Evolution research in Ohrid: The secret in Europe's oldest lake

 Lake Ohrid, Europe's oldest lake, lies between Macedonia and Albania. The deposits at its bottom are a unique climate archive. They show how new species arise - and then disappear again.

If you look down at the shimmering Lake Ohrid from the heights of the Galičica National Park, you can imagine for a moment that there are no hotels and restaurants, no shopping markets and factories. You can, at least for a moment, get a feeling for what it was like when the border region between Macedonia and Albania was deserted.

Evolution research in Ohrid

People have settled on the shores of the lake for about 6500 years, but the water has a much, much longer history. "The Ohrid lake is the oldest lake in Europe. It has existed for 1.36 million years without interruption," says geographer Bernd Wagner from the University of Cologne. "It's unique that we can track an ecosystem over such a long period of time."

For comparison, the age of the waters in Germany: Lake Constance, Müritz and others mostly emerged after the last ice age around 10,000 years ago when the glaciers melted. Only the Maar of the Eiffel are partly a bit older.

Lake Ohrid is a member of a rather exclusive club, that of the oldest lakes on earth. Lake Baikal, Tanganyika and Titicaca also belong to it. Together with colleagues, Wagner evaluated a 565 meter long sediment core with deposits from the bottom of the body of water. The samples are a unique archive for the development of the climate in the Mediterranean region. However, as the team now reports in the journal "Science Advances", they also allow a look into a unique laboratory of life.

"There are many endemic species that can only be found here," says evolutionary biologist Thomas Wilke from the University of Giessen. And whoever examines these species more closely, who studies their becoming and disappearing, can watch evolution at work.

He can see how long it takes for a new species to form in a new habitat and analyze their competition for habitat and food. And he can determine when and why they eventually disappear again. All of this information can be found in the innumerable layers of the sediment core, the oldest at the bottom and the youngest at the top. "The drill core is a picture book of the history of the lake," says Wilke.

The researchers know about 200 species that are unique to Lake Ohrid. The best known is the Ohrid trout, which is around 60 centimeters long and marked with colorful spots. Above all, Wilke and his colleagues had eyes for the much smaller lake inhabitants that can be found in the sediment: diatoms. The team was able to detect more than 150 different species of these so-called diatoms.

The diatoms have a hard shell made of silicon dioxide. And it is quite indestructible, which is why some of the specimens in the sediment survived many hundreds of thousands of years undamaged. Depending on their type, they show characteristic shapes and structures under the microscope. These individual characteristics helped the researchers to understand the time periods in which new species emerged in the lake - and when they finally became extinct again.

The new research overturns a paradigm of evolutionary researchers. Up until now, says Wilke, the following situation has been assumed: If a new habitat is created anywhere in the world, the formation rate of new species is high at the beginning because all species can still find a suitable habitat. In contrast, the rate of extinction, according to previous opinion, is very low at the beginning. "But it looks completely different," says Wilke, summarizing the findings from Lake Ohrid.

The analysis of the sediment showed that there were high rates of extinction even at the beginning of life in the lake. The evolutionary biologist explains that many species have found an ecological niche where competition was low. Often enough, however, this was unsuitable - and the species finally disappeared. Only gradually did the lake calm down: "In the beginning, many species only existed for a few thousand years," says Wilke. "But now there are millions." The lake's ecosystem has become stable over time.

More interesting than the Galápagos for evolutionary research

But what is the point if you know the speciation rates of algae in a lake in the Balkans? The researchers say that it can also be used to study the fate of other species in other parts of the world. "You'd think that such small algae come and go," says Wilke. "But the periods of time in which species of diatoms appear and disappear again are comparable to those of mammals." The researcher says that the diatoms from Lake Ohrid are "good models for evolution".

With the help of the tiny diatoms, one can even learn more about the development of the species than, for example, on the Galápagos Islands, which have been known for this since Charles Darwin, says Wilke. On the one hand, there are significantly more species in Lake Ohrid that are only found there. The larger sample makes the scientific analysis much more precise. On the other hand, the fossils of the diatoms are perfectly preserved in the sediment core. Of the species on the Galápagos, lizards and birds, fossil remains are largely missing.

Verschiedene Kieselalgen aus dem Ohridsee in einer nachkolorierten Rasterelektronenmikroskop-Aufnahme Foto Tom Wilke


At Lake Ohrid, you can see an example of what makes a stable ecosystem, says Wilke. After the turbulent early days, the communities remained amazingly stable, even if environmental factors had changed. Warm times and cold times came and went - and life went on. The species had found their place somewhere in deep lake water and had little to compete with each other. So they could withstand external stress comparatively well.

The lake can withstand a lot - but not everything


"The lake can buffer a lot," says Wilke. In principle, this is still the case today: Rising air temperatures in times of man-made climate change, nutrient abundance from agriculture, garbage, introduced species - the Ohrid Lake and life in it seem to have been able to cope with this so far, according to the researcher. But this impression is deceptive: "I can do a lot with the lake," warns Wilke. "But not everything."

To explain what can go wrong, the biologist cites the example of coral reefs in the world's oceans. These have been under stress for decades - due to overexploitation, garbage and dynamite fishing, for example. The rising water temperatures due to climate change as a further factor would have caused the reefs to tip over a tipping point in many places. Now the reefs are fighting for survival - and so it could also happen in the lake.

The aim must be to keep all pollution - from garbage and introduced species, for example - as low as possible so that the consequences of climate change do not bring the lake over the tipping point. When is this tipping point threatened? You can't really predict that, says Wilke. "A tiny change can be enough to cause a catastrophe." Then you lose not just one or two of the specialized species in the lake, but about 80 percent. "Then the cards are reshuffled and the struggle for survival begins again."

SOURCE: Der Spiegel (German), translated by Makedonien.mk


Further informations:

Deep drilling reveals massive shifts in evolutionary dynamics after formation of ancient ecosystem

Abstract
The scarcity of high-resolution empirical data directly tracking diversity over time limits our understanding of speciation and extinction dynamics and the drivers of rate changes. Here, we analyze a continuous species-level fossil record of endemic diatoms from ancient Lake Ohrid, along with environmental and climate indicator time series since lake formation 1.36 million years (Ma) ago. We show that speciation and extinction rates nearly simultaneously decreased in the environmentally dynamic phase after ecosystem formation and stabilized after deep-water conditions established in Lake Ohrid. As the lake deepens, we also see a switch in the macroevolutionary trade-off, resulting in a transition from a volatile assemblage of short-lived endemic species to a stable community of long-lived species. Our results emphasize the importance of the interplay between environmental/climate change, ecosystem stability, and environmental limits to diversity for diversification processes. The study also provides a new understanding of evolutionary dynamics in long-lived ecosystems.

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