![]() |
Lytoceras sp. Photo: Craig Chivers |
![]() |
The concretion prior to prep |
![]() |
Lytoceras sp. Photo: Craig Chivers |
![]() |
The concretion prior to prep |
Florence Filberg Centre, 411 Anderton Avenue, Courtenay, British Columbia, on the Traditional Territory of the K’ómoks First Nation, August 22-25, 2025
CELEBRATING THE PALEONTOLOGICAL BOUNTY OF THE COMOX VALLEY
The conference features over a dozen speakers in paleontology from Vancouver Island, mainland British Columbia, and beyond.
This year, we’re celebrating Courtenay’s own Traskasaura sandrae—a 12-metre-long marine elasmosaur discovered by Mike Trask along the Puntledge River. The fossil was recently named in the Journal of Systematic Paleontology, earning international recognition.
Traskasaura sandrae is a newly identified genus and species of elasmosaurid plesiosaur, a long-necked marine reptile, discovered in British Columbia, Canada.
The fossil, found along the Puntledge River on Vancouver Island, are from the Late Cretaceous (Santonian age), roughly 86 to 84 million years ago. Traskasaura sandrae is notable for its robust teeth, potentially adapted for crushing ammonites, and a unique mix of primitive and derived skeletal features, suggesting it was a powerful predator adapted for diving.
As well as highlighting this significant find and honouring the amazing life of Mike Trask, the symposium has an exciting lineup of scientific presentations, hands-on workshops, a paleontology-themed art exhibition, poster presentations, and guided field trips.
These events provide exciting opportunities to explore and celebrate the rich geological and paleontological history of Vancouver Island, bringing together world-renowned paleontologists, citizen scientists, fossil enthusiasts, researchers, artists, and the public in a vibrant exchange of ideas and inspiration.
Our Keynote Speaker is Dr. Kirk Johnson, Sant Director of the Smithsonian’s National Museum of Natural History, where he oversees the world's largest natural history collection.
As a field paleontologist, he has led expeditions in eighteen US states and eleven countries with a research focus on fossil plants and the extinction of the dinosaurs. He is known for his scientific articles, popular books, museum exhibitions, documentaries, and collaborations with artists.
BRITISH COLUMBIA PALEONTOLOGICAL ALLIANCE (BCPA)
The British Columbia Paleontological Alliance (BCPA) is a collaborative network of organisations led by professional and citizen scientists, working to advance the science of paleontology in the province.
Together, they promote fossil research and discovery through public education, responsible scientific collecting, and open communication among paleontologists, citizen scientists, fossil enthusiasts, researchers, and educators.
Every two years, the BCPA hosts a Paleontological Symposium, bringing together experts and the public from across Canada, North America, and beyond to share the latest research and discoveries related to British Columbia's fossil heritage. To learn more, visit www.bcfossils.ca.
VANCOUVER ISLAND PALEONTOLOGICAL SOCIETY (HOST ORGANIZATION):
This year, the Vancouver Island Paleontological Society (VIPS) is proud to host the 15th BCPA Symposium in Courtenay, in partnership with the Courtenay and District Museum & Palaeontology Centre.
Founded in 1992 and based in the Comox Valley, VIPS is a nonprofit society with charitable status in good standing dedicated to fostering public engagement with the natural world through field trips, workshops, symposia, and public lectures that bring science to life for the community.
COMMUNITY SPONSORSHIP, SILENT AUCTION ITEMS & WELCOME BAGS:
As host, the VIPS is currently welcoming sponsorship contributions and donations for the symposium's silent auction to help us offset conference costs, including printing, venue rental, catering, insurance, and participant support. We are also seeking items to include in our Welcome Bags for conference attendees, offering an excellent opportunity to showcase local businesses and community spirit.
Sponsors will be publicly recognised at the conference, within the Courtenay and District Museum, and across our social media platforms. Tax receipts are available for eligible donations.
Sponsorship cheques made out to the Vancouver Island Paleontological Society can be mailed to 930 Sandpines Drive, Comox, BC, V9M 3V3. Attn: 15th BCPA Symposium 2025.
We would be honoured to have your support—your contribution would bring meaningful value to this exciting scientific event. If you have an item to donate to our silent auction or to include in our Welcome Bags, we would be sincerely grateful and can arrange for convenient pickup.
To get involved or learn more, please contact us at bcpaleo.events@gmail.com—we’d love to hear from you!
Warm regards on behalf of the 15th BCPA Organising Committee.
Misty shores, moss-covered forests, dappled light, and the smell of salt air—these are my memories of Haida Gwaii, a land where ancient stories are written in stone.
Formerly known as the Queen Charlotte Islands, the archipelago of Haida Gwaii lies at the far western edge of Canada, where the Pacific Ocean meets the continental shelf. These islands—steeped in the rich culture of the Haida Nation—are not only a cultural treasure but a geologic and paleontological wonderland.
Geologically, Haida Gwaii is part of Wrangellia, an exotic tectonostratigraphic terrane that also includes parts of Vancouver Island, western British Columbia, and Alaska. The region's complex geological history spans hundreds of millions of years and includes volcanic arcs, seafloor spreading, and the accretion of entire landmasses.
The Geological Survey of Canada (GSC) has long been fascinated with these remote islands. Their geologists and paleontologists have led numerous expeditions over the past century, documenting the diverse sedimentary formations and fossiliferous beds. Much of the foundation for this work was laid by Joseph Frederick Whiteaves, the GSC’s chief paleontologist in Ottawa during the late 19th century.
In 1876, Whiteaves published a pioneering paper on the Jurassic and Cretaceous faunas of Skidegate Inlet. This work firmly established the paleontological significance of the archipelago and cemented Whiteaves’ reputation as a global authority in the field. His paper, "On the Fossils of the Cretaceous Rocks of British Columbia" (GSC Report of Progress for 1876–77), remains a key early reference for West Coast palaeontology.
Later, Whiteaves would go on to describe Anomalocaris canadensis from the Burgess Shale—an “unlike other shrimp” fossil that would later be recognized as one of the most extraordinary creatures of the Cambrian explosion.Whiteaves' early work on the fossil faunas of Haida Gwaii, particularly in the Haida Formation, created a foundation for generations of researchers to follow.
One of our most memorable fossil field trips was to the Cretaceous exposures of Lina Island, part of the Haida Formation. We considered it one of our “trips of a lifetime.”
With great sandstone beach exposures and fossil-rich outcrops dating from the Albian to Cenomanian, Lina Island offered both scientific riches and stunning natural beauty.
Our expedition was supported and organized by John Fam, Vice Chair of the Vancouver Paleontological Society, and Dan Bowen, Chair of the British Columbia Paleontological Alliance and the Vancouver Island Palaeontological Society.
Their dedication to fostering collaborative research and building relationships with local Haida communities was key. We were warmly welcomed, and field trips to fossil sites were arranged in partnership with community members and cultural stewards.
The Haida Formation yielded beautifully preserved specimens embedded both in bedding planes and in concretions—hard, rounded nodules that often house exceptionally preserved fossils. Among our finds were:
These fossils offered a rare glimpse into an ancient marine ecosystem that once teemed with life. Douvilleiceras, a spiny ammonite, is particularly striking. This genus, first identified by Whiteaves from Haida Gwaii, ranges from the Middle to Late Cretaceous and has been found across Asia, Africa, Europe, and the Americas. The Haida specimens, from the early to mid-Albian, remain among the most beautiful. It is one of my favourite ammonites of all time and I was blessed to find several good examples of that species.
All of the fossils I collected from Haida Gwaii have been skillfully prepped and donated to the Haida Gwaii Museum in Skidegate, British Columbia. It is a privilege to contribute in a small way to the scientific and cultural understanding of these extraordinary islands.
References and Further Reading:
Whiteaves, J.F. (1876). On the Fossils of the Cretaceous Rocks of British Columbia. Geological Survey of Canada, Report of Progress.
Jeletzky, J.A. (1970). Paleontology of the Cretaceous rocks of Haida Gwaii. Geological Survey of Canada, Bulletin 175.
Haggart, J.W. (1991). New Albian (Early Cretaceous) ammonites from Haida Gwaii. Canadian Journal of Earth Sciences, 28(1), 45–56.
Haggart, J.W. & Smith, P.L. (1993). Paleontology and stratigraphy of the Cretaceous Queen Charlotte Group. Geological Survey of Canada Paper 93-1A.
Carter, E.S., Haggart, J.W., & Mustard, P.S. (1988). Early Cretaceous radiolarians from Haida Gwaii and implications for tectonic setting. Micropaleontology, 34(1), 1–14.
![]() |
Douvelliceras spiniferum, Cretaceous Haida Formation |
![]() |
Fossil Sponge, Polypothecia quadriloba, Warminster, Wiltshire |
![]() |
Echinoids and Bivalves. Collection of Etheldred Benett (1775-1845) |
![]() |
Ichthyosaurus communis |
![]() |
Roy Chapman Andrews, AMNH 1928 Expedition to the Gobi Desert |
![]() | ||
Ichthyosaurus somersetensis Credit: Dean R Lomax |
It was the colour of this amazing trilobite that captured the eye of David Appleton in whose collection it now resides. He is an avid collector and coming into his own as a macro photographer. I have shared three of his delightful photos for you here.
It initially thought that the gold we see here was added during prep, particularly considering the colouration of the matrix, but macro views of the surface show mineralization and the veins running right through the specimen into the matrix. There is certainly some repairs but that is common in the restoration of these specimens. Many of the trilobites I have seen from Morocco have bronze on black colouring but not usually this pronounced. Even so, there is a tremendous amount of fine anatomy to explore and enjoy in this wonderfully preserved specimen.
Paralejurus is a genus of trilobite in the phylum Arthropoda from the Late Silurian to the Middle Devonian of Africa and Europe. These lovelies grew to be up to nine centimetres, though the fellow you see here is a wee bit over half that size at 5.3 cm.
Paralejurus specimens are very pleasing to the eye with their long, oval outline and arched exoskeletons.
Their cephalon or head is a domed half circle with a smooth surface. The large facet eyes have very pleasing crescent-shaped lids. You can see this rather well in the first of the photos here. The detail is quite remarkable.
As you move down from his head towards the body, there is an almost inconspicuous occipital bone behind the glabella in the transition to his burnt bronze thorax.
The body or thorax has ten narrow segments with a clearly arched and broad axial lobe or rhachis. The pygidium is broad, smooth and strongly fused in contrast to the genus Scutellum in the family Styginidae, which has a pygidium with very attractive distinct furrows that I liken to the look of icing ridges on something sweet — though that may just be me and my sweet tooth talking. In Paralejurus, they look distinctly fused — or able to fuse — to add posterior protection against predators with both the look and function of Roman armour.
In Paralejurus, the axillary lobe is rounded off and arched upwards. It is here that twelve to fourteen fine furrows extend radially to complete the poetry of his body design.
Trilobites were amongst the earliest fossils with hard skeletons and they come in many beautiful forms. While they are extinct today, they were the dominant life form at the beginning of the Cambrian.As a whole, they were amongst some of the most successful of all early animals — thriving and diversifying in our ancient oceans for almost 300 million years. The last of their brethren disappeared at the end of the Permian — 252 million years ago. Now, we enjoy their beauty and the scientific mysteries they reveal about our Earth's ancient history.
Photos and collection of the deeply awesome David Appleton. Specimen: 5.3 cm.
![]() |
Unescoceratops koppelhusae, Julius Csotonyi |
The Royal Tyrrell Museum of Palaeontology, named in honour of Joseph Burr Tyrrell, is a palaeontology museum and research facility in Drumheller, Alberta, Canada.
This jaw is the holotype specimen of this small leptoceratopsid dinosaur. Only a handful of isolated fossils have been found from this species, including a jaw that is the holotype specimen now in collections at the Royal Tyrell.
The Royal Tyrrell Museum of Palaeontology, named in honour of Joseph Burr Tyrrell, is a palaeontology museum and research facility in Drumheller, Alberta, Canada.
![]() |
Unescoceratops koppelhusae, RTMP Collections |
The Cleveland Museum of Natural History's Michael Ryan and David Evans of the Royal Ontario Museum in Toronto recently determined that the specimen was a new genus and species.
Unescoceratops is a genus of leptoceratopsid ceratopsian dinosaurs known from the Late Cretaceous (about 76.5-75 million years ago) of Alberta, Canada. Unescoceratops is thought to have been between one and two meters long and less than 91 kilograms. A plant-eater, its teeth were the roundest of all Leptocertopsids.
![]() |
Dinosaur Provincial Park, Alberta, Canada |
In addition to its particularly beautiful scenery, Dinosaur Provincial Park – located at the heart of the province of Alberta's badlands – is unmatched in terms of the number and variety of high-quality specimens.
To date, they represent more than 44 species, 34 genera and 10 families of dinosaurs, dating back 75-77 million years. This provides us with remarkable insight into life millions of years ago.
The park contains exceptional riparian habitat features as well as badlands of outstanding aesthetic value.
The creamy honey, beige and rust coloured hills around the fossil locality are outstanding examples of major geological processes and fluvial erosion patterns in semi-arid steppes — think glorious!The genus is named to honour the UNESCO World Heritage Site designation for the locality where the specimen was found and from the Greek “ceratops,” which means 'horned face'.
Dr Michael Ryan explained that he meant to honour UNESCO's efforts to increase understanding of natural history sites around the world.
© Julius T. Csotonyi An illustration of Unescoceratops koppelhusae, a plant-eating dinosaur from the Late Cretaceous period that lived approximately 75 million years ago shared with his gracious permission.
ABOUT THE ARTIST
Dr. Julius Csotonyi is a Vancouver-based scientific illustrator and natural history fine artist. He is a featured paleoartist on Season One and Season Two of BC's Fossil Bounty. Julius has a scientific background in ecology (MSc) and microbiology (PhD) which has taken him to study sensitive ecosystems, from sand dunes in the Rocky Mountain parks to hydrothermal vents at the bottom of the Pacific Ocean.
These experiences have fuelled his strong resolve to work toward preserving our Earth’s biota. Painting biological subjects is one means that he uses to both enhance public awareness of biological diversity and to motivate concern for its welfare.
He paints murals and panels that have appeared in numerous museums including the Smithsonian’s National Museum of Natural History, press release images for scientific publications, books, stamp sets — including the outstanding 2018 “Sharks of Canada” set for Canada Post — and coins for the Royal Canadian Mint. To view more of Julius Csotonyi's exquisite work visit: https://csotonyi.com/
![]() |
Puffbird similar to Fossil Birds found at Driftwood Canyon |
Metasequoia, the Dawn Redwood |
![]() |
A Tapir showing off his prehensile nose trunk |
This matrix you see here is the Gault Clay, known locally as the Blue Slipper. This fine muddy clay was deposited 105-110 million years ago during the Lower Cretaceous (Upper and Middle Albian) in a calm, fairly deep-water continental shelf that covered what is now southern England and northern France.
Lack of brackish or freshwater fossils indicates that the gault was laid down in open marine environments away from estuaries. The maximum depth of the Gault is estimated 40-60m a figure which has been reached by the presence of Borings made by specialist Algal-grazing gastropods and supported by a study made by Khan in 1950 using Foraminifera. Estimates of the surface water temperatures in the Gault are between 20-22°c and 17-19°c on the seafloor. These estimates have been reached by bulk analysis of sediments which probably register the sea surface temperature for calcareous nanofossils.
It is responsible for many of the major landslides around Ventnor and Blackgang the Gault is famous for its diverse fossils, mainly from mainland sites such as Folkestone in Kent.
Folkestone, Kent is the type locality for the Gault clay yielding an abundance of ammonites, the same cannot be said for the Isle of Wight Gault, however, the south-east coast of the island has proved to be fossiliferous in a variety of ammonites, in particular, the Genus Hoplites, Paranahoplites and Beudanticeras.
While the Gault is less fossiliferous here on the island it can still produce lovely marine fossils, mainly ammonites and fish remains from these muddy mid-Cretaceous seas. The Gault clay marine fossils include the ammonites (such as Hoplites, Hamites, Euhoplites, Anahoplites, and Dimorphoplites), belemnites (such as Neohibolites), bivalves (notably Birostrina and Pectinucula), gastropods (including the lovely Anchura), solitary corals, fish remains (including shark teeth), scattered crinoid remains, and crustaceans (look for the crab Notopocorystes).
Occasional fragments of fossil wood may also be found. The lovely ammonite you see here is from the Gault Clays of Folkstone. Not all who name her would split the genus Euhoplites. There’s a reasonable argument for viewing this beauty as a very thick form of E. loricatus with Proeuhoplites being a synonym of Euhoplites.
Jack Wonfor shared a wealth of information on the Gault and has many lovely examples of the ammonites found here in his collections. If you wish to know more about the Gault clay a publication by the Palaeontological Association called 'Fossils of the Gault clay' by Andrew S. Gale is available in Dinosaur Isle's gift shop.
There is a very good website maintained by Fred Clouter you can look at for reference. It also contains many handy links to some of the best fossil books on the Gault Clay and Folkstone Fossil Beds. Check it out here: http://www.gaultammonite.co.uk/
Euhoplites is an extinct ammonoid cephalopod from the Lower Cretaceous, characterized by strongly ribbed, more or less evolute, compressed to inflated shells with flat or concave ribs, typically with a deep narrow groove running down the middle.
In some, ribs seem to zigzag between umbilical tubercles and parallel ventrolateral clavi. In others, the ribs are flexious and curve forward from the umbilical shoulder and lap onto either side of the venter.
Its shell is covered in the lovely lumps and bumps we associate with the genus. The function of these adornments are unknown. I wonder if they gave them greater strength to go deeper into the ocean to hunt for food.
They look to have been a source of hydrodynamic drag, likely preventing Euhoplites from swimming at speed. Studying them may give some insight into the lifestyle of this ancient marine predator. Euhoplites had shells ranging in size up to a 5-6cm.
We find them in Lower Cretaceous, middle to upper Albian age strata. Euhoplites has been found in Middle and Upper Albian beds in France where it is associated respectively with Hoplites and Anahoplites, and Pleurohoplites, Puzosia, and Desmoceras; in the Middle Albian of Brazil with Anahoplites and Turrilites; and in the Cenomanian of Texas.
This species is the most common ammonite from the Folkstone Fossil Beds in southeastern England where a variety of species are found, including this 37mm beauty from the collections of José Juárez Ruiz.