A lake’s sediments are a window onto the past – the various layers deposited over time can provide valuable information on changes in local environmental conditions. Eawag researchers have studied how the settlement and economic development of the Joux Valley in Canton Vaud is reflected in the sediments of Lake Joux. By Andres Jordi
The Joux Valley in the Jura Mountains of Canton Vaud is mainly known as a traditional watchmaking centre. There is also some agriculture and, in the winter, the region attracts cross‑country skiing enthusiasts. The landscape is dominated by a lake with an area of around nine square kilometres – Lake Joux. The Joux Valley is now largely forested: Grand Risoux, for example, is Switzerland’s largest contiguous wooded area (Fig. 1). But in the past, it looked quite different. From the 14th century onwards, this remote high-lying valley was settled by farmers, who – to make the land more suitable for cattle breeding – drained wetlands and cleared large areas of forest.
However, the Joux Valley was not an ideal region for farming. Around the middle of the 15th century, the Little Ice Age brought increasingly cold and wet weather, leading to repeated crop failures and food shortages. The inhabitants, forced to diversify, began to exploit the remaining forests. The wood industry rapidly became an important source of income, and sawmills and charcoal burning flourished. Charcoal soon also fuelled the emerging metal industry. Along with iron mining, metalworking forges were established. In the 17th century, glassmakers and lapidaries also plied their trades. Finally, the late 18th century saw the introduction of watchmaking, which developed into the region’s most important sector in the 19th century. As a result of industrialization, agriculture declined, and cultivated fields were gradually replaced by pastureland or fallows.
Sediment archive dating back 1200 years
The history of human settlement in the Joux Valley is well documented in historical sources. But it is also recorded in the sediments of Lake Joux, as Nathalie Dubois – head of the Sedimentology group in Eawag’s Surface Waters department – explains: “Lake sediments are precious natural archives. Depending on the prevailing local conditions and influences, different substances are deposited on the lake bottom over time.” Scientists like Dubois who can interpret the various layers of sediments can thus gain valuable insights into a region’s history. Together with Marlène Lavrieux (a postdoc) and other co-workers, she investigated how the settlement and economic development of the Joux Valley is reflected in the sediments of Lake Joux.
For the study, sediment cores almost a metre long were extracted, using plastic tubes driven into the lake bottom (Fig. 2). Two cores were bisected, and samples were examined in detail in the laboratory: magnetic susceptibility and X-ray fluorescence scanning, density measurements and geochemical analyses were performed, as well as radiocarbon, lead-210 and caesium-137 dating. The sediment composition was also assessed visually with the aid of high-resolution photographs. “The cores date back around 1200 years,” says Dubois.
Erosion due to forest clearance
The sediment cores reveal the varied history of the Joux Valley (Fig. 3). Explaining the findings, Dubois notes: “Until the 13th century, environmental influences predominate, with the earliest settlers leaving no traces in the sediments.” Alternating layers of dark brown mud (known as gyttja) and lighter carbonate deposits indicate climatic fluctuations. The effects of human activities are first discernible in the overlying layers. Here, the plant constituents show a different pattern of long-chain hydrocarbons than in earlier layers. According to the researchers, this is due to a marked increase in inputs of organic matter to the lake, occurring between 1300 and 1450. During this period, numerous settlers arrived in the valley and began to clear the forests. Large amounts of organic matter from the bare soil were thus washed into Lake Joux. The increasingly wet climate – heralding the Little Ice Age – also contributed to soil erosion.