Fossils from the Early Cretaceous Period at the Swiss Museum

Paleontologists have identified a new species within the extinct turtle genus Craspedochelys, based on some remarkable fossil shells and subsequent bones discovered in Colombia.



Artistic reconstruction of Craspedochelys Renzi and the shallow marine ecosystem it inhabited. The flip-like shape of the forelimbs is inspired by the most complete known specimen of Thalassemys bruntrutana. Image credit: Juan Guilard.

Craspedochelys Renzi thrived during the early Cretaceous Hauterivian period, approximately 132 to 125 million years ago.

This ancient species belonged to the Thalassocheridia, a group of marine-adapted turtles from the Jurassic and Cretaceous eras.

“Throughout their evolutionary journey, various unrelated turtle groups have developed adaptations for marine and coastal habitats,” says Dr. Edwin Alberto Cadena, a paleontologist at the Smithsonian Tropical Research Institute of Natural History.

“One such group is the Thalassocheridia, traditionally classified into three Jurassic families: Eurysternidae, Plesiochelyidae, and Thalassemydidae, which have complex and often debated phylogenetic relationships.”

“Among these families, the ‘Plesiochelyidae’ is particularly diverse, encompassing at least ten species across four different genera: Craspedochelys, Plesiochelys, Portlandomys, and Tropidemys.”

“The shells of ‘Plesiochelyids’ can be distinguished from other thalassocheridians by their large size (40-55 cm in shell length), with adults lacking the thyroid cortex of the hanging skin, typically displaying only a thick layer of fontanel in the center.”



Craspedochelys Renzi is characterized by a distinct shell featuring several occipital bones. Image credits: Cadena et al. , doi: 10.1186/s13358-025-00394-1.

The fossil specimen of Craspedochelys Renzi was first discovered by Swiss geologist Otto Lenz during a field expedition in the Cunja de Cuisa region of Guazila Province, Colombia, in the 1950s.

This specimen included partial shells measuring 25.5 cm long and 23.1 cm wide, along with hind limb bones and caudal vertebrae.

It was later stored in the paleontological collection of the Naturhistorisches Museum Basel in Switzerland, where it remained unnoticed for over 60 years among the fossil invertebrate collection.

“Geological evidence connects these specimens to shallow marine sediments from the Moina Formation, dating to the Hauterivian,” the paleontologist explained.

This fossil represents the youngest known occurrence of Thalassocheridians globally during the Hauterivian, and it is the second record from a non-European group.

“The discovery of Craspedochelys Renzi will greatly enhance our understanding of Thalassocheridians, particularly the ‘Plesiochelyidae’, expanding their geographical range to North Gondwana and temporal range to the Hauterivian,” the researchers stated.

“This find underlines the significance of reevaluating historical collections and the potential for future discoveries in less explored areas such as northern South America.”

“The existence of Craspedochelys Renzi in the Moina Formation further underscores the intricate paleobiogeographic history of early Cretaceous coastal habitats and marine turtles.”

“It also offers new perspectives on the evolutionary dynamics of Thalassocheridia and the still unresolved, unstable phylogenetic relationships within the group, which necessitates further detailed investigation in future research.”

The discovery of Craspedochelys Renzi is discussed in a paper published in the Swiss Journal of Palaeontology.

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ea. Cadena et al. 2025. The first occurrence of the “Plesiochelyidae” turtle in the early Cretaceous period of South America. Swiss J Palaeontol 144, 52; doi:10.1186/s13358-025-00394-1

Source: www.sci.news

Giant Glacier Collapse Triggers Landslides, Engulfs Swiss Villages

The Birch Glacier triggered an avalanche of ice, snow, water, and rocks as its edge collapsed.

Jean-Christophe Bott/EPA-EFE/Shutterstock

Many glaciers in the Swiss Alps separated from the mountains, resulting in debris, mud, and ice crashing down onto the village of Blatten.

Authorities had been warning for weeks about the potential collapse of the Birch Glacier due to visible cracks in the ice. Earlier this month, both residents and livestock were evacuated from Bratten, a village situated in the valley beneath the glacier, which houses around 300 individuals.

Webcams and drone footage captured on the 28th show massive clouds of debris swirling through the Alpine valley as the glacier gives way, with immense flows of mud and rock blanketing the hillside and much of the village.

A press briefing in a nearby settlement on May 28th reported one person missing, though there were no immediate casualties. Much of Bratten is now covered beneath debris. The glacial collapse also registered as a 3.1 magnitude earthquake on the Richter scale, according to seismic data.

Images from the location indicate that, in addition to the village, vast expanses of forest have been devastated, which has dammed the nearby Lonza River, heightening the risk of floods in the area.

“Nature is more powerful than humanity. Those living in the mountains understand this. However, today we witnessed an exceptional event. It’s deeply disturbing to see the aftermath,” reported a Swiss news outlet.

As global temperatures rise, Alpine glaciers are becoming increasingly unstable. Official statistics show that in Switzerland, glaciers lost 10% of their volume between 2022 and 2023.

The melting of glaciers leads to the collapse of rocks and ice, resulting in debris flows into the valleys below. Research indicates that climate change is contributing to an increase in small rockfalls and landslides in the Alps.

However, further investigation is necessary to understand the specific events that transpired in Blatten, as stated by Mylène Jacquemart from ETH Zurich, who will assess the extent of the glacier failures and the underlying reasons. “Clearly, incidents similar to Bratten are rare. This is a complicated sequence of processes,” she elaborated.

Jack Mart emphasized the challenge of detecting changes in the frequency and severity of significant landslides.

“The alterations induced by climate change in the alpine regions (such as increased melting, reduced snow cover, warmer temperatures, and more rain than snow) negatively affect rock stability,” she noted. “Yet, could this series of events have occurred without climate change? It’s possible. A crucial question in hazard management is whether there is a noticeable rise in the frequency of certain events. Are occurrences that previously happened every decade now becoming more frequent?

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Source: www.newscientist.com