Journal Entry

We've now had the first official team meeting for the Lake Joyce expedition! After school yesterday, we convened on the U.C. Davis campus to meet each other and discuss the team's science goals for the coming expedition.

Researchers Tyler Mackey, Sasha Leidman, and Megan KrusorResearchers Tyler Mackey, Sasha Leidman and Megan Krusor at U.C. Davis

Tyler Mackey, our senior graduate student and one of our leaders, shared his past experiences in Antarctica with us and let us know what to expect this year. Megan Krusor, Sasha Leidman and I haven't been before, so we had lots of questions for Tyler. Along with learning about the logistics of the trip (which you'll see in future blogs), we got an overview of the scientific investigations we'll engage in.

Lake Joyce is home to the microbial communities that Megan introduced us to in the earlier video. Because this environment is so isolated, it limits who can live there, so there's really nothing preying on or burrowing through the microbes. This allows them to grow, forming mats that turn into really wonderful shapes that are very similar to microbial communities preserved in rocks from an earlier time on Earth. Below, you can see a photo of the modern mats on the left, and mats from 2.5 billion years ago on the right. In the ancient mats, the dark parts are inclusions of organic matter that are interpreted as layers of microbial mats. The white areas are carbonate minerals that precipitated on and within the mat to turn it into a rock:

Microbial Mats, Modern and AncientPhotos courtesy of Dale Andersen and Tyler Mackey

We are going to observe these mats, take samples and photographs, measure them and figure out how they change over time and in different environments. Hopefully, our insights will help us accurately interpret fossils from long ago.

In particular, we want to know how changes in the environment affect the mats. Due to climate change, the lake level has gone up by 7 meters in the last 30 years! This is largely due to glacial meltwater running off, bringing sediment with it. How much sediment is going into the lake, and where in the lake is it going? How does this influx of water and possibly nutrients affect the mat communities? These are some of the big questions we hope to explore during this field season.

Lake Joyce, 1947 to 2008Photos from Polar Geospatial Center and Google Earth, Courtesy of Anne Jungblut

I look forward to sharing more of our scientific processes as they unfold. I left our meeting with a better understanding of the science we’ll be doing and great sense that we’re going to have fun together in Antarctica!

Comments

Frank Z. Leidman

It's unclear to me why Megan Krusor and Sasha Leidman are not listed as team members on your blog, and why their profiles are not on the PolarTec site. Was this an inadvertent omission?

Guest

Your blog is wonderful.I love the clarity, the professional quality.
Also love your sense of wonder and scientific inquiry.

John Wood

Lucy,Your posts have been very interesting and a good beginning to understanding what you are facing on the expedition. You are so lucky to be that close to your team so all of you can get together. I'm sure that really helps put things into focus for you as well as already getting comfortable working together. Looking forward to more!
Cheers,
John

Lucy Coleman

This is a great question about who is listed on the expedition's homepage, and why! PolarTREC only features the teacher and the expedition's Principle Investigators on the homepage for the blog. In scientific terms, the PI's are the Team Leaders, and in this case, that's Dawn Sumner and Tyler Mackey. I should clarify that In total, though, there will be between 5-8 people at Lake Joyce who are each integral to the team. I hope to feature each person and their role in future blogs as I get to know them better.