Key Research

ARC scientists have determined that fish in arctic lakes depend on benthic (bottom-dwelling) plants and algae for food since phytoplankton growth is so low in most of these ecosystems.

This finding was revealed through a combination of long-term observations, lake fertilization experiments, and new 15N (nitrogen isotope) tracer methods that measure nitrogen cycling.

Arctic Alaska contains hundreds of thousands of lakes, almost all quite shallow. Research at the Arctic LTER on shallow lakes demonstrates that the food webs leading to fish are based mostly on primary production by bottom-dwelling algae rather than on plankton food webs. Yet, arctic fishery biologists continue to emphasize planktonic food webs and recent reviews of climate change in arctic freshwaters pay little attention to the benthic food web.

Comparisons of benthic and pelagic (i.e., excluding the lake bottom) primary production in lakes of various depths indicated that benthic production accounted for almost three quarters of total primary production in shallow lakes, and almost half of the primary production in deeper lakes ([1]Whalen et al. 2008). Additions of 15N to the upper waters of lakes demonstrated that almost all of the production of fish was derived from the benthic food web ([2] Hershey et al. 2006). Benthic invertebrates--mostly insects and snails living on the lake bottom--also impact nutrient cycling regimes in arctic lakes through grazing activities on benthic algae (Gettel et al. 2007). Snail enclosure experiments demonstrated that rates of nitrogen fixation increased with the density of snails. Results of these whole-lake and enclosure experiments represent some of the best examples of how animals influence nutrient cycling regimes in lake ecosystems.

Hershey AE, Beaty S, Fotino K, Kelly S, Keyse MD, Luecke C, O'Brien WJohn, Whalen SC. Stable isotope signatures of benthic invertebrates in arctic lakes indicate limited coupling to pelagic production. Limnology and Oceanography. 2006 ;51(1):177-188.

Citekey 192 not found

Hershey, A.E., S. Beaty, K. Fortino, S. Kelly, M. Keyse, C. Luecke, W.J. O'Brien, and S.C. Whalen. 2006. Stable isotope signatures of benthic invertebrates in arctic lakes demostrate limited coupling to pelagic production. Limno. Ocenogr. 51:177-188.
Gettel, G.M., A.E. Giblin, and R.W. Howarth. 2007. The effects of grazing by the snail Lymnaea elodes on benthic N2 fixation and primary production oligotrophic, arctic lakes. Limnol. Oceanogr. 52:2398-2409.

Whalen, S.C., B. A. Chalfant, and E.N. Fischer. 2008. Epipelic and pelagic primary porduction in Alaskan Arctic lakes of varying depth. Hydrobiologia 614:243-257. Google Scholar
 
Chris Luecke

 


References

Tracer Techniques

A tracer approach to investigation of the nitrogen (N) cycle of streams, first developed at the Arctic LTER, has transformed scientific understanding of the nitrogen cycle and food web structure in flowing waters.

Cascade Effect

The experimental addition of low levels of phosphorus to an arctic stream created a gradual transformation from a cobble-bottom stream covered with diatom-dominated biofilm to a moss-dominated bottom

Arctic Warming

Research at the Arctic LTER site is transforming scientific understanding of how the arctic landscape will respond to climate change. Warming of the Arctic is thawing previously frozen ground (permafrost) and in some places,

Linked Cycles

ARC LTER research over several decades has revealed strong linkages of carbon and nitrogen cycling through organic matter. This linkage is key to understanding and predicting changes in the arctic carbon cycle

Process Discovery

ARC scientists discovered that high concentrations of carbon dioxide and methane dissolved in groundwater are transported to arctic streams and rivers and released to the atmosphere.

Food Sources

ARC scientists have determined that fish in arctic lakes depend on benthic (bottom-dwelling) plants and algae for food since phytoplankton growth is so low in most of these ecosystems.