Onboard the Deepscan vessel with Adrian Shine, we coasted over calm waters to the centre of the loch where the sonar indicated the depth below us was 223 meters. While stationary on the surface, we lowered the sediment corer, handing off rope and responsibility between our team members as the transparent, cylindrical sampling vessel made its journey down. Inside the boat’s cabin, we could see the object’s descent recognized by the sonar system and depicted on the screen. Outside by the winch, we waited with bated breath to feel the tether jolt when the meter-long tube lands and fills with lake-floor substrate; the plunger fires on impact, creating a pressure imbalance that holds the sediment layers exactly where they are while we retrieve the messenger and cap it for transport back to UCL.
By collecting the silt, clay, and other organic matter that has accumulated at the base of this dimictic loch, paleolimnologists can recognize distinct laminae, particles, and even fossils to compose a timeline of Loch Ness history. These biological proxies not only inform how water bodies respond to and record changes in the environment, such as pollution or acidification, but also facilitate an in-depth understanding of past ecosystems. In 1997, a paper co-written by scientists of the UCL Environmental Change Research Centre and Adrian Shrine of the Loch Ness Research Unit demonstrated how sediment profiles can represent a baseline for pre-anthropogenic pollution levels as well present levels of accumulated pollutants and an approximate timeline of particulate presence. Three specific markers discussed in this study include: benthic and planktonic diatoms, whose relative presence indicate changes in loch productivity from nutrient enrichment; spheroidal carbonaceous particles (SCPs) produced by the combustion of fossil fuels, which first appear between 1850 and 1870 and become more abundant in the mid-20th century; and radionuclides Caesium 137, Americium 241, and Caesium 134, which depict the permanently traceable deposition of
fallout from weapons testing and the meltdown at Chernobyl Nuclear Power Plant.