Nornickel's commitment to environmental science in its operational regions has become a cornerstone of its activities. A key focus is studying Arctic biodiversity and unique natural sites, including the relict Lake Mogilnoye on Kildin Island.
Layered “Pie”
Lake Mogilnoye on Kildin Island in the Kolsky District of the Murmansk Region is a rare relict water body, formed around 1,000 years ago. It's Russia's only lake with a multi-layered water structure. Once connected to the sea, a coastal barrier later sealed it off from the Barents Sea, creating an isolated ecosystem. Its hallmark? Distinct water layers stacked like a pie.
The top five-meter layer is crystal-clear freshwater. Below it mixes fresh and saltwater, while the third layer brims with high salinity—about 32 parts per thousand. The second layer steals the show: in summer, purple bacteria turn it a stunning pinkish hue, acting as a natural barrier by absorbing hydrogen sulfide and keeping it from rising.
Each layer hosts its own specialized life forms, thriving only under stable conditions. At the bottom, a hydrogen sulfide-rich layer remains lifeless.
DENIS EFREMOV
Senior Researcher, Laboratory of Fish and Aquatic Invertebrate Ecology, Karelian Research Center of the Russian Academy of Sciences:
"During our summer expedition, we confirmed the lake's ongoing connection to the sea. We recorded water flow through the dam at five meters depth—previously known but now precisely measured. This enables constant exchange between the lake and the Barents Sea: surface currents flow into the lake at high tide, and outflow occurs at low tide. These dynamics were undocumented in scientific literature before. We also verified the lake's sensitivity to precipitation. Over the course of our expedition, a fierce storm battered the area for 3–4 days, accompanied by relentless rain that raised the water level by roughly 25 centimeters. This is unusual for typical lakes, which feature drainage outlets."
Kildin cod is an endemic species found exclusively in the world's only known habitat: the unique Mogilnoye Lake, a small (560 by 280 m) body of water on the northern Kola Peninsula, off the southeastern coast of Kildin Island.
The lake's distinctiveness stems from its stratified layers of varying salinity. Kildin cod inhabits the middle layer—a roughly 4 m thick zone with salinity levels of 8–28%—venturing occasionally into the upper layers near shallow areas to feed. This peculiar environment played a pivotal role in the fish's evolution as a distinct subspecies. The cod entered the lake during its time as a marine lagoon and became isolated when a spit-barrier severed it from the sea around the 10th century.
What sets Kildin cod apart from Atlantic cod? Atlantic cod is a bottom-dwelling fish. It lives near the seabed, foraging for food like crabs, shrimp, and small fish. It boasts a large mouth, powerful jaws, and sharp teeth—a true predator that typically grows to 1.5 meters.
Kildin cod, by contrast, is much smaller, with the largest specimens reaching just 70 cm. It lives only 7–8 years, far short of the 20 years its marine relative enjoys.
Over time in the lake's confined conditions, Kildin cod has evolved distinct external traits: a larger head, smaller mouth, shorter jaws, and weaker teeth.
These adaptations stem from the lake's poorer food base compared to the sea. The Kildin cod feeds on whatever is available—small crustaceans and worms—so it no longer needs a large mouth or powerful jaws. Evolution has streamlined away the excess.
Another striking difference lies in reproduction. Atlantic cod spawns near the bottom, where eggs sink, adhere to rocks, and hatch into fry.
The Kildin cod cannot afford this: hydrogen sulfide in the lake bottom would kill the eggs. Instead, it spawns directly into the water column. The buoyant eggs drift and develop mid-water, showcasing the remarkable ingenuity Lake Mogilnoye inhabitants have evolved to survive.
*Integrated Ecosystem Condition Index (IECI) is a method for assessing ecosystem health, developed by the Siberian Branch of the Russian Academy of Sciences for Nornickel.
The methodology centers on collecting data about terrestrial and aquatic ecosystem components—flora, fauna, and soils—near Nornickel's industrial sites. These are compared against pristine background sites, whose indicators serve as the reference benchmark.
Currently, the IECI is being tested for applicability in Kola Peninsula nature reserves, including Pasvik, Lapland, and Kandalaksha. The diverse biological resources in these reserves make it scientifically compelling to verify the index's ability to detect industrial environmental impacts.