During a 2018 expedition aboard R/V Falkor, Drs. David Caress, Ron Spelz-Madero, Raquel Negrete-Aranda, and Victoria Orphan, alongside a team of interdisciplinary researchers and engineers, explored the recently discovered Auka Vent Field. The Auka Vent field is a series of hydrothermal vents located in Pescadero Basin, one of several small ocean basins in the tectonically active Gulf of California (GOC). While mapping, exploring, and sampling Auka with ROV SuBastian, the team deployed seafloor mapping AUVs to explore other parts of the basin. The AUV data revealed another new hydrothermal vent field, which they named JaichMaa ’jag, a term from the indigenous Kiliwa people in the GOC that roughly translates to “Liquid Metal”. The name refers to an underwater cavern with hot fluid pooled at the ceiling creating a reflective surface like an upside-down lake, which was unveiled within a chimney in the new vent field. The work contributed to a growing body of research determining the hydrothermal vents in the Pescadero Basin are distinct from other known vent systems, from the minerals they emit to the animals that live on them. In September 2021, the researchers will return to further their interdisciplinary investigation of the Gulf of California. They plan to map the neighboring Carmen and Farallon Basins, characterize heat flow in the Pescadero Basin, and examine hydrothermal vent microbiology and ecology in the Auka and JaichMaa ’ja’ag fields in order to further our understanding of these recently discovered hydrothermal systems.

The Gulf of California 
The Gulf of California (GOC) is a relatively young feature of our planet. Its formation is estimated to have started ~12.5 million years ago when Baja California began to break away from the North American continent. The GOC is the northernmost portion of the East Pacific Rise, a mid-ocean ridge that extends down to Antarctica. Several tectonic plates move away from the Pacific Plate along the East Pacific Rise, creating a spreading center. Spreading centers are tectonic boundaries where new crust (the outermost layer of our planet) forms. The Gulf of California spreading varies from the rest of the East Pacific Rise because it is where the North American Plate begins to move alongside the Pacific Plate, transitioning into a transform fault. The transform motion dominates farther north and is known as the San Andreas fault system. 

The movement results in both spreading and sliding between the two plates and, over time, have opened up four deep ocean basins known as the Guaymas, Carmen, Farallon, and Pescadero Basins. Guaymas and Pescadero basins contain documented hydrothermal vents, but there has been little exploration and mapping of the Carmen and Farallon Basins. Leg One of the expedition will focus on multibeam mapping the Carmen and Farallon Basins to better characterize these geologic features and inform future scientific endeavors in the region. Mapping the Carmen and Farallon basins will also aid in understanding the opening of the Southern Gulf of California, as the science team searches for features affiliated with the opening of the Gulf.   

Hydrothermal Vents in the GOC
The hydrothermal vents in the Pescadero Basin vary significantly from other known vent communities physically, chemically, and ecologically. The temperature, chemical make-up, and animals that live on these vents are unlike vents found in other parts of the world. Due to the shape and surrounding land, the GOC facilitates heavy sedimentation of the Pescadero Basin. Debris runs into the basin from surrounding watersheds, and organic matter sinks to the bottom from photosynthetic organisms living in the surface waters. Most hydrothermal vent communities exist in deeper, offshore regions that do not experience sediment build-up. This sedimentation affects the chemistry and make-up of the hydrothermal vents. The vents observed in Pescadero Basin are uniquely composed of hydrothermal carbonates and clear, shimmering water around 290 degrees Celsius. These fluids have a higher pH and produce calcite-rich mineral deposits rather than the sulfides of more commonly observed vents. Hot water reacting with sediment forms organic gases and hydrothermal petroleum, a process that usually requires deep burial of organic-rich sediment and millions of years. 

Leg Two of the expedition will concentrate on heat flow of the hydrothermal vents and their surrounding areas. ROV SuBastian will be fitted with a temperature probe, and the scientists will take measurements at intervals starting near the vents and then moving away to create heat flow profiles. Mapping heat flow is essential for understanding hydrothermal circulation (the movement of hydrothermal fluids around the basins and GOC) and thermally-driven processes. 

Communities of the Pescadero Basin Vents 
No light penetrates to the bottom of the Pescadero Basin. Instead of relying on photosynthesis as the basis of the food web, microbes living on hydrothermal vents generate energy through chemical energy or ‘chemosynthesis’. The microbes in the Pescadero Basin use diverse sources of chemical energy including methane and hydrocarbons, as well as hydrogen and hydrogen sulfide gases dissolved in the hydrothermal fluid. Extremophilic microbes persist throughout the vent environment and are adapted to a large range of temperatures from above boiling point of water to the frigid cold temperatures of the deep sea. Some microbes are adapted to living in symbiosis with animals like tubeworms and anemones, while others live within chemical-rich sediments or exist endolithically, living within the interior of hydrothermal minerals. During Leg Three of the expedition, the scientists will document the diversity of different extremophilic microbes living across steep temperature gradients on and around the Pescadero Basin vents and characterize the menu of chemical compounds they use to create energy and grow

Alongside characterizing the microbial communities, the scientists will also investigate the larger animals living near the vents during Leg Three of the expedition. The 2018 expedition revealed that three primary animals are foundational within the Auka and JaichMaa ’ja’ag vents: a species of tubeworm, a blue scale worm, and a chemosynthetic anemone. The anemone is the first-ever cnidarian documented to have a symbiotic relationship with microbes and rely on chemosynthesis. In addition to examining the known animals, the scientists hope to find new species living around Pescadero Basin hydrothermal vents.

A map of the Carmen, Farallon, and Pescadero basins located in the Gulf of California. The red box indicates the study area of the expedition.
ROV SuBastian exploring a cavernous chamber formed by repeated, layered mineralization and collapse events.
ROV SuBastian collects a sample of bacterial mat on the seafloor. The presence of microbial mat indicates vent fluid seeping out of the seafloor.
A tall chimney in JaichMaa, a new hydrothermal vent field discovered during this cruise in the southern Pescadero Basin.
Mysterious blue microbes on the Auka hydrothermal vent dubbed “The Matterhorn”.
Clump of the tube worm Oasisia, unusually common in the Pescadero vent fields, surrounding a lone Riftia tube worm.
These vent fields have distinctive compositions of their fluids that result from interaction with the sediment that covers the volcanic heat sources below. These vent fields are almost entirely made of one mineral, calcite.
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Cruise Log

No cruise log entries at this time.

Data & Publications

All voucher material of animals collected during the cruise is accessioned into the Scripps Institution of Oceanography – Benthic Invertebrate Collection.

The resulting shipboard dataset is being archived at Rolling Deck to Repository and is now available.

Genetic data analyses results are being made publicly available on Dr. Goffredi’s webpage, but will be archived at GenBank soon.

ADCP data is curated and archived by University of Hawaii.

Deep-sea anemone associated microbiome (describing a new chemosynthetic symbiosis between the sea anemone Ositioctis pearseae and introcellular bacteria) data is archived at NCBI.

You can search Nucleotide Accension Numbers here. Accension numbers are: MW148236, MS148237, MW148238, MW158740, MW165066, MW172213, MW172214 and MW172220, MW172221.

  • Cruise Report: Interdisciplinary Investigation of a New Hydrothermal Vent Field
  • Paduan, J., et. al. (2019). Mapping Pescadero Basin Hydrothermal Vent Fields at Multiple Scales. Poster Presentation at AGU Fall Meeting, San Francisco, CA, USA.
  • Caress, D., et al. (2019). Use of 1-m Scale AUV and 1-cm Scale ROV Surveys to Guide Exploration and Sampling of the Auka Hydrothermal Vent Field, South Pescadero Basin, Gulf of California. Poster Presentation at AGU Fall Meeting, San Francisco, CA, USA.
  • Orphan, V., et. al. (2019). Genomic Diversity and Microbial Activities Fueled by Deep Fluids. Poster Presentation at AGU Fall Meeting, San Francisco, CA, USA.
  • Negrete-Aranda, R., et. al. (2019). First Heat Flow Measurements in the Auka and JaichMaa ja'ag vent fields, Pescadero Basin, Southern Gulf of California. Poster Presentation at AGU Fall Meeting, San Francisco, CA, USA.
  • Hatch, A., Liew, H., Hourdez, S., and G. Rouse. (2020). Hungry scale worms: Phylogenics of Peinaleopolynoe (Polynoidae, Annelida), with four new species. Zookeys 932:27-74, doi: 10.3897/zookeys.932.48532.
  • Goffredi, S., Motooka, C., Fike, D., Gusmao, L., Tilic, E., Rouse, G., and Rodriguez, E. (2021). Mixotrophic chemosynthesis in a deep-sea anemone from hydrothermal vents in the Pescadero Basin, Gulf of California. BMC Biology, 19(8), doi: 10.1186/s12915-020-00921-1. [This article has been published as OPEN ACCESS].
  • Speth, D., Yu, F., Connon, S., Lim, S., Magyar, J., Pena, M. et al. (2021). Microbial community of recently discovered Auka vent field sheds light on vent biogeography and evolutionary history of thermophily. BioRxiv, doi: 10.1101/2021.08.02.454472. [This article has been published sas OPEN ACCESS].

Live ROV Footage

ROV SuBastian live footage from Pescadero Basin in the Gulf of Baja.

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