Feeding hagfish
Credit: National Oceanic and Atmospheric Administration (NOAA),
Public domain, via Wikimedia Commons
Public domain, via Wikimedia Commons
Religion, Creationism, evolution, science and politics from a centre-left atheist humanist. The blog religious frauds tell lies about.
Hordle Cliff, Geology. Hordle Cliff is one of the most important and intensively studied fossil-bearing coastal exposures in southern England. Its significance lies in the exceptional sequence of Eocene marine sediments exposed by continual coastal erosion along the western Solent.The discovery and its broader significance were explained in a recent Natural History Museum news item by James Ashworth.
Geological setting
Hordle Cliff lies on the coast of Hampshire, west of Milford-on-Sea, forming part of the Hampshire Basin, a large sedimentary basin that accumulated marine and marginal-marine deposits during the early Cenozoic. The strata exposed here date mainly to the Late Eocene, approximately 41–34 million years ago, a time when southern England lay beneath a warm, shallow sea.
Stratigraphy
The cliff exposes a classic succession of Eocene formations, including:
- Barton Group (upper Eocene)
- Dominated by clays, silts, and fine sands
- Deposited in shallow marine conditions
- Exceptionally fossil-rich
- Barton Clay Formation
- The most famous unit at Hordle Cliff
- Known for abundant molluscs, sharks’ teeth, rays, fish remains, turtles, crocodilians, birds, and reptiles (including snakes)
- Indicates warm, subtropical seas with nearby coastal and estuarine environments
These sediments accumulated gradually, layer upon layer, in calm marine settings—exactly the opposite of the chaotic, high-energy deposition required by flood-geology models.
Depositional environment
During the Late Eocene, this region experienced:
- **Warm greenhouse climates
- High sea levels
- Low-energy marine sedimentation
Fine-grained clays settled slowly out of suspension, allowing delicate fossils to be preserved intact. Many beds show bioturbation, shell beds, and orderly fossil assemblages—clear evidence of stable ecosystems persisting over long periods.
Fossil significance
Hordle Cliff is internationally important because it preserves:
- Highly diverse faunas spanning multiple ecological niches
- Mosaic evolutionary forms, including transitional reptiles
- Fossils preserved in situ, not reworked or mixed from different ages
This makes the site particularly valuable for reconstructing Eocene ecosystems and tracing evolutionary change through time.
Structural and erosional features
The cliffs themselves are relatively soft and unstable:
- Frequent slumping and landslips continually expose fresh material
- Ongoing erosion has made Hordle Cliff productive for over two centuries
- The geology is simple and undisturbed, with gently dipping strata—no folding, overturning, or tectonic chaos
Why this matters for creationist claims
The geology of Hordle Cliff presents multiple, independent problems for young-Earth creationism:
- The sediments record millions of years of gradual deposition
- Fossils are ordered, local, and ecological, not globally mixed
- Climatic signals match global Eocene warming trends
- The strata fit seamlessly into the wider regional and global geological record
There is no evidence whatsoever of rapid, catastrophic deposition, let alone a single global flood. Instead, Hordle Cliff is a textbook example of slow geological processes operating exactly as modern geology predicts.
“Weird” new species of ancient fossil snake discovered in southern England
An extinct snake has slithered its way out of obscurity over four decades after its discovery.
The newly described species of reptile, Paradoxophidion richardoweni, is offering new clues in the search for the origin of ‘advanced’ snakes.
In 1981, the backbones of an ancient snake were uncovered at Hordle Cliff on England’s south coast. They’ve now been revealed as the remnants of a previously unknown species.
Research published in the journal Comptes Rendus Palevol has identified that the vertebrae belong to a new species named Paradoxophidion richardoweni. This animal would have lived around 37 million years ago, when England was home to a much wider range of snakes than it is now.
While little is known about this animal’s life, it could shed light on the early evolution of biggest group of modern snakes. This is because Paradoxophidion represents an early-branching member of the caenophidians, the group containing the vast majority of living snakes.
The new species is so early in the evolution of the caenophidians that it has a peculiar mix of characteristics now found in different snakes throughout this group. This mosaic of features is summed up in its genus name, with Paradoxophidion meaning ‘paradox snake’ in Greek.
Its species name, meanwhile, honours Sir Richard Owen. Not only did he name the first fossil snakes found at Hordle Cliff, but this scientist was also instrumental in establishing what’s now the Natural History Museum where the fossils are cared for, giving the name multiple layers of meaning.
Lead author Dr Georgios Georgalis, from the Institute of Systematics and Evolution of Animals of the Polish Academy of Sciences in Krakow, says that being able to describe a new species from our collections was ‘a dream come true’.
It was my childhood dream to be able to visit the Natural History Museum, let alone do research there, so, when I saw these very weird vertebrae in the collection and knew that they were something new, it was a fantastic feeling. It’s especially exciting to have described an early diverging caenophidian snake, as there’s not that much evidence about how they emerged. Paradoxophidion brings us closer to understanding how this happened.
Dr Georgios Georgalis, lead author
Institute of Systematics and Evolution of Animals
Polish Academy of Sciences
Krakow, Poland.
The most commonly found bones of fossil snakes are their vertebrae, which contain traits that scientists can use to identify the species.© Georgalis and Jones.
What’s been discovered at Hordle Cliff?
Hordle Cliff, near Christchurch on England’s south coast, provides a window into a period of Earth’s history known as the Eocene that lasted from around 56 to 34 million years ago.
Dr Marc Jones, our curator of fossil reptiles and amphibians who co-authored the research, says that this epoch saw dramatic climatic changes around the world.
Around 37 million years ago, England was much warmer than it is now, though the Sun was very slightly dimmer, levels of atmospheric carbon dioxide were much higher. England was also slightly closer to the equator, meaning that it received more heat from the Sun year round.
Dr Marc E.H. Jones, co-author
Curator of fossil reptiles and amphibians.
Natural History Museum
London, UK.
Fossils were first uncovered at Hordle Cliff around 200 years ago. In the early 1800s Barbara Rawdon-Hastings, the fossil-hunting Marchioness of Hastings, collected the skulls of crocodile relatives from the site, one of which Richard Owen would later name after her.
Since then, a variety of fossil turtles, lizards and mammals have also been uncovered at Hordle Cliff. There are also abundant snake fossils, including some particularly important species.
The fossil snakes found at Hordle Cliff were some of the first to be recognised when Richard Owen studied them in the mid-nineteenth century. They include Paleryx, the first named constrictor snake in the fossil record. Smaller snakes from this site, however, haven’t been as well investigated. Paradoxophidion’s vertebrae are just a few millimetres long, so historically they’ve not had a lot of attention.
Dr Georgios Georgalis.
To get a better look at these fossils, Marc and Georgios took CT scans of the bones. In total, they identified 31 vertebrae from different parts of the spine of Paradoxophidion.
We used these CT scans to make three dimensional models of the fossils. These provide a digital record of the specimen which we’ve shared online so that they can be studied by anyone, not just people who can come to the museum and use our microscopes.
Dr Marc E.H. Jones.
The scans show that the fossils are all slightly different shapes and sizes, as the snake’s spine bones gradually taper from head to tail. However, they share some features that show they all belong to one species.
Georgios estimates that Paradoxophidion would have been less than a metre long, but other details about this animal’s life are hard to say. The lack of a skull makes it difficult to know what it ate, while the vertebrae don’t have any sign of being adapted for a specialised lifestyle, such as burrowing.
A living link to the past?
Though the vertebrae don’t give much away about Paradoxophidion’s lifestyle, they are strikingly similar to a group of snakes known as the Acrochordids. These reptiles are known as elephant trunk snakes due to their unusually baggy skin.
Today, only a few species of these snakes can be found living in southeast Asia and northern Australia. But they’re among the earliest branches of the caenophidian family tree, with a fossil record extending back over 20 million years.
As Paradoxophidion is really similar to the acrochordids, it’s possible that this snake could be the oldest known member of this family. If it was, then it could mean that it was an aquatic species, as all Acrochordids are aquatic. On the other hand, it might belong to a completely different group of caenophidians. There’s just not enough evidence at the moment to prove how this snake might have lived, or which family it belongs to.
Dr Georgios Georgalis.
Finding out more about Paradoxophidion and the early evolution of the caenophidians means that more fossils will need to be studied. Georgios hopes to continue his work in our fossil reptile collections in the near future, where he believes more new species might be waiting.I’m planning to study a variety of snake fossils in the collection, including those originally studied by Richard Owen. These include the remains of the giant aquatic snake Palaeophis, which were first found in England in the nineteenth century. There are also several bones with differing morphology that haven’t been investigated before that I’m interested in looking at. These might represent new taxa and offer additional clues about snake evolution.
Dr Georgios Georgalis.
Publication:
A novel caenophidian serpent (Serpentes) peculiar to early divergence from the late Eocene of Hordle Cliff, EnglandTaken together, the geology of Hordle Cliff leaves no room for creationist evasions. The sediments accumulated slowly in warm, shallow Eocene seas, preserving stable marine ecosystems over millions of years. The fossils are local, ordered, and ecologically coherent, embedded within undisturbed strata that fit seamlessly into the wider geological history of southern England and the global Eocene record. None of this resembles the chaotic aftermath of a recent global catastrophe; all of it is exactly what conventional geology predicts.
We describe here a new genus and species of snake, based on several trunk and caudal vertebrae, from the late Eocene (MP 17a) of Hordle Cliff, England. We studied the fossil material using both visual microscopy and computed tomography (μCT), focusing on its intracolumnar variation and comparing it extensively with other Paleogene snake taxa from England and continental Europe. The new small taxon is characterized by a set of bizarre and distinctive vertebral features that may differentiate it from all other snakes. Its morphology is somewhat similar to that of russellophiids; however, some of its anatomical features are radically different from those seen in the latter group and thus defy such placement at the family level. Furthermore, the new English taxon bears a striking resemblance to extant acrochordids, particularly the species Acrochordus granulatus (Schneider, 1799). Consequently, we consider the new taxon to most likely represent an early divergent caenophid, possibly even a member of the Acrochordidae Bonaparte, 1831, well outside the stratigraphic and geographic distribution known to date for the latter group. It further adds to the astonishing diversity of vertebral morphologies in European Paleogene snakes.
Appendix 1. — Flythrough video of the μCT of the holotype trunk vertebra NHMUK PV R 10795.
Appendix 2. — Flythrough video of the μCT of the caudal vertebra NHMUK PV R 10796.
Georgalis G.L. & Jines M.E.H. (2025).
A new peculiar early diverging caenophidian snake (Serpentes) from the late Eocene of Hordle Cliff, England, in Georgalis G.L., Zaher H. & Laurin M. (eds) Snakes from the Cenozoic of Europe – towards a macroevolutionary and palaeobiogeographic synthesis.
Comptes Rendus Palevol 24 (25): 505-530. https://doi.org/10.5852/cr-palevol2025v24a25
Copyright: © 2025 The authors.
Published by [publisher]. Open access.
Reprinted under a Creative Commons Attribution 4.0 International license (CC BY 4.0)
What Were Docodontans? Docodontans were small, extinct mammaliforms that lived during the Jurassic period, between about 201 and 145 million years ago. Although not true mammals, they were close relatives and part of the larger group from which mammals evolved.
They are best known from their distinctive teeth, which had complex cusps adapted for an omnivorous diet of insects, plants, and other small food sources. Fossils suggest docodontans were shrew-like in size and appearance, with some adapted to specialised habitats – including burrowing, climbing, and even semi-aquatic lifestyles.
The group is important to palaeontologists because their anatomy preserves key stages in the evolution from reptile-like synapsids to the first true mammals. Discoveries like the one by Sofia Patrocínio help refine our understanding of when and how early mammal traits emerged.
Nova FCT student identified a new ancestor of mammals from a two-millimeter tooth
The fossil measures less than seven millimeters in total and is partially hidden in a rock. However, meticulous work has identified a new species that combines the name of a goddess with that of a constellation. The new species pushes back the emergence of this group of animals by 40 million years.
After several years of researching a molar tooth from an animal that might resemble a mouse and several months until she was able to publish the scientific article, Sofia Patrocínio "closed" this cycle on Friday, June 13, 2025. The result presented in the scientific journal Papers in Palaeontology owes nothing to bad luck, but it does have its share of incidents, as the paleontologist told ALMADENSE.
"There's a funny story from high school: I had to do a project on paleontology and got a failing grade; I was so upset I said it wouldn't happen again," she says in a relaxed conversation, while admitting that she loves what she does. And she does a lot of things, even though many of them aren't even paid. "Paleontology isn't seen as a serious profession." Something she's determined to change.
Sofia Patrocínio is from Cartaxo and graduated in Environmental Education and Nature Tourism. It's been more than half a dozen years since she enrolled in the program, but the price of student housing elsewhere was unaffordable (then, as it is now) , and it was one of the factors that forced her to stay closer to home and enroll at the Polytechnic Institute of Santarém. After that, she interned at Dino Parque da Lourinhã and stayed on to work there.
“It was them [my colleagues at Dino Parque] who encouraged me to do a master's degree in Paleontology at Nova; they said I had a knack for it,” he says, referring to the course at the Faculty of Science and Technology of the University of Lisbon (Nova FCT), which has a campus in the parish of Caparica, Almada.
It was impossible to remove the fossil from the rock due to the risk of damaging it. In the center of the image, the yellowish structure corresponds to the dentary (mandible), and the dark structure is the partially visible molar.Photo: Sofia Patrocínio
In one of her master's degree courses, Vertebrate Paleontology, Sofia Patrocínio and her colleagues were challenged to prepare and describe fossils, some from the Lourinhã Museum collection and some from an excavation in Greenland. The then-master's student worked with needles and a microscope to remove the sediments still clinging to the fossil, which was less than seven millimeters long —even so, she was unable to free the entire piece, as we will see.
She then described the fossil in detail and attempted to identify its group and its phylogenetic relationships with other animal groups—in other words, she attempted to place the animal in its proper position on the tree of life. "It had similarities with several groups, but didn't seem to belong to any. It was most likely a new species," says the researcher. "I had so much study material that I could have continued [with the same topic] for my master's degree."
How does a tooth allow us to identify a new species?
The first step was to include the species in the order Docodonta, a group of mammaliforms—the evolutionary predecessors of mammals—with very distinctive molars. To put it simply, the molars were long and low, with a characteristic cusp pattern. (Cusps are the conical protrusions on molars, which we also have.) But this particular tooth had characteristics that didn't fit into any of the previously known genera or species within docodonts.
Docodont fossils are very rare, but there are fossils with entire jaws, which allowed comparison with the available material and ruled out a tooth with a small defect. "If it were just a change in the tooth's morphology, there might be doubt, but I counted five to seven differences," explains Sofia Patrocínio. Among these differences was a cusp facing the tongue.
While the tooth's original pattern allowed it to be classified as a new species, the layer in which it was found offers another new discovery. To determine the age of fossils, paleontologists "measure" the age of rocks found in the same layer. In this case, the fossil would have formed about 200 million years ago, during the transition between the Triassic and Jurassic periods (the period in which a wide variety of easily recognizable dinosaurs emerged). Even more interesting is that this species would have appeared 40 million years before the oldest known docodont species.
A new species at the transition between pre-docodont mammals and docodonts adds another piece to the puzzle of mammalian evolution, particularly the order Docodonta, which diversified and occupied various environments at the same time as large dinosaurs roamed the Earth. Furthermore, this fossil places the origin of docodonts in Greenland and Europe—connected before the continents separated into their current positions—rather than Russia and Asia as previously thought.
The layers of soil containing the fossils are like shelves in a bookcase, each corresponding to a period of time. By exploring each shelf as if reading the books stored there, the scientists were able to date the layer and the fossils—among them a new species of dinosaur, Plateosaurus trossingensis, identified by a fellow student in Sofia's master's program — and also describe the environment. The fossils were found in an ancient lake, with little oxygen in the water and which served as a passageway for many animals.
200 million years ago, when the 'Nujalikodon cassiopeiae' fossil is believed to have formed, what are now Greenland and Europe were connected, and also in contact with the continental plates of North America and Asia.Adapted from: Patrocínio et al. (2025) Papers in Paleontology
A goddess tooth named after a constellation
Now 25, Sofia Patrocínio boasts the identification of a new species on her resume. "It's strange; it seems like it hasn't sunk in yet." Whoever discovers a new species can give it a name, naturally following the rules used by the scientific community. A species always has two Latin names (first the genus name, which functions almost like our surnames, and then the "proper name" that conveys the distinctive characteristic), as defined by the scientist Carlos Linnaeus in the mid-18th century.
This new docodont was named Nujalikodon cassiopeiae . Nujalik is the goddess of the earth hunt in Inuit mythology—the indigenous population of the Arctic regions of Canada, Alaska, and Greenland—and "nujalikodon" means "Nujalik's tooth." The specific epithet cassiopeiae owes its name to the constellation Cassiopeia, whose five stars appear to form a W, like the cusps of the molar Sofia Patrocínio studied.
Naming the species requires all the prior work of studying fossils, in this case a complete molar, the piece of bone that housed the tooth, and the broken roots of a second tooth. But a large portion of the fossil was not visible; it was still embedded within the rock, and removing it could irreparably damage the tooth. Furthermore, it was extremely small, the molar measuring only two millimeters. Therefore, a scan of the fossil was necessary—a kind of CT scan for very small objects—which was very difficult to achieve, says the researcher. "But without the scan, it was impossible to move forward, nor to submit the article for publication." Then, using the 831 photographs from the scan—as if the fossil had been cut into very thin slices—a three-dimensional model was created on the computer, allowing us to see the details hidden within the rock.
The 831 photographs taken by the scan allowed a three-dimensional reconstruction of the fossil measuring just seven millimeters.Adapted from Patrocínio et al. (2025) Papers in Paleontology
Sofia Patrocínio's work was supported by her advisors, Vicente Crespo, a paleontologist at Nova FCT, and Elsa Panciroli, a researcher at the National Museum of Scotland, and involved collaboration with other researchers. The work was funded by the Foundation for Science and Technology, as part of the GeoBioTec project.
Having completed this stage, the paleontologist hopes to continue studying the evolution of mammalian ancestors with a doctorate from the Instituto Superior Técnico of the University of Lisbon. This time, she will study the inner ear—but she will continue to observe bones and very small structures. In the meantime, she will participate in paleontological excavations, collaborate with a fossil database in Portugal, and, in the activities she organizes for Ciência Viva, try to spark children's interest in paleontology.
Publication:
ABSTRACTThis fossil tooth extends the known existence of docodontans by around 40 million years, placing them much earlier in the evolutionary timeline than previously documented. This is significant because:
The first mammaliaforms emerged in the Late Triassic, but their exact origins remain unclear due to the scarcity of fossils from this period. One of the earliest diverging mammaliaform groups, the order Docodonta, became unusually ecomorphologically diverse compared with other early mammals, and this may be connected to the possession of complex molar cusp morphology. The specimen described here, found in the Rhætelv Formation of the Kap Stewart Group (Rhaetian–Sinemurian) of central East Greenland, provides novel information on docodontan origins and evolution, as well as key biogeographic insights into early mammal dispersal. Nujalikodon cassiopeiae gen. et sp. nov. is the first mammaliaform found in the Rhætelv Formation, and is likely to be Early Jurassic (Hettangian) in age. Comprising an incomplete dentary with a single preserved molar, it was visualized using micro-computed tomography; the molar bears similarities to the putative early docodontan Delsatia, and docodontan Dobunnodon. Phylogenetic analysis places Nujalikodon cassiopeiae as a basal member of Docodonta or a close sister taxon, making it one of the oldest definitive docodontans and pushing the origin of the group back to at least the Early Jurassic. It provides insights into the development of docodontan dental complexity, a key factor in their ecological diversification during the Middle to Late Jurassic. Its presence in Greenland supports the hypothesis that docodontans originated in the region now comprising Europe and Greenland before dispersing across the rest of Laurasia.
Patrocínio, S., Panciroli, E., Rotatori, F.M., Mateus, O., Milàn, J., Clemmensen, L.B. and Crespo, V.D. (2025)
The oldest definitive docodontan from central East Greenland sheds light on the origin of the clade. Pap Palaeontol, 11: e70022. https://doi.org/10.1002/spp2.70022
© 2025 John Wiley & Sons, Inc.
Reprinted under the terms of s60 of the Copyright, Designs and Patents Act 1988.