S
Sigurdur Brynjolfsson
Researcher at University of Iceland
Publications - 10
Citations - 478
Sigurdur Brynjolfsson is an academic researcher from University of Iceland. The author has contributed to research in topics: Phaeodactylum tricornutum & Fucoxanthin. The author has an hindex of 7, co-authored 10 publications receiving 364 citations.
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Maximizing biomass productivity and cell density of Chlorella vulgaris by using light-emitting diode-based photobioreactor.
Weiqi Fu,Olafur O Gudmundsson,Adam M. Feist,Gisli Herjolfsson,Sigurdur Brynjolfsson,Bernhard O. Palsson,Bernhard O. Palsson +6 more
TL;DR: Growth results were improved under the less expensive light of 660 nm LEDs, and illumination was augmented by optimization at systematic level, providing for a biomass productivity of up to 2.11 gDCW/L/day, the best results ever reported.
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Structural analysis of a transform fault-rift zone junction in North Iceland
TL;DR: In this paper, the authors provided a model for the tectonic development of these junctions, based on an analogy between two offset cuts (mode I fractures) loaded in tension and segments of the axial rift zones (or parts thereof in the case of the Husavik fault).
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Exploring Valuable Lipids in Diatoms
TL;DR: This review aims to summarize the recent advances in diatom lipid study and proposes some possible future directions and applications of diatom-derived lipids.
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Photo-Oxidative Stress-Driven Mutagenesis and Adaptive Evolution on the Marine Diatom Phaeodactylum tricornutum for Enhanced Carotenoid Accumulation
TL;DR: UVC radiation was utilized to induce mutations in the marine diatom Phaeodactylum tricornutum and screened strains with enhanced accumulation of neutral lipids and carotenoids and Adaptive laboratory evolution (ALE) was also used in parallel to develop altered phenotypic and biological functions in P. tricORNutum.
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Overlapping rift-zone segments and the evolution of the South Iceland Seismic Zone
TL;DR: The South Iceland seismic zone is a 20-60 km-wide (north-south) and up to 70 km-long zone of north and north-northeast trending dextral strike-slip faults buried by Holocene lava flows as discussed by the authors.