2019
DOI: 10.2312/icdp.5059.001
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Operational report for the 2017 Surtsey Underwater volcanic System for Thermophiles, Alteration processes and INnovative concretes (SUSTAIN) drilling project at Surtsey Volcano, Iceland

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Cited by 5 publications
(2 citation statements)
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“…The island was formed between 1963 and 1967 by underwater basaltic eruptions from the seafloor [15–17]. Cultivation and strain isolation was part of an effort supported by the International Continental Scientific Drilling Program (ICDP) among other project partners, to characterize the subsurface edifice of the island in terms of volcanology, mineralogy, hydrology, chemistry and microbiology [18–20]. Of many bacteria isolated while studying the cultivable part of the subsurface prokaryotic diversity, the strains described here were selected because of their low 16S rRNA gene sequence similarity (~96 %) to other species.…”
Section: Isolation and Ecologymentioning
confidence: 99%
“…The island was formed between 1963 and 1967 by underwater basaltic eruptions from the seafloor [15–17]. Cultivation and strain isolation was part of an effort supported by the International Continental Scientific Drilling Program (ICDP) among other project partners, to characterize the subsurface edifice of the island in terms of volcanology, mineralogy, hydrology, chemistry and microbiology [18–20]. Of many bacteria isolated while studying the cultivable part of the subsurface prokaryotic diversity, the strains described here were selected because of their low 16S rRNA gene sequence similarity (~96 %) to other species.…”
Section: Isolation and Ecologymentioning
confidence: 99%
“…The active hydrothermal-seawater system discovered passes through the subsurface deposits, in which the maximal temperature of 124.6 • C in 2017 exceeded the presumed upper limit for functional life [22,[25][26][27][28]. Thirty-eight years later, three new cored boreholes (SE-02a, SE-02b, and SE-03) were drilled specifically for microbiological and geological analysis [29][30][31]. Over the years, many studies have explored the Surtsey edifice in terms of geology, mineral, and chemical composition, suggesting that fluid-rock interactions in the submarine Surtsey basaltic deposits behave similarly to basaltic oceanic crust [32][33][34][35][36].…”
Section: Introductionmentioning
confidence: 99%