Trace metal and phosphorus dynamics in Lake Superior

We have been working on issues of the cycling of trace elements and their interaction with phytoplankton in Lake Superior, since 1999. The most recent project was funded by NSF (Bob Sterner, U. Minnesota, lead PI) and focuses on the dynamics of the nitrogen cycle in the lake. The Sherrell lab has contributed to this effort by studying the seasonal and geographical distribution of bioactive trace metals (e.g. Fe, Zn, Cu, Cd) and by developing the methods to measure the very low concentrations of dissolved phosphorus in this large oligotrophic lake.

Graduate student Yongcheng Ji (PhD 2006; MAKE PDF LINK) explored the relationship between the unusually large uptake of Zn by the microbial assemblage in the lake and the extreme limitation of primary production by phosphorus. Graduate student Eleni Anagnostou (MS 2005; now a PhD student) developed and applied a new method for detecting very low nanomolar concentrations of dissolved inorganic P, while RIAL lab manager Paul Field and PI Sherrell found ways to improve the sensitivity of ICP-MS for measuring low concentrations of total dissolved P (including dissolved organic P). With these methods, we are gaining an understanding of P dynamics in large lakes when there is very little of it available to the biota. These findings help to shed light on P cycling in the oligotrophic ocean.

Figure 1: Rob Sherrell and Rutgers graduate student Yongcheng Ji near Devil's Island, Lake Superior


Figure 2: Rob Sherrell (in red) with postdoc Sanjeev Kumar and technician Jason Agnich (U. Minn.) aborad the R/V Blue Heron outside Duluth, MN.

Figure 3: Rutgers graduate student Eleni Anagnostou sampling uncontaminated surface water (tube over pulley behind) near the Apostle Islands, Lake Superior


Figure 4: Erosion of water caves in very old sedimentary rocks on Devil's Island, Lake Superior