Researcher Egbert Schwartz and PolarTREC teacher Justin Kendhammer will travel to the Dry Valleys of Antarctica in search of life in the seemingly barren soil. One of the questions they will attempt to answer is whether microbes in the soil are native to Antarctic soil or whether they have been blown onto the continent from elsewhere in the world.
PolarTREC alumni and science teacher Bill Schmoker is taking his second research trip to the Arctic this summer as one of a handful of educators chosen as a Lindblad Expeditions National Geographic Grosvenor Teacher Fellow.
This article and associated video describe the findings of researchers who undertook core drilling at Lake El’gygytgyn, a lake that sits today inside a basin formed by a meteorite that struck the earth 3.6 million years ago. An associated video allows us to hear the enthusiasm and details as researcher Julie Brigham-Grette describes the findings of this remarkable discovery.
Density currents drive 3D movements within the world’s oceans that dwarf surface currents by volume. Density-driven movements due to temperature/salinity differences keep the world’s oceans well mixed & help to re-distribute heat from tropical areas towards polar areas. Resultant upwelling creates some of the world’s richest ocean ecosystems. Density movements known as turbidity currents are the world’s largest
Many students are familiar with topographic maps showing relief of land surfaces. In this lab they will produce their own bathymetric maps, the underwater equivalent. A bathymetric map shows sea floor features by contouring depths below sea level (instead of elevation above sea level as in topographic maps). Students will first probe depths in “Mystery Bay”, a box
Lake El'gygytgyn (67.5º N, 172º E) is one of the best preserved large asteroid impact craters on earth. In the winter of 2009, I joined an international science team and traveled to the frozen arctic lake to drill and extract lake sediments to study climate change as well as sample the rocks that were changed when the crater
The sediment in Lake El'gygytgyn, (pronounced EL-ge-GIT-gin) located in NE Siberia, holds one of the longest records of climate change anywhere in the continental Arctic. How does sediment (clay and mud) tell us something about past climate? Proxy data! By studying the microfossils of diatoms and pollen in the sediment, we can re-construct the lake environment millions of
Field Notes newsletter discusses research at Lake El'gygytgyn, and provides a link to follow Tim Martin's PolarTREC journals. Access the article using the link provided.