costa Rica, I am reflecting on my growth thanks to Alvin and its Amphipod Handbag. More importantly, I am ready to get back to WHOI and uncover the results and meaning of this new data.


The EPR Biofilms4Larvae project is support by a multi-institutional NSF grant: OCE-1948580 (Arellano), OCE-1947735 (Mullineaux), OCE-1948623 (Vetriani).

The Inactive Sulfides project is support by a multi-institutional NSF grant: OCE-2152453 (Mullineaux & Beaulieu) and OCE-2152422 (Sylvan & Achberger).


Wide view of the first deployment of the Amphipod Handbag deployed by Alvin at the base of a Riftia bush (tube worms) at an active vent named Tica Mound. Credit: Shawn Arellano, Chief scientist, Western Washington University; Alvin Operations Group; National Science Foundation; ©Woods Hole Oceanographic Institution

Wide view of the deployment of the Amphipod Handbag deployed by Alvin near the top of the inactive sulfide feature named Lucky’s Mound. Credit: Shawn Arellano, Chief scientist, Western Washington University; Alvin Operations Group; National Science Foundation; ©Woods Hole Oceanographic Institution

Zoomed photo of the first deployment of the Amphipod Handbag with an eelpout looking on. Credit: Shawn Arellano, Chief scientist, Western Washington University; Alvin Operations Group; National Science Foundation; ©Woods Hole Oceanographic Institution

Looking on to the recovery of the Amphipod Handbag by Alvin. Credit: Shawn Arellano, Chief scientist, Western Washington University; Alvin Operations Group; National Science Foundation; ©Woods Hole Oceanographic Institution

Wave goodbye at the Alvin hatch before the commute to work on the seafloor. Credit: Costantino Vetriani.


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