Articles | Volume 25
https://doi.org/10.5194/sd-25-35-2019
https://doi.org/10.5194/sd-25-35-2019
Science report
 | 
12 Jun 2019
Science report |  | 12 Jun 2019

SUSTAIN drilling at Surtsey volcano, Iceland, tracks hydrothermal and microbiological interactions in basalt 50 years after eruption

Marie D. Jackson, Magnús T. Gudmundsson, Tobias B. Weisenberger, J. Michael Rhodes, Andri Stefánsson, Barbara I. Kleine, Peter C. Lippert, Joshua M. Marquardt, Hannah I. Reynolds, Jochem Kück, Viggó T. Marteinsson, Pauline Vannier, Wolfgang Bach, Amel Barich, Pauline Bergsten, Julia G. Bryce, Piergiulio Cappelletti, Samantha Couper, M. Florencia Fahnestock, Carolyn F. Gorny, Carla Grimaldi, Marco Groh, Ágúst Gudmundsson, Ágúst T. Gunnlaugsson, Cédric Hamlin, Thórdís Högnadóttir, Kristján Jónasson, Sigurdur S. Jónsson, Steffen L. Jørgensen, Alexandra M. Klonowski, Beau Marshall, Erica Massey, Jocelyn McPhie, James G. Moore, Einar S. Ólafsson, Solveig L. Onstad, Velveth Perez, Simon Prause, Snorri P. Snorrason, Andreas Türke, James D. L. White, and Bernd Zimanowski

Viewed

Total article views: 3,565 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,822 647 96 3,565 290 106 111
  • HTML: 2,822
  • PDF: 647
  • XML: 96
  • Total: 3,565
  • Supplement: 290
  • BibTeX: 106
  • EndNote: 111
Views and downloads (calculated since 12 Jun 2019)
Cumulative views and downloads (calculated since 12 Jun 2019)

Viewed (geographical distribution)

Total article views: 2,850 (including HTML, PDF, and XML) Thereof 2,835 with geography defined and 15 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 19 Apr 2024
Download
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.