The Suboxic Zone in the Black Sea
When: November 2, 2004 2:30PM PST
The Black Sea is a large permanent anoxic basin that has been considered an analog for the ancient earth’s ocean. This sea has an oxic surface layer over an anoxic (sulfide containing) deep layer. At the boundary there is a layer that is about 50 m thick with no oxygen or sulfide. In this layer there are many interesting intermediate redox reactions involving species of Fe, Mn and N.
To join using a videoconferencing system:
Please RSVP to Mike Toillion (email@example.com) if you will be joining by Polycom.
To view the slides, connect to http://connect.arc.nasa.gov/uwseminar/
To join using a web browser:
The slides and audio/video for this meeting will be presented using Adobe Connect. To join the meeting, connect to:
If you are having problems connecting, you can try joining http://connect.arc.nasa.gov/uwseminar/?launcher=false, or rebooting your computer, or try joining from another network.