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New insights into the adaptive chloroplast capture in European white oaks

By de novo assembling 114 oak plastomes and analyzing 91 Fagaceae species, this study reveals that chloroplast capture in European white oaks likely occurred prior to the Last Glacial Maximum and may be driven by adaptive positive selection on key genes like *rbcL*, challenging previous assumptions about the timing and mechanisms of these evolutionary events.

Original authors: Dimitra Sergiadou, Daniel Wood, Luke T Dunning, Erik D Kjaer, Jill K Olofsson

Published 2026-11-05
📖 5 min read🧠 Deep dive

Original authors: Dimitra Sergiadou, Daniel Wood, Luke T Dunning, Erik D Kjaer, Jill K Olofsson

Original paper licensed under CC BY 4.0 (https://creativecommons.org/licenses/by/4.0/). ⚕️ This is an AI-generated explanation of a preprint that has not been peer-reviewed. It is not medical advice. Do not make health decisions based on this content. Read full disclaimer

Trees leave behind a quiet, complex history written in their DNA. For scientists trying to understand how plants evolve, the chloroplast is a particularly useful notebook. Found inside plant cells, these tiny structures act as solar panels, capturing sunlight to fuel growth. Unlike the main genome found in the cell's nucleus, which is a mix of genetic material from both parents, the chloroplast is usually passed down from only one parent, the mother. This makes it a stable, unbroken line of inheritance that rarely gets shuffled around. Because of this stability, scientists have long used chloroplast DNA to trace family trees and track how species moved across landscapes after ice ages. However, nature is rarely simple. Sometimes, when two different species of plants grow close together and crossbreed, the offspring can end up with the nuclear DNA of one parent but the chloroplast of the other. This event, known as chloroplast capture, can blur the lines between species, making it look like they are more closely related than they actually are. Understanding when and why this happens helps researchers piece together the true story of how forests survived the dramatic climate shifts of the past.

In a new study, researchers focused on two famous European trees: the pedunculate oak and the sessile oak. These two species are neighbors across much of Europe, often growing side by side and frequently mixing their genes. For decades, scientists have noticed that these two distinct trees look almost identical when you examine their chloroplast DNA. The prevailing theory was that this similarity was a recent event, a result of the trees swapping chloroplasts as they migrated northward after the last ice age, roughly twenty thousand years ago. To test this idea, the team gathered a massive amount of genetic data. They collected samples from over one hundred oak trees across twenty-one different locations in nine European countries, ranging from Turkey to the United Kingdom. Using modern sequencing technology, they reconstructed the complete chloroplast genomes for each tree, creating a detailed genetic map of the species. They then combined this new data with existing information from nearly one hundred other species in the beech and oak family to build a massive family tree and calculate exactly when different branches split apart.

The results of this deep dive revealed a more complicated history than the simple migration story suggested. The genetic analysis showed that the two oak species do not form two separate, clean groups based on their chloroplasts. Instead, the trees fell into three main genetic groups, or lineages, that were mixed together. A tree from Denmark might share the exact same chloroplast DNA as a tree from Poland or France, regardless of whether it is a pedunculate or sessile oak. This confirms that chloroplast capture has indeed happened, but the timing tells a different story. By analyzing the rate at which genetic mutations accumulate over time, the researchers estimated that the splits between these three main lineages occurred much earlier than the end of the last ice age. The oldest split between the lineages happened around 2.68 million years ago, and even the youngest splits within the groups date back hundreds of thousands of years. This suggests that the sharing of chloroplasts between these oaks was not just a recent accident of migration, but an event that began long before the glaciers retreated, possibly during earlier periods of climate change.

The study also looked for signs that this genetic swapping might have been driven by natural selection rather than just chance. The researchers examined the specific genes inside the chloroplast to see if any were being actively favored by evolution. They found evidence of positive selection in two specific genes. One of these genes, which helps build a crucial enzyme for photosynthesis, showed signs of a selective sweep. This means that a beneficial mutation likely spread rapidly through the population, replacing other variations and leaving the chloroplast DNA looking very uniform. This process could explain why the genetic diversity in these trees is so low. It is possible that a specific version of the chloroplast offered a survival advantage, perhaps helping the trees adapt to new environments, and as it spread, it carried the entire chloroplast genome with it.

Ultimately, this research reshapes our understanding of how these iconic trees have survived and evolved. While the old story of a simple post-ice-age migration explains some of the patterns, the new data points to a much deeper and more complex history. The chloroplasts of European white oaks have been mixing for millions of years, long before the last ice age ended. The study suggests that the low genetic diversity seen in these trees today is likely the result of ancient evolutionary forces, including natural selection acting on key genes, rather than just a recent mixing event. By combining whole-genome data with careful dating, the researchers have shown that the evolutionary history of these forests is not a straight line, but a tangled web of ancient connections and adaptive changes that continue to influence the trees we see today.

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