SUSTAIN drilling at Surtsey volcano, Iceland, tracks hydrothermal and microbiological interactions in basalt 50 years after eruption
Department of Geology and Geophysics, University of Utah, Salt Lake City, Utah, USA
Magnús T. Gudmundsson
Nordvulk, Institute of Earth Sciences, University of Iceland, Reykjavík, Iceland
Tobias B. Weisenberger
ÍSOR, Iceland GeoSurvey, Reykjavík, Iceland
J. Michael Rhodes
Department of Geosciences, University of Massachusetts, Amherst, Massachusetts, USA
Andri Stefánsson
Nordvulk, Institute of Earth Sciences, University of Iceland, Reykjavík, Iceland
Barbara I. Kleine
Nordvulk, Institute of Earth Sciences, University of Iceland, Reykjavík, Iceland
Peter C. Lippert
Department of Geology and Geophysics, University of Utah, Salt Lake City, Utah, USA
Joshua M. Marquardt
Department of Geology and Geophysics, University of Utah, Salt Lake City, Utah, USA
Hannah I. Reynolds
Nordvulk, Institute of Earth Sciences, University of Iceland, Reykjavík, Iceland
Jochem Kück
Helmholtz Centre Potsdam, GFZ German Research Centre for Geosciences, Potsdam, Germany
Viggó T. Marteinsson
Matís, Exploration & Utilization of Genetic Resources, Reykjavík, Iceland
Faculty of Food Science and Nutrition, University of Iceland, Reykjavík, Iceland
Pauline Vannier
Matís, Exploration & Utilization of Genetic Resources, Reykjavík, Iceland
Wolfgang Bach
Department of Geosciences and MARUM, University of Bremen, Bremen, Germany
Amel Barich
ÍSOR, Iceland GeoSurvey, Reykjavík, Iceland
Geothermal Research Cluster (GEORG), Reykjavik, Iceland
Pauline Bergsten
Matís, Exploration & Utilization of Genetic Resources, Reykjavík, Iceland
Faculty of Life and Environmental Sciences, University of Iceland, Reykjavík, Iceland
Julia G. Bryce
University of New Hampshire, Durham, New Hampshire, USA
Piergiulio Cappelletti
Dipartimento di Scienze della Terra, dell'Ambiente e delle Risorse (DiSTAR), University FEDERICO II, Naples, Italy
Samantha Couper
Department of Geology and Geophysics, University of Utah, Salt Lake City, Utah, USA
M. Florencia Fahnestock
University of New Hampshire, Durham, New Hampshire, USA
Carolyn F. Gorny
Nordvulk, Institute of Earth Sciences, University of Iceland, Reykjavík, Iceland
Carla Grimaldi
Dipartimento di Scienze della Terra, dell'Ambiente e delle Risorse (DiSTAR), University FEDERICO II, Naples, Italy
Marco Groh
Helmholtz Centre Potsdam, GFZ German Research Centre for Geosciences, Potsdam, Germany
Ágúst Gudmundsson
Jarðtaeknistofan, (GEOICE Geological Services Ltd), Hafnarfjörður, Iceland
Ágúst T. Gunnlaugsson
Nordvulk, Institute of Earth Sciences, University of Iceland, Reykjavík, Iceland
Cédric Hamlin
K.G. Jebsen Centre for Deep Sea Research, Department of Earth Science, University of Bergen, Bergen, Norway
Thórdís Högnadóttir
Nordvulk, Institute of Earth Sciences, University of Iceland, Reykjavík, Iceland
Kristján Jónasson
Collections and Systematics Department, Icelandic Institute of Natural History, Gardabaer, Iceland
Sigurdur S. Jónsson
ÍSOR, Iceland GeoSurvey, Reykjavík, Iceland
Steffen L. Jørgensen
K.G. Jebsen Centre for Deep Sea Research, Department of Earth Science, University of Bergen, Bergen, Norway
Alexandra M. Klonowski
Faculty of Food Science and Nutrition, University of Iceland, Reykjavík, Iceland
Beau Marshall
DOSECC Exploration Services, Salt Lake City, Utah, USA
Erica Massey
Nordvulk, Institute of Earth Sciences, University of Iceland, Reykjavík, Iceland
Jocelyn McPhie
School of Natural Sciences, University of Tasmania, Hobart, Australia
James G. Moore
U.S. Geological Survey, Menlo Park, California, USA
Einar S. Ólafsson
Nordvulk, Institute of Earth Sciences, University of Iceland, Reykjavík, Iceland
Solveig L. Onstad
K.G. Jebsen Centre for Deep Sea Research, Department of Earth Science, University of Bergen, Bergen, Norway
Velveth Perez
Nordvulk, Institute of Earth Sciences, University of Iceland, Reykjavík, Iceland
Collections and Systematics Department, Icelandic Institute of Natural History, Gardabaer, Iceland
Simon Prause
ÍSOR, Iceland GeoSurvey, Reykjavík, Iceland
Snorri P. Snorrason
Verkís Consulting Engineers, Reykjavík, Iceland
Andreas Türke
Matís, Exploration & Utilization of Genetic Resources, Reykjavík, Iceland
James D. L. White
Geology Department, University of Otago, Dunedin, New Zealand
Bernd Zimanowski
Institut für Geographie und Geologie, Universität Würzburg, Würzburg, Germany
Related authors
Andreas Türke, Marie D. Jackson, Wolfgang Bach, Wolf-Achim Kahl, Brian Grzybowski, Beau Marshall, Magnús T. Gudmundsson, and Steffen Leth Jørgensen
Sci. Dril., 25, 57–62, https://doi.org/10.5194/sd-25-57-2019, https://doi.org/10.5194/sd-25-57-2019, 2019
M. D. Jackson, M. T. Gudmundsson, W. Bach, P. Cappelletti, N. J. Coleman, M. Ivarsson, K. Jónasson, S. L. Jørgensen, V. Marteinsson, J. McPhie, J. G. Moore, D. Nielson, J. M. Rhodes, C. Rispoli, P. Schiffman, A. Stefánsson, A. Türke, T. Vanorio, T. B. Weisenberger, J. D. L. White, R. Zierenberg, and B. Zimanowski
Sci. Dril., 20, 51–58, https://doi.org/10.5194/sd-20-51-2015, https://doi.org/10.5194/sd-20-51-2015, 2015
Short summary
Short summary
A new drilling program at Surtsey Volcano, a 50-year-old oceanic island and UNESCO World Heritage site in Iceland, will undertake interdisciplinary investigations of rift zone volcanism, dynamic hydrothermal mineral assemblages in basaltic tephra, and subterrestrial microbial colonization and succession in altered tephra and hydrothermal fluids. Long-term monitoring of evolving hydrothermal and biological processes will occur through installation of a 200m deep Surtsey subsurface observatory.
Marcel Ortler, Achim Brauer, Stefano C. Fabbri, Jean Nicolas Haas, Irka Hajdas, Kerstin Kowarik, Jochem Kueck, Hans Reschreiter, and Michael Strasser
Sci. Dril., 33, 1–19, https://doi.org/10.5194/sd-33-1-2024, https://doi.org/10.5194/sd-33-1-2024, 2024
Short summary
Short summary
The lake drilling project at Lake Hallstatt (Austria) successfully cored 51 m of lake sediments. This was achieved through the novel drilling platform Hipercorig. A core-log seismic correlation was created for the first time of an inner Alpine lake of the Eastern Alps. The sediments cover over 12 000 years before present with 10 (up to 5.1 m thick) instantaneous deposits. Lake Hallstatt is located within an UNESCO World Heritage area which has a rich history of human salt mining.
Cécile Massiot, Ludmila Adam, Eric S. Boyd, S. Craig Cary, Daniel R. Colman, Alysia Cox, Ery Hughes, Geoff Kilgour, Matteo Lelli, Domenico Liotta, Karen G. Lloyd, Tiipene Marr, David D. McNamara, Sarah D. Milicich, Craig A. Miller, Santanu Misra, Alexander R. L. Nichols, Simona Pierdominici, Shane M. Rooyakkers, Douglas R. Schmitt, Andri Stefansson, John Stix, Matthew B. Stott, Camille Thomas, Pilar Villamor, Pujun Wang, Sadiq J. Zarrouk, and the CALDERA workshop participants
Sci. Dril., 33, 67–88, https://doi.org/10.5194/sd-33-67-2024, https://doi.org/10.5194/sd-33-67-2024, 2024
Short summary
Short summary
Volcanoes where tectonic plates drift apart pose eruption and earthquake hazards. Underground waters are difficult to track. Underground microbial life is probably plentiful but unexplored. Scientists discussed the idea of drilling two boreholes in the Okataina Volcanic Centre, New Zealand, to unravel the connections between volcano, faults, geotherms, and the biosphere, also integrating mātauranga Māori (Indigenous knowledge) to assess hazards and manage resources and microbial ecosystems.
Matthew W. Hayward, Colin N. Whittaker, Emily M. Lane, William L. Power, Stéphane Popinet, and James D. L. White
Nat. Hazards Earth Syst. Sci., 22, 617–637, https://doi.org/10.5194/nhess-22-617-2022, https://doi.org/10.5194/nhess-22-617-2022, 2022
Short summary
Short summary
Volcanic eruptions can produce tsunamis through multiple mechanisms. We present validation cases for a numerical method used in simulating waves caused by submarine explosions: a laboratory flume experiment and waves generated by explosions at field scale. We then demonstrate the use of the scheme for simulating analogous volcanic eruptions, illustrating the resulting wavefield. We show that this scheme models such dispersive sources more proficiently than standard tsunami models.
Henning Lorenz, Jan-Erik Rosberg, Christopher Juhlin, Iwona Klonowska, Rodolphe Lescoutre, George Westmeijer, Bjarne S. G. Almqvist, Mark Anderson, Stefan Bertilsson, Mark Dopson, Jens Kallmeyer, Jochem Kück, Oliver Lehnert, Luca Menegon, Christophe Pascal, Simon Rejkjær, and Nick N. W. Roberts
Sci. Dril., 30, 43–57, https://doi.org/10.5194/sd-30-43-2022, https://doi.org/10.5194/sd-30-43-2022, 2022
Short summary
Short summary
The Collisional Orogeny in the Scandinavian Caledonides project provides insights into the deep structure and bedrock of a ca. 400 Ma old major orogen to study deformation processes that are hidden at depth from direct access in modern mountain belts. This paper describes the successful operations at the second site. It provides an overview of the retrieved geological section that differs from the expected and summarises the scientific potential of the accomplished data sets and drill core.
Jeffrey P. Gay, Lowell Miyagi, Samantha Couper, Christopher Langrand, David P. Dobson, Hanns-Peter Liermann, and Sébastien Merkel
Eur. J. Mineral., 33, 591–603, https://doi.org/10.5194/ejm-33-591-2021, https://doi.org/10.5194/ejm-33-591-2021, 2021
Short summary
Short summary
We examined the experimental deformation and phase transition of a bridgmanite analogue, NaCoF3, using a resistive-heated diamond anvil cell and a synchrotron radiation source. We wanted to observe the behavior of NaCoF3 under uniaxial compression and its plastic properties, as well as to determine if it is a suitable analogue for natural samples. We observe 100 and 001 compression textures and link those to the dominant deformation mechanism in the perovskite structure.
Eyjólfur Magnússon, Finnur Pálsson, Magnús T. Gudmundsson, Thórdís Högnadóttir, Cristian Rossi, Thorsteinn Thorsteinsson, Benedikt G. Ófeigsson, Erik Sturkell, and Tómas Jóhannesson
The Cryosphere, 15, 3731–3749, https://doi.org/10.5194/tc-15-3731-2021, https://doi.org/10.5194/tc-15-3731-2021, 2021
Short summary
Short summary
We present a unique insight into the shape and development of a subglacial lake over a 7-year period, using repeated radar survey. The lake collects geothermal meltwater, which is released in semi-regular floods, often referred to as jökulhlaups. The applicability of our survey approach to monitor the water stored in the lake for a better assessment of the potential hazard of jökulhlaups is demonstrated by comparison with independent measurements of released water volume during two jökulhlaups.
Daniela Novembre, Domingo Gimeno, Piergiulio Cappelletti, and Sossio Fabio Graziano
Eur. J. Mineral., 33, 315–328, https://doi.org/10.5194/ejm-33-315-2021, https://doi.org/10.5194/ejm-33-315-2021, 2021
Short summary
Short summary
Zeolites are used in several technological applications. Knowledge of their genetic mechanisms in geological deposits can help to understand the type of zeolite forming in specific conditions and their sector of possible use. The pyroclastic deposit
Tufo Rosso a Scorie Nere(Vico volcano, Latium, Italy) exhibits intense zeolitization processes at chabazite and phillipsite. This abundant presence makes the deposit worthy of being considered for possible exploitation.
Jochem Kück, Marco Groh, Martin Töpfer, Andreas Jurczyk, and Ulrich Harms
Sci. Dril., 29, 39–48, https://doi.org/10.5194/sd-29-39-2021, https://doi.org/10.5194/sd-29-39-2021, 2021
Short summary
Short summary
New cable-free borehole memory sondes allow measurements in boreholes with very unstable walls, which is common, e.g., in soft sediments below lakes. The drill-pipe-mounted memory sondes can pass through narrowed zones. While being pulled up by the drill pipes, they measure natural radioactivity, velocity of sound, electrical conductivity, magnetizability, and the temperature of the borehole rocks. We describe the memory sondes and appendant depth devices, both tested in thorough field tests.
Felix Kästner, Simona Pierdominici, Judith Elger, Alba Zappone, Jochem Kück, and Christian Berndt
Solid Earth, 11, 607–626, https://doi.org/10.5194/se-11-607-2020, https://doi.org/10.5194/se-11-607-2020, 2020
Short summary
Short summary
Knowledge about physical properties at depth is crucial to image and understand structures linked with orogenic processes. We examined seismic velocities from core and downhole data from the COSC-1 borehole, Sweden, and calibrated our results with laboratory measurements on core samples. Despite a strong mismatch between the core and downhole velocities due to microcracks, mafic units are resolved at all scales, while at sample scale, strong seismic anisotropy correlates with the rock foliation.
Elmar Albers, Wolfgang Bach, Frieder Klein, Catriona D. Menzies, Friedrich Lucassen, and Damon A. H. Teagle
Solid Earth, 10, 907–930, https://doi.org/10.5194/se-10-907-2019, https://doi.org/10.5194/se-10-907-2019, 2019
Short summary
Short summary
To understand the fate of carbon in subducted oceanic sediments and crust, we studied carbonate phases in rocks from the Mariana subduction zone. These show that carbon is liberated from the downgoing plate at depths less than 20 km. Some of the carbon is subsequently trapped in minerals and likely subducts to greater depths, whereas fluids carry the other part back into the ocean. Our findings imply that shallow subduction zone processes may play an important role in the deep carbon cycle.
Andreas Türke, Marie D. Jackson, Wolfgang Bach, Wolf-Achim Kahl, Brian Grzybowski, Beau Marshall, Magnús T. Gudmundsson, and Steffen Leth Jørgensen
Sci. Dril., 25, 57–62, https://doi.org/10.5194/sd-25-57-2019, https://doi.org/10.5194/sd-25-57-2019, 2019
Guðmundur Ó. Friðleifsson, Wilfred A. Elders, Robert A. Zierenberg, Ari Stefánsson, Andrew P. G. Fowler, Tobias B. Weisenberger, Björn S. Harðarson, and Kiflom G. Mesfin
Sci. Dril., 23, 1–12, https://doi.org/10.5194/sd-23-1-2017, https://doi.org/10.5194/sd-23-1-2017, 2017
Short summary
Short summary
The Iceland Deep Drilling Project research well IDDP-2 at Reykjanes, Iceland, reached supercritical conditions at 4.5 km in January 2017. The bottom hole temperature was 426 °C and the fluid pressure was 34 MPa. Reykjanes is the landward extension of the Mid-Atlantic Ridge in Iceland, and unique among Icelandic geothermal systems in being recharged by seawater. The setting and fluid characteristics at Reykjanes provide a geochemical analog of a mid-ocean ridge submarine black smoker system.
Wolf-Achim Kahl, Christian Hansen, and Wolfgang Bach
Solid Earth, 7, 651–658, https://doi.org/10.5194/se-7-651-2016, https://doi.org/10.5194/se-7-651-2016, 2016
Short summary
Short summary
A new flow-through reaction cell consisting of an X-ray transparent semicrystalline thermoplastic has been developed for percolation experiments. Core holder, tubing and all confining parts are designed of PEEK (polyetheretherketone) to allow concomitant surveillance of the reaction progress by X-ray microtomography. The reaction progress of the flow-through experiment can be monitored without dismantling the sample from the core holder.
M. D. Jackson, M. T. Gudmundsson, W. Bach, P. Cappelletti, N. J. Coleman, M. Ivarsson, K. Jónasson, S. L. Jørgensen, V. Marteinsson, J. McPhie, J. G. Moore, D. Nielson, J. M. Rhodes, C. Rispoli, P. Schiffman, A. Stefánsson, A. Türke, T. Vanorio, T. B. Weisenberger, J. D. L. White, R. Zierenberg, and B. Zimanowski
Sci. Dril., 20, 51–58, https://doi.org/10.5194/sd-20-51-2015, https://doi.org/10.5194/sd-20-51-2015, 2015
Short summary
Short summary
A new drilling program at Surtsey Volcano, a 50-year-old oceanic island and UNESCO World Heritage site in Iceland, will undertake interdisciplinary investigations of rift zone volcanism, dynamic hydrothermal mineral assemblages in basaltic tephra, and subterrestrial microbial colonization and succession in altered tephra and hydrothermal fluids. Long-term monitoring of evolving hydrothermal and biological processes will occur through installation of a 200m deep Surtsey subsurface observatory.
V. Marteinsson, A. Klonowski, E. Reynisson, P. Vannier, B. D. Sigurdsson, and M. Ólafsson
Biogeosciences, 12, 1191–1203, https://doi.org/10.5194/bg-12-1191-2015, https://doi.org/10.5194/bg-12-1191-2015, 2015
Short summary
Short summary
Colonization of life on Surtsey has been observed systematically since the formation of the island. Microbial colonization and the influence of associate vegetation and birds on viable counts of environmental bacteria at the surface of the Surtsey was explored for the first time in diverse surface soils. Also, hot subsurface samples deep in the centre of this volcanic island were collected. Both uncultivated bacteria and archaea were found in the subsurface samples collected below 145 m.
K. Edwards, W. Bach, A. Klaus, and the IODP Expedition 336 Scientific Party
Sci. Dril., 17, 13–18, https://doi.org/10.5194/sd-17-13-2014, https://doi.org/10.5194/sd-17-13-2014, 2014
Cited articles
Adkins, S.: Volcanic cores from Iceland's youngest island, Coring Magazine,
6, 38–39, 2018.
Alexandersson, T.: The sedimentary xenoliths from Surtsey: turbidites
indicating shelf growth, Surtsey Res. Progr. Rept., 6, 101–116, 1972.
ASTM C97/C97M-18: Standard Test Methods for Absorption and Bulk Specific
Gravity of Dimension Stone, ASTM International, West Conshohocken, PA,
https://doi.org/10.1520/C0097_C0097M-18, 2018.
Baldursson, S. and Ingadóttir, Á.: Nomination of Surtsey for the
UNESCO World Heritage List, Icelandic Institute of Natural History,
Reykjavik, 2007.
Einarsson, P.: Plate boundaries, rifts and transforms in Iceland, Jökull,
58, 35–58, 2008.
Hafstað, Þ. H., Jónasson, Þ., and Hjaltadóttir, S.:
Vestmannaeyjar. Borholur á Heimey og mælingar á þeim (in
Icelandic), Vestmannaeyjar, Measurements in boreholes on Heimaey,
Orkustofnun, Greinargerð ÞÞ-ÞJ-SHj-2002/13, 19 pp., 2002.
Jackson, M. and Swanson-Hysell, N. L.: Rock magnetism of remagnetized
carbonate rocks: Another look, in: Remagnetization and Chemical Alteration of
Sedimentary Rocks, edited by: Elmore, R. D., Muxworthy, A. R., Aldana, M. M.,
and Mena, M., Geological Society of London Special Publication, 371,
279–303, https://doi.org/10.1144/SP371.3, 2012.
Jackson, M. D., Gudmundsson, M. T., Bach, W., Cappelletti, P., Coleman, N.
J., Ivarsson, M., Jónasson, K., Jørgensen, S. L., Marteinsson, V.,
McPhie, J., Moore, J. G., Nielson, D., Rhodes, J. M., Rispoli, C., Schiffman,
P., Stefánsson, A., Türke, A., Vanorio, T., Weisenberger, T. B.,
White, J. D. L., Zierenberg, R., and Zimanowski, B.: Time-lapse
characterization of hydrothermal seawater and microbial interactions with
basaltic tephra at Surtsey Volcano, Sci. Dril., 20, 51–58,
https://doi.org/10.5194/sd-20-51-2015, 2015.
Jakobsson, S. P.: Dredge hauls from Vestmannaeyjagrunn, Iceland, Surtsey Res.
Progr. Rept., 9, 142–148, 1982.
Jakobsson, S. P.: Geological map of Surtsey, scale 1:5000, Icelandic
Institute of Natural History and the Surtsey Research Society,
Reykjavík, 2000.
Jakobsson, S. P. and Moore, J. G.: The Surtsey research drilling project of
1979, Surtsey Res. Progr. Rept., 9, 76–93, 1982.
Jakobsson, S. P. and Moore, J. G.: Hydrothermal minerals and alteration rates
at Surtsey volcano, Iceland, Geol. Soc. Am. Bull., 97, 648–659, 1986.
Jakobsson, S. P., Gudmundsson, G., and Moore, J. G.: Geological monitoring of
Surtsey, Iceland, 1967–1998, Surtsey Research, 11, 99–108, 2000.
Jakobsson, S. P., Thors, K., Vésteinsson, Á. T., and
Ásbjörnsdóttir, L.: Some aspects of the seafloor morphology at
Surtsey volcano: the new multibeam bathymetric survey of 2007, Surtsey
Research, 12, 9–20, 2009.
Kokelaar, B. P.: The mechanism of Surtseyan volcanism, J. Geological Society
of London, 140, 939–944, 1983.
Lovley, D. R., Stolz, J. F., Nord Jr., L., and Phillips, E. J. P.: Anaerobic
production of magnetite by a dissimulatory iron-reducing microorganism,
Nature, 330, 252–254, 1987.
Magnússon, B., Magnússon, S. H., Ólafsson, E., and Sigurdsson, B.
D.: Plant colonization, succession and ecosystem development on Surtsey with
reference to neighbouring islands, Biogeosciences, 11, 5521–5537,
https://doi.org/10.5194/bg-11-5521-2014, 2014.
Marteinsson, V., Klonowski, A., Reynisson, E., Vannier, P., Sigurdsson, B.
D., and Ólafsson, M.: Microbial colonization in diverse surface soil
types in Surtsey and diversity analysis of its subsurface microbiota,
Biogeosciences, 12, 1191–1203, https://doi.org/10.5194/bg-12-1191-2015,
2015.
Moore, J. G.: Structure and eruptive mechanisms at Surtsey Volcano, Iceland,
Geol. Magazine, 122, 649–661, 1985.
Oddsson, B.: Rock quality designation and drilling rate correlated with
lithology and degree of alteration in volcanic rocks from the Surtsey 1979
drill hole, Surtsey Res. Prog. Rept., 9, 94–97, 1982.
Ólafsson, M. and Jakobsson, S. P.: Chemical composition of hydrothermal
water and water-rock interactions on Surtsey volcanic island: A preliminary
report, Surtsey Research, 12, 29–38, 2009.
Reynisson, R. F. and Jakobsson, S. P.: Xenoliths of exotic origin at Surtsey
volcano, Iceland, Surtsey Research, 12, 21–27, 2009.
Rhodes, J. M. and Vollinger, M. J.: Composition of basaltic lavas sampled by
phase-2 of the Hawaii Scientific Drilling Project: Geochemical stratigraphy
and magma types, Geochem. Geophy. Geosy., 5, Q03G13,
https://doi.org/10.1029/2002GC000434, 2004.
Roberts, A. P.: Magnetic mineral diagenesis, Earth Science Reviews, 151,
1–47, 2015.
Santelli, C. M., Orcutt, B. N., Banning, E., Bach, W., Moyer, C. L., Sogin,
M. L., Staudigel, H., and Edwards, K. J.: Abundance and diversity of
microbial life in ocean crust, Nature, 453, 653–656, 2008.
Schipper, C. I. and White, J. D. L.: Magma-slurry interaction in Surtseyan
eruptions, Geology, 44, 195–198, 2016.
Schipper, C. I., Jakobsson, S. P., White, J. D. L., Palin, J. M., and
Bush-Marcinowski, T.: The Surtsey magma series, Sci.-Rep.-UK, 5, 11498,
https://doi.org/10.1038/srep11498, 2015.
Schipper C. I., Le Voyer, M., Moussallam, Y., White, J. D. L., Thordarson,
T., Kimura, J.-I., and Chang, Q.: Degassing and magma mixing during the
eruption of Surtsey Volcano (Iceland, 1963–1967): the signatures of a
dynamic and discrete rift propagation event, Bull. Volcanol., 78, 1–19,
2016.
Staudigel, H.: Hydrothermal alteration processes in the oceanic crust.
Treatise on geochemistry, edited by: Holland, H. D. and Turekian, K. K.,
511–535, Amsterdam, Boston, Elsevier-Pergamon, 2004.
Thórarinsson, S.: Surtsey, The New Island in the North Atlantic, The
Viking Press, New York, 1967.
Thórarinsson, S.: Sídustu thaettir Eyjaelda (English summary: The
last phases of the Surtsey eruption), Náttúrufraedingurinn, 38,
113–135, 1969.
Thórarinsson, S., Einarsson, Th., Sigvaldason, G., and Elísson, G.:
The submarine eruption off the Vestmann Islands 1963–64, Bull. Volcanol.,
29, 435–455, 1964.
Thors, K. and Jakobsson, S. P.: Two seismic reflection profiles from the
vicinity of Surtsey, Iceland, Surtsey Res. Progr. Rept. 9, 149–151, 1982.
Tómasson, J.: On the origin of sedimentary water beneath Vestmann
Islands, Jökull, 17, 300–311, 1967.
Türke, A. T., Jackson, M. D., Bach, W., Kahl, W.-A., Gudmundsson, M. T., and Jørgensen, S.
L.: Design of the Subsurface Observatory at Surtsey Volcano, Iceland, Sci.
Dril., in press, 2019.
Weisenberger, T. B., Gudmundsson, M. T., Jackson, M. D., Gorny, C.,
Türke, A., Kleine, B. I., Marshall, B., Jørgensen, S. L., Marteinsson,
V. Þ., Stefánsson, A., White, J. D. L., Barich, A., Bergsten, P.,
Bryce, J., Couper, S., Fahnestock, F., Franzson, H., Grimaldi, C., Groh, M.,
Guðmundsson, Á., , Gunnlaugsson Á. Þ., Hamlin, C.,
Högnadóttir, Þ., Jónasson, K., Jónsson, S. S., Klonowski,
A., Kück, J., Magnússon, R. L., Massey, E., McPhie, J., Ólafsson,
E. S., Onstad, S. L., Prause, S., Perez, V., Rhodes, J. M., and Snorrason, S.
P.: Operational Report for the 2017 Surtsey Underwater volcanic System for
Thermophiles, Alteration processes and INnovative Concretes (SUSTAIN)
drilling project at Surtsey Volcano, Iceland, Geo Forschungs Zentrum (GFZ)
German Research Centre for Geosciences, https://doi.org/10.2312/ICDP.5059.001, 2019.
White, J. D. L. and Ross, P.-S.: Maar-diatreme volcanoes: A review, J. Volc.
Geotherm. Res., 201, 1–29, 2011.
Witke, A.: Iceland drilling project aims to unearth how islands form, Nature,
547, 387–388, 2017.
Short summary
Three new cored boreholes through Surtsey volcano, an isolated island in southeastern Iceland, provide fresh insights into understanding how explosive submarine volcanism and the earliest alteration of basaltic deposits proceed in a pristine oceanic environment. The still-hot volcano was first sampled through a drill core in 1979. The time-lapse drill cores record the changing geochemical, mineralogical, microbiological, and material properties of the basalt 50 years after eruptions terminated.
Three new cored boreholes through Surtsey volcano, an isolated island in southeastern Iceland,...