As previously summarized by Hammond et al. (2015), from 1983 to 2013, the NOAA Vents program conducted systematic and multidisciplinary exploration, discovery, and research related to hydrothermal vents, submarine volcanic eruptions, and associated ocean physical, chemical, and biological processes. In 2014, Vents divided into two programs, Earth-Ocean Interactions (EOI) and Acoustics, and considered a broader range of questions about how seafloor and subseafloor processes contribute to ocean health, biogeochemical cycles, ecosystem diversity, and climate change. Here, we highlight major accomplishments since 2014, including deep-sea technologies that EOI, Vents, and Pacific Marine Environmental Laboratory (PMEL) Engineering have developed to advance marine science. EOI research is driven by a need for better observational data on issues of global importance, including the role of continental margin seeps in the global methane/carbon cycle, benthic ecology, and fisheries habitat; the role of hydrothermal systems in global biogeochemical cycles, including carbon dioxide removal; the potential impact of deep-sea mining of metal sulfides on ecosystem services provided by hydrothermal vents; and how hydrothermal iron functions as an essential nutrient. NOAA Ocean Exploration, the Schmidt Ocean Institute, the Ocean Exploration Trust, and the National Science Foundation have supported and collaborated in this work. Global exploration of the deep sea with the purpose of understanding global ocean processes remains a cornerstone of EOI science.

 

Photo of the midsection of a metal sulfide chimney, 1970 m depth, at Puy des Folles volcano, Mid-Atlantic Ridge, from ROV SuBastian dive 500, April 2, 2023. Abundant vent fish (Zoarcidae), shrimp (Alvinocaridae), limpets (Lepetodrilidae), and crab (Bythograeidae) are seen on the oxidized (orange) and bacterial mat-covered (white) surfaces of this diffusely active hydrothermal vent. © Schmidt Ocean Institute. > High res figure

 

Continental Margin Seeps: Exploration, Characterization, and Research

Seeps have been known on the Cascadia Margin since the 1990s (Suess et al., 1999; Rehder et al., 2002; Collier and Lilley, 2005; Heeschen et al., 2005), but the pace of discovery of gas seeps increased greatly when the application of sonar backscatter for detecting gas bubbles in the water column revealed that seeps are ubiquitous on the continental shelf and slope (Riedel et al., 2018; Johnson et al., 2019; Merle et al., 2021). Several EOI-led cruises since 2016 (Figure 1) have been instrumental in systematically mapping and characterizing methane seeps within the US Cascadia Margin, resulting in a foundational database and inventory of nearly 3,500 bubble seep locations, grouped into over 1,300 seep sites, at water depths ranging from 100 m to >2,000 m (Merle et al., 2021). The mapping coverage represented in this database is still only ~40% of the entire Cascadia Margin seafloor area, so many thousands more seeps are likely present. Seeps release methane into the water column, create carbonate hard ground habitat, and host the conversion of chemosynthetic energy into biomass that radiates into the benthic environment (Levin et al., 2016), raising the importance of exploration and characterization of coastal margin seeps. Merle et al. (2021) found a high incidence of gas plumes on the shelf in water shallower than 200 m. The shelf remains largely un-surveyed for bubble plumes, so it is likely that many more seep sites will be located in the future at shallow depths where methane is more likely to reach the atmosphere (Michel et al., 2021).

 

FIGURE 1. Earth-Ocean Interactions (EOI) Program field projects, 2014–2023. (a) Map of field research areas for EOI 2014–2023. White text indicates geographical areas of research. White circles indicate areas where remotely operated vehicle (ROV) dives were conducted. Red text and red triangles mark sites of volcanic eruptions investigated by EOI. Blue text and blue lines show cruise tracks and cruise names. (b) Timeline of PMEL/EOI research expeditions from 2014 to 2023. Dark gray text denotes cruises led by EOI. Blue denotes cruises with significant participation by EOI. During this time, EOI scientists logged >2,500 person-days at sea on 24 research cruises with 661 ship days. Symbols and location names show the timing of volcanic eruptions discovered and/or studied by EOI. > High res figure

 

EOI has contributed to the exploration, enumeration, and characterization of methane seeps along the Cascadia Margin (Figure 2) by organizing and leading cruises (Figure 1) and publishing results on the distribution of seeps (Merle et al., 2021; Johnson et al., 2022), the chemical and isotopic compositions of seep gases and their origins (Baumberger et al., 2018), the variation of microbial communities across seep sites (Seabrook et al., 2018), and the acoustic signatures of seeps (Dziak et al., 2018). A survey of methane on the 2021 NOAA West Coast Ocean Acidification cruise indicates that methane from seeps reaches the surface ocean over the continental shelf and upper slope (Butterfield et al., 2022), contributing to the marine methane flux to the atmosphere.

EOI has contributed to technology development for understanding seeps with a new gas-tight methane hydrate sampler (Figure 2d; Lupton et al., 2018) and field testing of a deep-sea laser spectrometer built by Opto-Knowledge Systems Inc. for in situ methane analysis. EOI work on Cascadia Margin has primarily been supported by the NOAA Office of Ocean Exploration (OE) and PMEL in partnership with the Ocean Exploration Trust (OET), using OET’s E/V Nautilus and its remotely operated vehicle (ROV) Hercules. OET prioritizes public education and outreach, as well as making data widely available, so these EOI cruises and discoveries have received significant media and public interest while contributing substantially to national data repositories.

 

FIGURE 2. ROV Hercules photos show representative images of Cascadia Margin seeps taken during E/V Nautilus expeditions. (a) A vigorous methane bubble release from a 700 m deep pit at the Coquille site was imaged during NA095 in 2018. The pit was 2 m deep and 4 m in diameter. Its walls were coated by a mix of hydrate and white bacterial mats. (b) White and orange bacterial mats at the active methane seep site SW Heceta Bank at 1,235 m water depth were captured during expedition NA095 in 2018. (c) Temperature is measured in a clam bed surrounded by brittle stars at the warm seep site NW Coquille Seamount at 1,765 m water depth during NA128 in 2021. (d) Hydrate samples were collected using a gas-tight sampler at a methane hydrate outcrop with active bubble release in Astoria Canyon at 757 m water depth during NA128 in 2021. > High res figure

 

The diversity of Cascadia methane seeps is still being uncovered, and given that only ~30 of the thousands of seep sites have been visited and sampled by human-occupied vehicles (HOVs) or ROVs, there is much more to explore and discover. Correlation between an anomaly in the deep subseafloor structure, from 2021 R/V Langseth seismic reflection data and the distribution of seep locations from acoustic water column data, led to the discovery of a rarely observed warm seep at the base of the continental slope ~15 km east of the Cascadia deformation front offshore southern Oregon (Beeson et al., 2022). The warm seep implies that the fluids are rising from deep within the continental margin, probably along an active fault. An open question for future studies is to determine how common or rare such warm seep sites may be and if monitoring them may provide valuable information about tectonic stresses and earthquake potential within the subduction zone (Phillip et al., 2023).

 

Hydrothermal Vents and Submarine Volcanoes

EOI contributes to exploration, discovery, and research on seafloor hydrothermal vents and volcanic processes (Figure 1). Data from instruments built by PMEL and installed as part of the Ocean Observatories Initiative (OOI) network led to the successful forecast of an eruption at Axial Seamount (Juan de Fuca Ridge, Northeast Pacific Ocean) in 2015, and previously scheduled field work allowed for characterization of the new lava flow and changes in hydrothermal discharge (Chadwick et al., 2016; Baker et al., 2019).

Exploration of the Mariana back-arc basin from R/V Falkor in 2015 (one of many collaborations with the Schmidt Ocean Institute) resulted in the detection of plumes from 13 previously undocumented vent sites (Baker et al., 2017). Subsequent NOAA Ship Okeanos Explorer/ROV Hercules and Schmidt Ocean Institute R/V Falkor/ROV SuBastian dives in 2016 at four of the newly detected hydrothermal areas, including a recent and still-cooling back-arc lava flow (Chadwick et al., 2018) and a large high-temperature vent field at 17°N (Figure 3), provided essential data for comparing the biology and geochemistry of arc and back-arc settings (Brunner et al., 2022).

 

FIGURE 3. The Hafa Adai vent field, at 3,300 m depth near 16.96°N, 144.87°E in the Mariana back-arc basin, was discovered in 2015 and surveyed in 2016. (a) A bathymetric map of the vent field shows ROV dive tracks and locations of six active vents. (b) A vertical surface on the side of Sequoia chimney supporting representative fauna including shrimp, limpets, snails, and crab was imaged during dive S43 on December 9, 2016. (c) Active black smokers at the top of Two Towers chimney were photographed during dive S41 on December 7, 2016. Photos © Schmidt Ocean Institute. > High res figure

 

In March–April, 2023, an EOI-led team of international researchers employed water column surveys, high-​resolution bathymetric mapping with two Monterey Bay Aquarium Research Institute autonomous underwater vehicles, and ROV dives during the inaugural expedition of the new Schmidt Ocean Institute R/V Falkor (too) to explore three target areas along the Mid-Atlantic Ridge. The FKt230303 expedition (https://schmidtocean.org/​cruise/​in-​search-​of-​hydrothermal-​lost-​cities/​cruise-log) discovered three new high-temperature hydrothermal systems between 20°N and 25°N, including vents on two off-axis oceanic core complexes and one on-axis volcano. The only active hydrothermal areas previously known in this section of the Mid-Atlantic Ridge, Snake Pit and the Trans-Atlantic Geotraverse (TAG) field, were both discovered in 1985.

With mounting pressure to supply critical minerals for electric vehicles and other technology as the climate crisis intensifies, there is an ongoing debate about the need for, the economic feasibility of, and the degree of environmental harm to be expected from deep-sea mining of hydrothermal mineral deposits and manganese nodule deposits. Continuing to gather scientific data about deep-sea hydrothermal sites is of primary importance in order to understand the ecosystem services they provide and to develop science-​based environmental management plans to protect ocean health and regulate deep-sea mining (Boschen et al., 2016).

Most metals exiting the seafloor at hydrothermal vents form near-field mineral deposits (e.g., mounds and chimneys) or precipitate and settle to the seafloor close to their sources. However, hydrothermal iron is transported more than 4,000 km west from the southern East Pacific Rise across the south Pacific Ocean basin (Resing et al., 2015) in a plume that aligns with the well-documented hydrothermal helium (³He) plume (Lupton and Craig, 1981; Lupton, 1998). Iron is an important, and often limiting, micronutrient for primary production in the surface ocean, and hence, has a significant role in converting CO₂ to particulate carbon and exporting it to the seafloor. Characterizations of the distribution and magnitude of hydrothermal iron sources (Resing et al., 2015; Baker et al., 2016; Buck et al., 2018) and transport mechanisms (Wang et al., 2021; Tagliabue et al., 2022b; Lough et al., 2023) are critical factors in modeling how and where primary productivity depends on hydrothermal iron, and improved understanding of these factors could help evaluate the feasibility of ocean iron fertilization as a CO₂ removal mechanism. Modeling studies connect hydrothermal iron to primary production and the global carbon cycle, especially in the Southern Ocean where hydrothermal iron may be responsible for 15%–30% of the export production south of the Polar Front (Resing et al., 2015; Tagliabue and Resing, 2016). Modeling also predicts that hydrothermal venting in or near the Southern Ocean is likely to be the most important source area of hydrothermal iron for carbon export (Tagliabue and Resing, 2016). This model prediction is supported by recent observations of elevated iron and manganese above the Pacific-Antarctic Ridge crest (Tagliabue et al., 2022a). The discovery of hydrothermal activity on the Australian-Antarctic Ridge (Hahm et al., 2015), combined with the presence of this venting below a massive phytoplankton bloom in the surface Southern Ocean (Schine et al., 2021), has inspired an expedition to this region by EOI scientists and collaborators that is scheduled for 2025. Its objective is to definitively link hydrothermal venting and primary productivity in the Southern Ocean.

Deep-sea exploration contributes to understanding how seafloor processes impact ocean biogeochemistry, support sustainable resources, pose potential hazards to coastal communities, and contribute to the accumulation or removal of greenhouse gases in the atmosphere. Most of the seafloor is still unexplored, including large tracts of the US exclusive economic zone and most of the Southern Ocean. The submarine portions of the Aleutian arc, where there are many active subaerial volcanoes, have been neither mapped with sufficient resolution nor systematically surveyed for submerged hydrothermal/volcanic activity. The territories of the Northern Mariana Islands, American Samoa, and the US Virgin Islands are all located near submarine arc volcanoes, many of which were shown to be active through Vents and EOI explorations. The massive eruption of the Hunga Tonga-Hunga Ha’apai volcano in January 2022, and resulting tsunamis, highlighted the importance of understanding the hazards posed by submarine arc volcanoes with summits near the sea surface, as well as the role of shallow eruptions in stimulating ocean productivity (Bonnet et al., 2023). The PMEL EOI program aims to continue to explore and contribute to the development of innovative technology and ocean/​seafloor observation methods to address current and emerging issues of scientific and societal importance.

 

Acknowledgments

Over the years, the Earth-Ocean Interactions Program has benefited from the talents of Ed Baker, Bob Embley, John Lupton, Steve Hammond, Nathan Buck, Camilla Wilkinson, Leigh Evans, Hoang-My Christensen, Susanna Michael, Bob Dziak, Chris Meinig, Noah Lawrence-Slavas, Marv Lilley, Ben Larson, Dave Clague, Dave Caress, Cornel de Ronde, Craig Moyer, Verena Tunnicliffe, Julie Huber, and many others. Thanks to Sarah Battle and Sandra Bigley for their work on graphics. This publication is partially funded by the Cooperative Institute for Climate, Ocean, and Ecosystem Studies under NOAA Cooperative Agreement NA20OAR4320271, Contribution No. 2023-1305, PMEL contribution number 5525. Research funding provided by Pacific Marine Environmental Lab, NOAA Ocean Exploration, Schmidt Ocean Institute, National Science Foundation, and the Ocean Exploration Trust.

Butterfield, D.A., S.L. Walker, T. Baumberger, J. Beeson, J. Resing, S.G. Merle, A. Antriasian, K. Roe, G.-S. Lu, P. Barrett, and W.W. Chadwick Jr. 2023. The PMEL Earth-Ocean Interactions Program: Beyond vents. Oceanography 36(2–3):206–211, https://doi.org/10.5670/oceanog.2023.229.

Baker, E.T., J.A. Resing, R.M. Haymon, V. Tunnicliffe, J.W. Lavelle, F. Martinez, V. Ferrini, S.L. Walker, and K. Nakamura. 2016. How many vent fields? New estimates of vent field populations on ocean ridges from precise mapping of hydrothermal discharge locations. Earth and Planetary Science Letters 449:186–196, https://doi.org/10.1016/​j.epsl.2016.05.031.

Baker, E.T., S.L. Walker, J.A. Resing, W.W. Chadwick Jr., S.G. Merle, M.O. Anderson, D.A. Butterfield, N.J. Buck, and S. Michael. 2017. The effect of arc proximity on hydrothermal activity along spreading centers: New evidence from the Mariana back-arc (12.7°–18.3°N). Geochemistry, Geophysics, Geosystems 18(11):4,211–4,228, https://doi.org/​10.1002/2017GC007234.

Baker, E.T., S.L. Walker, W.W. Chadwick Jr., D.A. Butterfield, N.J. Buck, and J.A. Resing. 2019. Post-eruption enhancement of hydrothermal activity: A 33-year, multi-eruption time series at Axial Seamount (Juan de Fuca Ridge). Geochemistry, Geophysics, Geosystems 20(2):814−828, https://doi.org/​10.1029/2018GC007802.

Baumberger, T., R.W. Embley, S.G. Merle, M.D. Lilley, N.A. Raineault, and J.E. Lupton. 2018. Mantle-derived helium and multiple methane sources in gas bubbles of cold seeps along the Cascadia Continental Margin. Geochemistry, Geophysics, Geosystems 19(11):4,476–4,486, https://doi.org/​10.1029/2018GC007859.

Beeson, J., T. Baumberger, S.G. Merle, A. Antriasian, A. Trehu, D. Butterfield, N. Buck, G. Lu, S.L. Walker, K. Roe, and others. 2022. Fluid flow within the shallow forearc of the Cascadia Subduction Zone: Seismic imaging, high-resolution ROV mapping, and gas/fluid geochemistry. Abstract T32E-0192 presented at 2022 Fall Meeting of the American Geophysical Union, Chicago, IL, December 12–16, 2022.

Bonnet, S., C. Guieu, C. Tilliette., C. Boulart, P.E. Bouruet-Aubertot, F. Gazeau, C. Scalabrin, M. Bressac, A.N. Knapp, Y. Cuypers, and others. 2023. Natural iron fertilization by shallow hydrothermal sources fuels diazotroph blooms in the ocean. Science 380(6647):812–817, https://doi.org/​10.1126/​science.abq4654.

Boschen, R.E., A.A. Rowden, M.R. Clark, and J.P.A. Gardner. 2016. Mining of deep-sea seafloor massive sulfides: A review of the deposits, their benthic communities, impacts from mining, regulatory frameworks and management strategies. Ocean and Coastal Management 84:54–67, https://doi.org/10.1016/j.ocecoaman.2013.07.005.

Brunner, O., C. Chen, T. Giguère, S. Kawagucci, V. Tunnicliffe, H.K. Watanabe, and S. Mitarai. 2022. Species assemblage networks identify regional connectivity pathways among hydrothermal vents in the Northwest Pacific. Ecology and Evolution 12:e9612, https://doi.org/10.1002/ece3.9612.

Buck, N.J., J.A. Resing, E.T. Baker, and J.E. Lupton. 2018. Chemical fluxes from a recently erupted shallow submarine volcano on the Mariana Arc. Geochemistry, Geophysics, Geosystems 19(5):1,660–1,673, https://doi.org/​10.1029/​2018GC007470.

Butterfield, D.A., C. Zwiers, J. Sharp, R. McCabe, C. Mahoney, R. Feely, B. Carter, D. Greeley, S. McAllister, and T. Baumberger. 2022. Dissolved methane and air-sea flux in coastal waters from Queen Charlotte Sound to southern California. Abstract OB09 presented at the Ocean Sciences Meeting, February 27–March 14, 2022 (virtual).

Chadwick, W.W. Jr., B.P. Paduan, D.A. Clague, B.M. Dreyer, S.G. Merle, A.M. Bobbitt, D.W. Caress, B.T. Philip, D.S. Kelley, and S.L. Nooner. 2016. Voluminous eruption from a zoned magma body after an increase in supply rate at Axial Seamount. Geophysical Research Letters 43(23):12,063–12,070, https://doi.org/​10.1002/2016GL071327.

Chadwick, W.W. Jr., S.G. Merle, E.T. Baker, S.L. Walker, J.A. Resing, D.A. Butterfield, M.O. Anderson, T. Baumberger, and A.M. Bobbitt. 2018. A recent volcanic eruption discovered on the central Mariana back-arc spreading center. Frontiers in Earth Science 6:172, https://doi.org/10.3389/feart.2018.00172.

Collier, R., and M.D. Lilley. 2005. Composition of shelf methane seeps on Cascadia continental margin. Geophysical Research Letters 32(6), https://doi.org/​10.1029/2004GL022050.

Dziak, R.P., H. Matsumoto, R.W. Embley, S.G. Merle, T.-K. Lau, T. Baumberger, S.R. Hammond, and N. Raineault. 2018. Passive acoustic records of seafloor methane bubble streams on the Oregon continental margin. Deep Sea Research Part II 150:210–217, https://doi.org/10.1016/j.dsr2.​2018.04.001.

Hahm, D., E.T. Baker, T.S. Rhee, Y.-J. Won, J.A. Resing, J.E. Lupton, W.-K. Lee, M. Kim, and S.-H. Park. 2015. First hydrothermal discoveries on the Australian-Antarctic Ridge: Discharge sites, plume chemistry, and vent organisms. Geochemistry, Geophysics, Geosystems 16(9):3,061–3,075, https://doi.org/​10.1002/​2015GC005926.

Hammond, S.R., R.E. Embley, and E.T. Baker. 2015. The NOAA Vents Program 1983 to 2013: Thirty years of ocean exploration and research. Oceanography 28(1):160–173, https://doi.org/​10.5670/oceanog.2015.17.

Heeschen, K.U., R.W. Collier, M.A. de Angelis, E. Suess, G. Rehder, P. Linke, and G.P. Klinkhammer. 2005. Methane sources, distributions, and fluxes from cold vent sites at Hydrate Ridge, Cascadia Margin. Global Biogeochemical Cycles 19(2), https://doi.org/10.1029/2004GB002266.

Johnson, H.P., S. Merle, M. Salmi, R. Embley, E. Sampaga, and M. Lee. 2019. Anomalous concentration of methane emissions at the continental shelf edge of the Northern Cascadia Margin. Journal of Geophysical Research: Solid Earth 124(3):2,829–2,843, https://doi.org/​10.1029/​2018JB016453.

Johnson, H.P., S.G. Merle, T.A. Bjorklund, S.L. Hatula, T. Baumberger, S.L. Walker, J. Liu, N.D. Ward, and C. Wang. 2022. Methane plume emissions associated with Puget Sound faults in the Cascadia forearc. Geochemistry, Geophysics, Geosystems 23(1):e2021GC010211, https://doi.org/​10.1029/2021GC010211.

Levin, L.A., A.R. Baco, D.A. Bowden, A. Colaco, E.E. Cordes, M.R. Cunha, A.W.J. Demopolulos, J., Gobin, B.M. Grupe, J. Le, and others. 2016. Hydrothermal vents and methane seeps: Rethinking the sphere of influence. Frontiers in Marine Science 3:72, https://doi.org/10.3389/fmars.2016.00072.

Lough, A.J.M., A. Tagliabue, C. Demasy, J.A. Resing, T. Mellett, N.J. Wyatt, and M.C. Lohan. 2023. Tracing differences in iron supply to the Mid-Atlantic Ridge valley between hydrothermal vent sites: Implications for the addition of iron to the deep ocean. Biogeosciences 20(2):405–420, https://doi.org/10.5194/bg-20-405-2023.

Lupton, J., and H. Craig. 1981. A major helium-3 source at 15°S on the East Pacific Rise. Science 214(4516):13–18, https://doi.org/10.1126/science.214.4516.13.

Lupton, J.E. 1998. Hydrothermal helium plumes in the Pacific Ocean. Journal of Geophysical Research: Oceans 103(C8):15,853–15,868, https://doi.org/​10.1029/98JC00146.

Lupton, J.E., T. Baumberger, C. Young, R.W. Embley, S.G. Merle, and C.M. Wilkinson. 2018. A new method for sampling solid methane hydrate on the seafloor. Abstract OS24C-04 presented at the Fall Meeting of the American Geophysical Union, December 10–14, 2018, Washington, DC.

Merle, S.G., R.W. Embley, H.P. Johnson, T.-K. Lau, B.J. Phrampus, N.A. Raineault, and L.J. Gee. 2021. Distribution of methane plumes on Cascadia Margin and implications for the landward limit of methane hydrate stability. Frontiers in Earth Science 9:531714, https://doi.org/10.3389/feart.2021.531714.

Michel, A.P.M., V.L. Preston, K.E. Fauria, and D.P. Nicholson. 2021. Observations of shallow methane bubble emissions from Cascadia Margin. Frontiers in Earth Science 9:613234, https://doi.org/​10.3389/​feart.2021.613234.

Philip, B.T., E.A. Solomon, D.S. Kelley, A.M. Trehu, T.L. Whorley, E. Roland, M. Tominaga, and R.W. Collier. 2023. Fluid sources and overpressures within the central Cascadia Subduction Zone revealed by a warm, high-flux seafloor seep. Science Advances 9(4), https://doi.org/10.1126/sciadv.add6688.

Rehder, G., R.W. Collier, K. Heeschen, P.M. Kosro, J. Barth, and E. Suess. 2002. Enhanced marine CH₄ emissions to the atmosphere off Oregon caused by coastal upwelling. Global Biogeochemical Cycles 16(3):2-1–2-11, https://doi.org/​10.1029/​2000GB001391.

Resing, J.A., P.N. Sedwick, C.R. German, W.J. Jenkins, J.W. Moffett, B.M. Sohst, and A. Tagliabue. 2015. Basin-scale transport of hydrothermal dissolved metals across the South Pacific Ocean. Nature 523:200–203, https://doi.org/10.1038/nature14577.

Riedel, M., M. Scherwath, M. Römer, M. Veloso, M. Heesemann, and G.D. Spence. 2018. Distributed natural gas venting offshore along the Cascadia Margin. Nature Communications 9:3264, https://doi.org/10.1038/s41467-018-05736-x.

Schine, C.M.S., A.-C. Alderkamp, G. van Dijken, L.J.A. Gerringa, S. Sergi, P. Laan, H. van Haren, W.H. van de Poll, and K.R. Arrigo. 2021. Massive Southern Ocean phytoplankton bloom fed by iron of possible hydrothermal origin. Nature Communications 12:1211, https://doi.org/10.1038/s41467-021-21339-5.

Seabrook, S., F.C. De Leo, T. Baumberger, N. Raineault, and A.R. Thurber. 2018. Heterogeneity of methane seep biomes in the northeast Pacific. Deep Sea Research Part II 150:195–209, https://doi.org/​10.1016/j.dsr2.2017.10.016.

Suess, E., M.E. Torres, G. Bohrmann, R.W. Collier, J. Greinert, P. Linke, G. Rehder, A. Trehu, K. Wallman, G. Winckler, and E. Zuleger. 1999. Gas hydrate destabilization: Enhanced dewatering, benthic material turnover and large methane plumes at the Cascadia convergent margin. Earth and Planetary Science Letters 170:1–15, https://doi.org/​10.1016/S0012-821X(99)00092-8.

Tagliabue, A., and J. Resing. 2016. Impact of hydrothermalism on the ocean iron cycle. Philosophical Transactions of the Royal Society of London A 374:20150291, https://doi.org/10.1098/rsta.2015.0291.

Tagliabue, A., A.R. Bowie, T.M. Holmes, P. Latour, P.C. van der Merwe, M. East, K. Wuttig, and J.A. Resing. 2022a. Constraining the contribution of hydrothermal iron to Southern Ocean export production using deep ocean iron observations. Frontiers in Marine Science 9:754517, https://doi.org/​10.3389/​fmars.2022.754517.

Tagliabue, A., A.J.M. Lough, C. Vic, V. Roussenov, J. Gula, M.C. Lohan, J.A. Resing, and R.G. Williams. 2022b. Mechanisms driving the dispersal of hydrothermal iron from the northern Mid Atlantic Ridge. Geophysical Research Letters 49(22):e2022GL100615, https://doi.org/​10.1029/2022GL100615.

Wang, H., J.A. Resing, Q. Yan, N.J. Buck, S.M. Michael, H. Zhou, M. Liu, S.L. Walker, Q. Yang, and F. Ji. 2021. The characteristics of Fe speciation and Fe-binding ligands in the Mariana back-arc hydrothermal plumes. Geochimica et Cosmochimica Acta 292:24–36, https://doi.org/10.1016/j.gca.​2020.09.016.

This is an open access article made available under the terms of the Creative Commons Attribution 4.0 International License (https://creativecommons.org/licenses/by/4.0/), which permits use, sharing, adaptation, distribution, and reproduction in any medium or format as long as users cite the materials appropriately, provide a link to the Creative Commons license, and indicate the changes that were made to the original content. Images, animations, videos, or other third-party material used in articles are included in the Creative Commons license unless indicated otherwise in a credit line to the material. If the material is not included in the article’s Creative Commons license, users will need to obtain permission directly from the license holder to reproduce the material.