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Editors' notes This article has been reviewed according to Science X's editorial process and policies. Editors have highlighted the following attributes while ensuring the content's credibility: fact-checked peer-reviewed publication proofread In a warmer climate, summers warm much faster than winters. That is the conclusion of research into fossil shells by Earth scientist Niels de Winter. With this knowledge, we can better map the consequences of current global warming in the North Sea area. Alongside colleagues from institutions such as the Institute for Natural Sciences in Brussels, de Winter, affiliated with the Department of Earth Sciences at Vrije Universiteit Amsterdam and the AMGC research group at Vrije Universiteit Brussel, measured the chemical composition of fossil shells from Antwerp, Belgium. Those shells originate from mollusks such as oysters, cockles, and scallops found during the construction works of the Kieldrecht Lock. The mollusks lived during the Pliocene, approximately three million years ago, in the North Sea, which at that time also covered parts of Flanders and the Netherlands. The shells grew layer by layer, much like tree rings or fingernails, and stored very detailed information in their shell during their lifetime. During the Pliocene, the Earth was on average 2.5 to 3 degrees Celsius warmer than it is now. In their study, published in Science Advances, the researchers took a "snapshot" of the climate at that time to gain insight into the difference between the seasons in a warmer climate. They use the "clumped isotope analysis" method. With this method, researchers study the composition of shells in even more detail. They do this by measuring the extent to which rare heavy isotopes of both oxygen and carbon occur in the same carbonate from which shells are built. These isotopes are more common in shells that formed in colder waters. As a result, the measurements can be used to reconstruct the temperature at which the shells were formed. This method is more accurate than conventional methods for temperature reconstructions because it does not rely on assumptions about the composition of the seawater in which the mollusks grew. The key insight is that summers warm much more than winters in a warmer climate such as the Pliocene. While winters became about 2.5 degrees warmer, temperatures during summer were about 4.3 degrees higher. The researchers see a similar result in models projecting future climate, which predict roughly the same amount of warming for the year 2100. The study gives us a glimpse of what the climate in Europe will be like if we continue our current trend toward a warmer world. De Winter said, "We will likely experience stronger temperature differences between summer and winter, and the chance of heat waves during the summer will increase." More information: Niels de Winter, Amplified seasonality in western Europe in a warmer world, Science Advances (2024). DOI: 10.1126/sciadv.adl6717. www.science.org/doi/10.1126/sciadv.adl6717 Journal information: Science Advances Provided by Vrije Universiteit Brussel