Lakes and streams in the foothills near Toolik Lake, Alaska, at 68 degrees
N have been studied since 1975 to predict physical, chemical and biological
impacts of future global change. Experimental manipulations include whole
lake and continuous stream fertilization as well as removal and addition of
predators (copepods, lake trout, grayling, sculpin). Based on our evidence
the following scenario is likely. Warming thaws the upper layers of permaf
rost and streams and lakes become enriched with phosphorus. Streams respond
quickly with higher production of diatoms but animal grazers keep biomass
changes to a minimum. Fish productivity also increases. If phosphorus level
s are too high, mosses become the dominant primary producer and sequester a
ll of the nutrients. Growth of Arctic grayling under the present conditions
only occurs in summers with higher than average stream flow. The present p
opulation would be stressed by warmer temperatures. When higher phosphorus
levels reach lakes and cause slight eutrophication, the number of trophic l
evels will increase, especially within the microbial food web. Warmer lake
temperatures increase stratification and, combined with eutrophication, cou
ld decrease oxygen in the hypolimnion. Oxygen levels will also decrease in
winter under the ice cover. Eventually this habitat change will eliminate t
he lake trout, a top predator. Removal of lake trout results in a striking
increase in abundance and productivity of smaller fish, including small lak
e trout, and the emergence of burbot as an alternate top predator. Large sp
ecies of zooplankton will become virtually extinct.