Surprises from the drill pipe
Vogel subsequently wrote his MA thesis at the University of Umeå in Sweden about quick and low-cost ways to carry out a geochemical analysis of lake sediment cores. Later he wrote a dissertation at the University of Cologne about new methodological approaches to the analysis of drilling cores, for which he also worked on the history of the climate and environment in the northern Mediterranean region. So Hendrik Vogel has had a sustained in the potential of lake sediments in climate research. "I am interested in how a climate signal is stored in the lake," he explains. "Every lake is different, and you cannot always work with the same parameters: first of all you have to try to understand the lake as a system." That means that the geologist can never be certain what surprises a sediment core might produce on the day. He describes it as like "unwrapping a present."
The places where Hendrik Vogel has unwrapped scientific presents include Sweden, Antarctica, Macedonia and Albania as well as Siberia and Indonesia. Here on Lake Towuti in Sulawesi he is currently planning his most important field campaign to date. A test bore carried out in 2010, of which the photo with the improvised expedition boat is a souvenir, demonstrated the lake's potential as a climate archive - in a very important geographical area for the climate system. Lake Towuti is located at the centre of the so-called Indo-Pacific Warm Pool, whose characteristic feature is the unusually high temperatures of the ocean surface. Above this warm zone is the planet's biggest convection cell, one of the engines of atmospheric circulation. "If there is any change here, the knock-on effects are felt worldwide," says Vogel.
Traces on the sea bed
The aim of the drilling planned for 2015 is to bring up cores going right through the 250 metre thick layer of sediment down to the bedrock. It is hoped that analysis of this material will provide first class information in high temporal resolution about the climate history of the past 600,000 years. The focus will be on the hydrology and changes in precipitation over the course of time. These have left traces on the lake bed, since depending on how heavily and how much it rained, different elements like titanium or aluminium as a component of clay minerals would be washed in from the lake's drainage basin. And the newly installed X-ray fluorescence spectrometer in the lab in Bern enables Hendrik Vogel to detect their presence in the sediment layers with millimetre accuracy.
But one challenge remains: how can the various inputs be dated? To a certain extent Hendrik Vogel and his colleagues are placing their hopes, apart from established dating methods such as paleomagnetics, in a lucky break. It would be extremely helpful if they were to discover further datable layers of ash from known volcanic eruptions in addition to those already found.