Person: Leena Inkinen
Leena Inkinen is one of Falkor (too)’s Pursers.
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Leena Inkinen is one of Falkor (too)’s Pursers.
Antonieta Clunes Reyes, 1983. Lives and works in Antofagasta, Northern Chile. Designer, transdisciplinary artist, and curator. She obtained her Diploma in Photography at the University of Chile and studied a Master of Media Arts at the same institution. As a researcher, she has led projects that address media archeology, such as Technoandinism: ancestral technologies of … Continued
The UN Ocean Decade Conference is a global forum where governments, leaders, maritime sectors, universities, NGOs, the private sector, and civil society will meet and new collaborations will be fostered, spurred by rich dialogue between science, policy, and society. Explore the Schmidt Ocean Institute events and talks below, or click here to view the full … Continued
Betzler, C., Hübscher, C., Lindhorst, S., Lüdmann, T., Hincke, C., Beaman, R., and Webster, J. (2024). Seismic stratigraphic and sedimentary record of a partial carbonate platform drowning, Queensland Plateau, north-east Australia. Marine Geology, 470, doi: 10.1016/j.margeo.2024.107255. [This article has been published as OPEN ACCESS].
Chen, C., Jamieson, J., and Tunnicliffe, V. (2024). Hydrothermal vent fauna of the Galapagos Rift: updated species list with new records. Marine Biodiversity, 54 (16), doi: 10.1007/s12526-024-01408-w. [This article has been published as OPEN ACCESS].
Final Expedition Report: Northern Depths of the Great Barrier Reef
Final Expedition Report: Biodiverse Borderlands
Osvaldo Ulloa is a Professor at the Department of Oceanography and Director of the Millennium Institute of Oceanography at the Universidad de Concepción in his native Chile. He is also a member of the Chilean Academy of Sciences. For the last twenty years, his research has focused on microbial phylogenetic diversity, environmental genomics, and biogeochemistry … Continued
Expedition dates: April 12 - May 15, 2024 Oxygen Minimum Zones, or OMZs, are areas in the water column with less oxygen, primarily due to naturally occurring physical and biological processes within the Ocean. The core of the OMZs is anoxic, making them inhospitable to most large animals, yet microbes have adapted to live and … Continued