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Michael Schlüter

Researcher at Alfred Wegener Institute for Polar and Marine Research

Publications -  174
Citations -  6180

Michael Schlüter is an academic researcher from Alfred Wegener Institute for Polar and Marine Research. The author has contributed to research in topics: Catheter ablation & Water column. The author has an hindex of 37, co-authored 174 publications receiving 5643 citations. Previous affiliations of Michael Schlüter include University of Kiel & University of Bremen.

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Novel microbial communities of the Haakon Mosby mud volcano and their role as a methane sink

TL;DR: It is found that the upward flow of sulphate- and oxygen-free mud volcano fluids restricts the availability of these electron acceptors for methane oxidation, and hence the habitat range of methanotrophs, which limits the capacity of the microbial methane filter at active marine mud volcanoes to <40% of the total flux.
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Rhizon sampling of porewaters near the sediment‐water interface of aquatic systems

TL;DR: In this article, a newly developed Rhizon in situ sampler (RISS) is presented for porewater sampling from sediments in aquatic systems and the results revealed that horizontally aligned Rhizons can sample pore water with a vertical resolution of 1 cm.
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Radiofrequency current catheter ablation of accessory atrioventricular pathways.

TL;DR: It is concluded that radiofrequency current catheter ablation is both effective and safe for patients with symptomatic tachyarrhythmias mediated by accessory atrioventricular pathways.
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Acute outcomes of MitraClip therapy for mitral regurgitation in high-surgical-risk patients: emphasis on adverse valve morphology and severe left ventricular dysfunction

TL;DR: Mitral valve repair using the MitraClip system was shown to be feasible in patients at high surgical risk primarily determined by an adverse mitral valve morphology and/or severe LV dysfunction.
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Methane discharge from a deep-sea submarine mud volcano into the upper water column by gas hydrate-coated methane bubbles

TL;DR: In this article, it was shown that a significant portion of the methane from discharged methane bubbles can reach the upper water column, which may be explained due to the formation of hydrate skins.