Oceanography The Official Magazine of
The Oceanography Society
Volume 31 Issue 01

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Volume 31, No. 1
Pages 128 - 135

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Deep-Sea Volcanic Eruptions Create Unique Chemical and Biological Linkages Between the Subsurface Lithosphere and the Oceanic Hydrosphere

By Rachel L. Spietz, David A. Butterfield, Nathaniel J. Buck, Benjamin I. Larson, William W. Chadwick Jr., Sharon L. Walker, Deborah S. Kelley, and Robert M. Morris  
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Article Abstract

In April 2015, pressure recorders, seismometers, and hydrophones attached to the Ocean Observatories Initiative (OOI) Cabled Array on Axial Seamount detected, in real time, a volcanic eruption predominantly located along the north rift zone (NRZ). Real-time detection enabled a rapid response cruise to augment OOI data with ship-based physical, chemical, and biological sampling of the eruption and the new lava flows. The combined data set demonstrates the synergistic value of real-time monitoring combined with rapid response efforts that sample beyond the boundaries of a fixed cabled array. These combined data show that the 2015 eruption gave rise to chemically and microbiologically variable hydrothermal plumes over new NRZ lava flows, reflecting chemical and biological linkages between the subsurface lithosphere and the oceanic hydrosphere. The warmest and least diluted plume near the new lava flows was 0.119°C above background seawater and hosted thermophilic and hyperthermophilic taxa that are typically identified in hydrothermal fluids emanating from the warm subsurface. Cooler and more diluted hydrothermal plumes farther from a hydrothermal fluid source were 0.072°–0.078°C above background seawater and hosted mesophilic and psychrophilic taxa that are typically identified in neutrally buoyant plumes at persistent hydrothermal venting sites. Potentially chemosynthetic microbial lineages, including Epsilonproteobacteria, Gammaproteobacteria, and Methanococcales, were positively correlated with elevated temperature anomalies. These data suggest that hydrothermal fluid flow through new lava flows on the NRZ supported diverse microbial communities for several months following the 2015 eruption and that subsurface heterogeneity contributed to the structure of unique hydrothermal-plume-hosted microbial communities.

Citation

Spietz, R.L., D.A. Butterfield, N.J. Buck, B.I. Larson, W.W. Chadwick Jr., S.L. Walker, D.S. Kelley, and R.M. Morris. 2018. Deep-sea volcanic eruptions create unique chemical and biological linkages between the subsurface lithosphere and the oceanic hydrosphere. Oceanography 31(1):128–135, https://doi.org/10.5670/oceanog.2018.120.

Supplementary Materials

> Methods, Figure S1, and Tables S1 and S2 (120 KB pdf)

References
    Anantharaman, K., J.A. Breier, C.S. Sheik, and G.J. Dick. 2013. Evidence for hydrogen oxidation and metabolic plasticity in widespread deep-sea sulfur-oxidizing bacteria. Proceedings of the National Academy of Sciences of the United States of America 110(1):330–335, https://doi.org/10.1073/pnas.1215340110.
  1. Anderson, R.E., M.T. Beltrán, S.J. Hallam, and J.A. Baross. 2013. Microbial community structure across fluid gradients in the Juan de Fuca Ridge hydrothermal system. FEMS Microbiology Ecology 83(2):324–339, https://doi.org/​10.1111/j.1574-6941.2012.01478.x.
  2. Baker, E.T. 1998. Patterns of event and chronic hydrothermal venting following a magmatic intrusion: New perspectives from the 1996 Gorda Ridge eruption. Deep Sea Research Part II 45(12):2,599–2,618, https://doi.org/10.1016/S0967-0645(98)00085-X.
  3. Baker, E.T., G.J. Massoth, and R.A. Feely. 1987. Cataclysmic hydrothermal venting on the Juan de Fuca Ridge. Nature 329:149–151, https://doi.org/​10.1038/329149a0.
  4. Baker, E.T., R.P. Lowell, J.A. Resing, R.A. Feely, R.W. Embley, G.J. Massoth, and S.L. Walker. 2004. Decay of hydrothermal output following the 1998 seafloor eruption at Axial Volcano: Observations and models. Journal of Geophysical Research 109, B01205, https://doi.org/10.1029/2003JB002618.
  5. Butterfield, D.A., I.R. Jonasson, G.J. Massoth, R.A. Feely, K.K. Roe, R.E. Embley, J.F. Holden, R.E. McDuff, M.D. Lilley, and J.R. Delaney. 1997. Seafloor eruptions and evolution of hydrothermal fluid chemistry. Philosophical Transactions of the Royal Society A 355(1723):369–386, https://doi.org/​10.1098/rsta.1997.0013.
  6. Caress, D.W., D.A. Clague, J.B. Paduan, J.F. Martin, B.M. Dreyer, W.W. Chadwick Jr., A. Denny, and D.S. Kelley. 2012. Repeat bathymetric surveys at 1-metre resolution of lava flows erupted at Axial Seamount in April 2011. Nature Geoscience 5(7):483–488, https://doi.org/10.1038/ngeo1496.
  7. Chadwick, W.W., Jr., D.A. Clague, R.W. Embley, M.R. Perfit, D.A. Butterfield, D.W. Caress, J.B. Paduan, J.F. Martin, P. Sasnett, S.G. Merle, and A.M. Bobbitt. 2013. The 1998 eruption of Axial Seamount: New insights on submarine lava flow emplacement from high-resolution mapping. Geochemistry, Geophysics, Geosystems 14(10):3,939–3,968, https://doi.org/​10.1002/ggge.20202.
  8. Chadwick, W.W., Jr., J.B. Paduan, D.A. Clague, B.M. Dreyer, and S.G. Merle. 2016. Voluminous eruption from a zoned magma body after an increase in supply rate at Axial Seamount. Geophysical Research Letters 5:63–70, https://doi.org/​10.1002/2016GL071327.
  9. Delaney, J.R., D.S. Kelley, M.D. Lilley, D.A. Butterfield, J.A. Baross, W.S.D. Wilcock, R.W. Embley, and M. Summit. 1998. The quantum event of oceanic crustal accretion: Impacts of diking at mid-ocean ridges. Science 281(5374):222–230, https://doi.org/​10.1126/science.281.5374.222.
  10. Djurhuus, A., S. Mikalsen, H. Giebel, and A. Rogers. 2017. Cutting through the smoke: Free-living bacterial diversity in deep-sea hydrothermal plumes. Royal Society Open Science 4:160829, https://doi.org/​10.1098/rsos.160829.
  11. Dziak, R.P., and C.G. Fox. 1999. Long-term seismicity and ground deformation at Axial Volcano, Juan de Fuca Ridge. Geophysical Research Letters 26(24):3,641–3,644, https://doi.org/​10.1029/1999GL002326.
  12. Gulmann, L.K., S.E. Beaulieu, T.M. Shank, K. Ding, W.E. Seyfried, and S.M. Sievert. 2015. Bacterial diversity and successional patterns during biofilm formation on freshly exposed basalt surfaces at diffuse-flow deep-sea vents. Frontiers in Microbiology 6:901, https://doi.org/10.3389/fmicb.2015.00901.
  13. Holden, J.F., M. Summit, and J.A. Baross. 1998. Thermophilic and hyperthermophilic microorganisms in 3–30°C hydrothermal fluids following a deep-sea volcanic eruption. FEMS Microbiology Ecology 25:33–41, https://doi.org/​10.1111/j.1574-6941.1998.tb00458.x.
  14. Huber, J.A., D.A. Butterfield, and J.A. Baross. 2002. Temporal changes in archaeal diversity and chemistry in a mid-ocean ridge subseafloor habitat. Applied and Environmental Microbiology 68(4):1,585–1,594, https://doi.org/​10.1128/AEM.68.4.1585-1594.2002.
  15. Huber, J.A., D.A. Butterfield, and J.A. Baross. 2003. Bacterial diversity in a subseafloor habitat following a deep-sea volcanic eruption. FEMS Microbiology Ecology 43:393–409, https://10.1111/​j.1574-6941.​2003.​tb01080.x.
  16. Huber, J.A., D.B. Mark Welch, H.G. Morrison, S.M. Huse, P.R. Neal, D.A. Butterfield, and M.L. Sogin. 2007. Microbial population structures in the deep marine biosphere. Science 318(5847):97–100, https://doi.org/​10.1126/​science.1146689.
  17. Kelley, D.S., J.R. Delaney, and S.K. Juniper. 2014. Establishing a new era of submarine volcanic observatories: Cabling Axial Seamount and the Endeavour Segment of the Juan de Fuca Ridge. Marine Geology 352:426–450, https://doi.org/​10.1016/j.margeo.2014.03.010.
  18. Kelley, D.S., J.R. Delaney, and the Cabled Array Team. 2016. NSF’s Cabled Array: A wired tectonic plate and overlying ocean. OCEANS 2016 MTS/IEEE Monterey, OCE 2016, https://doi.org/10.1109/OCEANS.2016.7761398.
  19. Liu, Y. 2010. Methanomicrobiales. Pp. 583–593 in Handbook of Hydrocarbon and Lipid Microbiology. K.N. Timmis, ed., Springer Berlin Heidelberg, https://doi.org/10.1007/978-3-540-77587-4_45.
  20. Lupton, J.E., J.R. Delaney, H.P. Johnson, and M.K. Tivey. 1985. Entrainment and vertical transport of deep-ocean water by buoyant hydrothermal plumes. Nature 316(6029):621–623, https://doi.org/​10.1038/316621a0.
  21. Lutz, R.A., T.M. Shank, D.J. Fornari, R.M. Haymon, M.D. Lilley, K.L. Von Damm, and D. Desbruyeres. 1994. Rapid growth at deep-sea vents. Nature 371:633–634, https://doi.org/​10.1038/371663a0.
  22. Mattes, T.E., B.L. Nunn, K.T. Marshall, G. Proskurowski, D.S. Kelley, O.E. Kawka, D.R. Goodlett, D.A. Hansell, and R.M. Morris. 2013. Sulfur oxidizers dominate carbon fixation at a biogeochemical hot spot in the dark ocean. The ISME Journal 7(12):2,349–2,360, https://doi.org/10.1038/ismej.2013.113.
  23. McCollom, T.M. 2000. Geochemical constraints on primary productivity in submarine hydrothermal vent plumes. Deep Sea Research Part I 47(1):85–101, https://doi.org/10.1016/S0967-0637(99)00048-5.
  24. McCollom, T.M., and E.L. Shock. 1997. Geochemical constraints on chemolithoautotrophic metabolism by microorganisms in seafloor hydrothermal systems. Geochimica et Cosmochimica Acta 61(20):4,375–4,391, https://doi.org/10.1016/S0016-7037(97)00241-X.
  25. Meyer, J.L., N.H. Akerman, G. Proskurowski, and J.A. Huber. 2013. Microbiological characterization of post-eruption “snowblower” vents at axial seamount, Juan de Fuca Ridge. Frontiers in Microbiology 4:153, https://doi.org/10.3389/fmicb.2013.00153.
  26. Nooner, S.L., and W.W. Chadwick Jr.. 2016. Inflation-predictable behavior and co-eruption deformation at Axial Seamount. Science 354(6318):1399–1403, https://doi.org/10.1126/science.aah4666.
  27. Opatkiewicz, A.D., D.A. Butterfield, and J.A. Baross. 2009. Individual hydrothermal vents at Axial Seamount harbor distinct subseafloor microbial communities. FEMS Microbiology Ecology 70(3):413–424, https://doi.org/​10.1111/​j.1574-6941.2009.00747.x.
  28. Sheik, C.S., K. Anantharaman, J.A. Breier, J.B. Sylvan, K.J. Edwards, and G.J. Dick. 2015. Spatially resolved sampling reveals dynamic microbial communities in rising hydrothermal plumes across a back-arc basin. The ISME Journal 9(6):1,434–1,445, https://doi.org/10.1038/ismej.2014.228.
  29. Shock, E.L., and M.E. Holland. 1997. Geochemical energy sources that support the subsurface biosphere. Pp. 153–165 in The Subseafloor Biosphere at Mid-Ocean Ridges. W.S.D. Wilcock, E.F. Delong, D.S. Kelley, J.A. Baross, and S.C. Cary, eds, American Geophysical Union, Washington, DC.
  30. Summit, M., and J.A. Baross. 1998. Thermophilic subseafloor microorganisms from the 1996 North Gorda Ridge eruption. Deep Sea Research Part II 45(12):2,751–2,766, https://doi.org/10.1016/S0967-0645(98)00092-7.
  31. Sunamura, M., Y. Higashi, C. Miyako, J.I. Ishibashi, and A. Maruyama. 2004. Two bacteria phylotypes are predominant in the Suiyo Seamount hydrothermal plume. Applied and Environmental Microbiology 70(2):1,190–1,198, https://doi.org/​10.1128/AEM.70.2.1190-1198.2004.
  32. Topcuoglu, B.D., L.C. Stewart, H.G. Morrison, D.A. Butterfield, J.A. Huber, and J.F. Holden. 2016. Hydrogen limitation and syntrophic growth among natural assemblages of thermophilic methanogens at deep-sea hydrothermal vents. Frontiers in Microbiology 7:1240, https://doi.org/10.3389/fmicb.2016.01240.
  33. Tunnicliffe, V., R.W. Embley, J.F. Holden, D.A. Butterfield, G.J. Massoth, and S.K. Juniper. 1997. Biological colonization of new hydrothermal vents following an eruption on Juan de Fuca Ridge. Deep-Sea Research Part I 44(9–10):1,627–1,644, https://doi.org/10.1016/S0967-0637(97)00041-1.
  34. Wilcock, W.S.D., M. Tolstoy, F. Waldhauser, C. Garcia, Y.J. Tan, D.R. Bohnenstiehl, J. Caplan-Auerback, R.P. Dziak, A.F. Arnulf, and M.E. Mann. 2016. Seismic constraints on caldera dynamics from the 2015 Axial Seamount eruption. Science 354(6318):1,395–1,399, https://doi.org/​10.1126/science.aah5563.
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