Friday, 18 July 2025

SPIRALING BEAUTY: AMMONITES AS INDEX FOSSILS

Argonauticeras besairei, Collection of José Juárez Ruiz.
An exceptional example of fractal building of an ammonite septum, in this clytoceratid Argonauticeras besairei from the awesome José Juárez Ruiz.

Ammonites were predatory, squid-like creatures that lived inside coil-shaped shells.

Like other cephalopods, ammonites had sharp, beak-like jaws inside a ring of squid-like tentacles that extended from their shells. They used these tentacles to snare prey, — plankton, vegetation, fish and crustaceans — similar to the way a squid or octopus hunt today.

Catching a fish with your hands is no easy feat, as I'm sure you know. But the Ammonites were skilled and successful hunters. They caught their prey while swimming and floating in the water column. Within their shells, they had a number of chambers, called septa, filled with gas or fluid that were interconnected by a wee air tube. By pushing air in or out, they were able to control their buoyancy in the water column.

They lived in the last chamber of their shells, continuously building new shell material as they grew. As each new chamber was added, the squid-like body of the ammonite would move down to occupy the final outside chamber.

They were a group of extinct marine mollusc animals in the subclass Ammonoidea of the class Cephalopoda. These molluscs, commonly referred to as ammonites, are more closely related to living coleoids — octopuses, squid, and cuttlefish) than they are to shelled nautiloids such as the living Nautilus species.

The Ammonoidea can be divided into six orders:
  • Agoniatitida, Lower Devonian - Middle Devonian
  • Clymeniida, Upper Devonian
  • Goniatitida, Middle Devonian - Upper Permian
  • Prolecanitida, Upper Devonian - Upper Triassic
  • Ceratitida, Upper Permian - Upper Triassic
  • Ammonitida, Lower Jurassic - Upper Cretaceous
Ammonites have intricate and complex patterns on their shells called sutures. The suture patterns differ across species and tell us what time period the ammonite is from. If they are geometric with numerous undivided lobes and saddles and eight lobes around the conch, we refer to their pattern as goniatitic, a characteristic of Paleozoic ammonites.

If they are ceratitic with lobes that have subdivided tips; giving them a saw-toothed appearance and rounded undivided saddles, they are likely Triassic. For some lovely Triassic ammonites, take a look at the specimens that come out of Hallstatt, Austria and from the outcrops in the Humboldt Mountains of Nevada.

Hoplites bennettiana (Sowby, 1826).
If they have lobes and saddles that are fluted, with rounded subdivisions instead of saw-toothed, they are likely Jurassic or Cretaceous. If you'd like to see a particularly beautiful Lower Jurassic ammonite, take a peek at Apodoceras. Wonderful ridging in that species.

One of my favourite Cretaceous ammonites is the ammonite, Hoplites bennettiana (Sowby, 1826). This beauty is from Albian deposits near Carrière de Courcelles, Villemoyenne, near la région de Troyes (Aube) Champagne in northeastern France.

At the time that this fellow was swimming in our oceans, ankylosaurs were strolling about Mongolia and stomping through the foliage in Utah, Kansas and Texas. Bony fish were swimming over what would become the strata making up Canada, the Czech Republic and Australia. Cartilaginous fish were prowling the western interior seaway of North America and a strange extinct herbivorous mammal, Eobaatar, was snuffling through Mongolia, Spain and England.

In some classifications, these are left as suborders, included in only three orders: Goniatitida, Ceratitida, and Ammonitida. Once you get to know them, ammonites in their various shapes and suturing patterns make it much easier to date an ammonite and the rock formation where is was found at a glance.

Ammonites first appeared about 240 million years ago, though they descended from straight-shelled cephalopods called bacrites that date back to the Devonian, about 415 million years ago, and the last species vanished in the Cretaceous–Paleogene extinction event.

They were prolific breeders that evolved rapidly. If you could cast a fishing line into our ancient seas, it is likely that you would hook an ammonite, not a fish. They were prolific back in the day, living (and sometimes dying) in schools in oceans around the globe. We find ammonite fossils (and plenty of them) in sedimentary rock from all over the world.

In some cases, we find rock beds where we can see evidence of a new species that evolved, lived and died out in such a short time span that we can walk through time, following the course of evolution using ammonites as a window into the past.

For this reason, they make excellent index fossils. An index fossil is a species that allows us to link a particular rock formation, layered in time with a particular species or genus found there. Generally, deeper is older, so we use the sedimentary layers rock to match up to specific geologic time periods, rather the way we use tree-rings to date trees. A handy way to compare fossils and date strata across the globe.

References: Inoue, S., Kondo, S. Suture pattern formation in ammonites and the unknown rear mantle structure. Sci Rep 6, 33689 (2016). https://doi.org/10.1038/srep33689
https://www.nature.com/articles/srep33689?fbclid=IwAR1BhBrDqhv8LDjqF60EXdfLR7wPE4zDivwGORTUEgCd2GghD5W7KOfg6Co#citeas

Photo: Hoplites Bennettiana from near Troyes, France. Collection de Christophe Marot

Wednesday, 16 July 2025

VICTORIA ARBOUR: ARMOURED GIANTS, ANCIENT ECOSYSTEMS AND CUTTING EDGE CANADIAN PALEONTOLOGY

Dr. Victoria Arbour
Dr. Victoria Arbour, Curator of Paleontology at the Royal BC Museum in Victoria, British Columbia, is one of Canada’s foremost vertebrate paleontologists. 

Specializing in ankylosaurs—the club-tailed, heavily armored dinosaurs of the Cretaceous—Arbour has become a leading voice in both the scientific community and the public eye, reshaping how we understand dinosaur evolution, biomechanics, and paleobiogeography. 

Her research bridges detailed anatomical study with innovative technologies, yielding groundbreaking discoveries about how these ancient creatures lived, fought, and evolved. Charmingly humble and unassuming, she is a delight in the field and in front of the lens.

Victoria Arbour completed her Ph.D. at the University of Alberta under the supervision of renowned paleontologist Dr. Philip Currie. Her early work focused on ankylosaurid dinosaurs, particularly the tail club structures that define the group. 

Her doctoral thesis and subsequent studies dissected the biomechanics of ankylosaur tail clubs, demonstrating that these dinosaurs likely used their tails as active weapons—a concept that was previously more speculative than evidenced.

In one of her early papers, Arbour and Currie (2011) reconstructed the tail club’s structure and function using finite element analysis and compared it to weapon systems in modern animals. Her work helped establish ankylosaurs as more than passive tanks; they were dynamic animals capable of delivering powerful, bone-breaking blows to rivals or predators.

New Dinosaurs for a New Generation

Among Arbour’s most significant contributions are the descriptions and naming of several new species of ankylosaurs, including:

Zuul crurivastator (2017): Arbour co-authored the paper describing Zuul, a remarkably complete ankylosaur fossil from Montana. Named after the Ghostbusters monster, Zuul is preserved with intact skin impressions and tail club spikes. The species name, crurivastator, means "destroyer of shins"—a nod to its powerful tail weapon. The find gave paleontologists unprecedented insight into ankylosaur soft tissue, armor arrangement, and injury patterns.

Borealopelta markmitchelli (2017): Although discovered by others, Arbour contributed to the public communication and interpretation of this exceptionally preserved nodosaurid from Alberta’s oil sands. The fossil includes preserved skin and stomach contents, which have helped reconstruct its camouflage strategy and diet.

Ziapelta sanjuanensis (2014): As lead author, Arbour described this ankylosaur from New Mexico, expanding the known diversity of North American ankylosaurs and underscoring biogeographic connections between Canada and the southwestern United States during the Late Cretaceous.

British Columbia’s Dinosaur Heritage

As Curator at the Royal BC Museum, Arbour plays a critical role in paleontology in British Columbia—a province better known for marine reptiles than for terrestrial dinosaurs. Nevertheless, her work has amplified interest in BC’s unique fossil heritage, from the ichthyosaurs of the Peace Region to marine reptiles like the Courtenay Elasmosaur.

Arbour plays a pivotal role in the ongoing research and interpretation of the Courtenay elasmosaur, Elasmosaurus sp., a 13-metre-long marine reptile discovered on Vancouver Island. 

Building upon earlier studies, Arbour has applied modern scientific techniques to examine the specimen’s anatomy and paleoecological context. Her work includes detailed analyses of the skull, vertebrae, and limb bones, contributing to a better understanding of the evolutionary relationships and biomechanics of elasmosaurs. 

Through comparative research with other North American and global plesiosaur finds, Arbour has helped clarify the taxonomic placement of the Courtenay specimen and its role in the broader picture of Cretaceous marine ecosystems.

Arbour has partnered with local scientists and citizen paleontologists to help elevate BC’s presence on the paleontological map. She has advocated for fossil protection legislation and regularly engages with the public through museum exhibits, interviews, and school outreach.

Technology Meets Deep Time

Arbour is also part of a wave of paleontologists bringing high-tech tools to ancient bones. She frequently uses 3D scanning, photogrammetry, and CT imaging to study fossils in unprecedented detail. These methods allow her to reconstruct the internal anatomy of ankylosaurs, visualize muscle attachment points, and model how these creatures moved and fought.

In her 2020 publication with Mallon and Evans, Arbour examined the distribution of ankylosaur fossils across North America and evaluated their evolutionary history. 

Using phylogenetic methods and morphometric analyses, she tracked how isolation and habitat shifts influenced ankylosaur evolution—helping explain why Canada’s ankylosaurs were different from those in the southern U.S.

Champion of Public Science

Beyond her research, Arbour is a passionate advocate for science communication and equity in paleontology. Her Twitter feed, popular talks, and media appearances make complex science accessible and fun. She has written popular articles for The Conversation, participated in CBC’s Quirks & Quarks, and is a familiar face in science outreach events across Canada.

She is a very engaging speaker. For those who joined us for Arbour's engaging talk to the Vancouver Paleontological Society and members of the British Columbia Paleontological Alliance on her fieldwork at the Carbon Creek Basin Dinosaur Trackway—and so many others—will be pleased to hear that she will be delivering a talk on her most recent work at this 15th BCPA Symposium in Courtenay, August 22-25, 2025. 

The Carbon Creek Basin site is located just west of Hudson’s Hope in the Peace River area and boasts nearly 1,200 dinosaur tracks from at least 12 different types of dinosaurs—including two dinosaur track types that have not been observed at any other site in the Peace Region. Her talk showcased her work and her spirit in the field—coated in mud, dust and battling blackflies, but smiling through it all in the thrill of discovery.

Her mentorship of young scientists and support for women and underrepresented groups in science has made her a role model in the field. She also contributed to the popular Dinosaurs of Alberta field guide and helped curate exhibits that bring museum visitors face-to-face with ancient life.

Dr. Victoria Arbour’s work continues to deepen our understanding of how dinosaurs lived and interacted in their environments. Her contributions are a testament to the power of curiosity, perseverance, and scientific rigor. In the layered rocks of Alberta and the museum halls of Victoria, her legacy is already well-anchored—and growing with every new discovery.

Here are some key scientific papers authored or co-authored by Dr. Victoria Arbour:

Arbour, V. M., & Currie, P. J. (2011). Ankylosaurid dinosaur tail clubs evolved through stepwise acquisition of key features. Journal of Anatomy, 219(6), 672–685. https://doi.org/10.1111/j.1469-7580.2011.01437.x

Arbour, V. M., Zanno, L. E., & Evans, D. C. (2014). A new ankylosaurid dinosaur from the Judith River Formation of Montana, USA, based on a complete skull and tail club. Royal Society Open Science, 4(5): 161086. https://doi.org/10.1098/rsos.161086

Arbour, V. M., & Evans, D. C. (2017). A new ankylosaurine dinosaur from the Judith River Formation of Montana, USA, based on a complete skull and tail club. Royal Society Open Science, 4: 161086. https://doi.org/10.1098/rsos.161086

Brown, C. M., Henderson, D. M., Vinther, J., Fletcher, I., Sistiaga, A., Herrera, J., & Arbour, V. M. (2017). An exceptionally preserved armored dinosaur reveals the morphology and allometry of keratinous structures. Current Biology, 27(16), 2514–2521.e3. https://doi.org/10.1016/j.cub.2017.06.071

Arbour, V. M., & Evans, D. C. (2020). A new ankylosaurine dinosaur from the Judith River Formation, Montana, USA, and implications for the diversification and biogeography of Late Cretaceous ankylosaurs. PeerJ, 8:e9603. https://doi.org/10.7717/peerj.9603

Arbour, V. M., & Currie, P. J. (2013). Anatomy, evolution, and function of tail clubbing in ankylosaurs (Dinosauria: Ornithischia). Journal of Zoology, 292(2), 111–117. https://doi.org/10.1111/jzo.12033




Tuesday, 15 July 2025

15TH BCPA PALEONTOLOGICAL SYMPOSIUM: COURTENAY, BRITISH COLUMBIA

SAVE THE DATE: 15th British Columbia Paleontological Symposium

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.

Saturday, 12 July 2025

ALBERTA'S PREHISTORIC GIANTS: THE DINOSAURS

Alberta's Badlands and Dinosaur Hunting Grounds
Alberta, Canada, is one of the most dinosaur-rich places on Earth. 

Its fossil beds are a window into the Mesozoic, showcasing a dazzling array of ancient life from the Late Cretaceous. 

From the thunderous footsteps of Tyrannosaurus rex to the intricate frills of Styracosaurus, Alberta’s badlands are a treasure trove of discovery that has fascinated paleontologists for over a century.

The story of Alberta's dinosaurs begins in the late 19th century. In 1884, geologist Joseph Burr Tyrrell stumbled upon the skull of a carnivorous dinosaur while surveying coal seams near Red Deer River. 

This skull belonged to Albertosaurus sarcophagus, a relative of T. rex—and marked the first significant dinosaur discovery in what is now Dinosaur Provincial Park.

By the early 20th century, Alberta had caught the attention of fossil hunters worldwide. Between 1910 and 1917, the American Museum of Natural History sent Charles H. Sternberg and his sons to excavate Alberta’s badlands. 

Charles Hazelius Sternberg was a legendary fossil hunter and one of the most important figures in Alberta’s early paleontological history. Born in 1850 in Kansas, Sternberg began collecting fossils in the American West before being hired by the American Museum of Natural History to excavate in Canada. 

From 1910 to 1917, he and his three sons worked extensively in Alberta’s badlands, unearthing thousands of dinosaur fossils from the Belly River Group and other Cretaceous formations. He was a paleo legend and, by all accounts, the world's best dad!

Their discoveries included spectacular specimens of ceratopsians like Centrosaurus and hadrosaurs like Corythosaurus. Sternberg’s work helped establish Alberta as a global hotspot for dinosaur research, and his passion for fossils is reflected in his memoir, The Life of a Fossil Hunter (1909), which remains a classic of paleontological literature.

Their expeditions yielded thousands of fossil specimens, including ceratopsians like Centrosaurus and Chasmosaurus, and duck-billed hadrosaurs such as Lambeosaurus and Corythosaurus.

Designated a UNESCO World Heritage Site, Dinosaur Provincial Park is one of the most productive fossil sites in the world. Over 50 species of dinosaurs have been found here, dating from around 76 to 74 million years ago during the Campanian stage of the Late Cretaceous.

The park preserves part of the ancient floodplain of the Western Interior Seaway, a vast inland sea that once split North America in two. The mix of river channels, swamps, and coastal habitats created ideal conditions for fossil preservation.

Famous finds from the park include:

  • Gorgosaurus libratus – A fearsome tyrannosaurid predator
  • Parasaurolophus walkeri – Known for its stunning cranial crest
  • Styracosaurus albertensis – A ceratopsian with magnificent spiked frills

Alberta continues to yield spectacular discoveries. In 2020, a new species of meat-eating dinosaur was unveiled: Thanatotheristes degrootorum, nicknamed the “Reaper of Death.” Discovered by John De Groot along the Bow River, this tyrannosaur roamed Alberta about 79 million years ago—making it the oldest known tyrannosaurid from Canada.

Another remarkable find came in 2011 near Fort McMurray: the best-preserved armored dinosaur ever found, Borealopelta markmitchelli. This nodosaur, discovered by workers in the Suncor Millennium Mine, was so well preserved that its skin, scales, and even possible pigmentation patterns remain visible. The fossil is now housed at the Royal Tyrrell Museum in Drumheller and has revolutionized our understanding of dinosaur defense and coloration.

In 2022, a new species of dome-headed pachycephalosaur, Acrotholus audeti, was described from southern Alberta. It revealed that these head-butting herbivores were more diverse and common than previously thought.

If you're captivated by Alberta's prehistoric past, you’re in luck—there are several world-class institutions where you can see these giants up close:

Royal Tyrrell Museum of Palaeontology (Drumheller)

  • Home to over 160,000 fossil specimens, the museum showcases Alberta’s dinosaur heritage with life-sized displays, fossil labs, and immersive exhibits.

Philip J. Currie Dinosaur Museum (Wembley)

  • Named after the renowned Canadian paleontologist Philip Currie, this museum focuses on the Grande Prairie region’s dinosaur discoveries, including those from the Wapiti Formation.

University of Alberta Paleontology Museum (Edmonton)

  • Located on campus, this museum features a wide array of fossil vertebrates and invertebrates, and often highlights ongoing research from U of A scientists.

Dinosaur Provincial Park Visitor Centre

  • Located within the fossil-rich badlands, this center offers interpretive displays and guided hikes to real fossil beds.

Many of Alberta’s groundbreaking discoveries are thanks to Canadian researchers like:

  • Philip J. Currie, whose work on tyrannosaurs, especially Albertosaurus, has reshaped our understanding of predator behavior.
  • Darla Zelenitsky, whose research on dinosaur reproduction, eggs, and nesting behavior continues to uncover intimate details of prehistoric life.
  • François Therrien, a curator at the Royal Tyrrell Museum specializing in carnivorous dinosaur paleoecology.

Alberta's unique geological history, its rich fossiliferous formations—like the Dinosaur Park, Horseshoe Canyon, and Wapiti formations—and a legacy of active fieldwork and public engagement have made it a global hotspot for dinosaur discovery. Whether you're walking the trails of Dinosaur Provincial Park or marveling at life-sized skeletons in the Royal Tyrrell Museum, Alberta offers a front-row seat to the age of dinosaurs.

Fancy a read? Check out these Scientific Papers on some of the research being done:

Currie, P. J. (2003). Allosaurus, Saurophaganax, and other large theropods of the Morrison Formation. In The Carnivorous Dinosaurs. Indiana University Press.

Zelenitsky, D. K., & Therrien, F. (2008). “Oviraptorosaur dinosaurs from Alberta, Canada: Nesting behavior and diversity.” Journal of Vertebrate Paleontology, 28(3), 636-651.

Brown, C. M., Henderson, D. M., Vinther, J., Fletcher, I., Sistiaga, A., Herrera, J., & Summons, R. E. (2017). “An exceptionally preserved three-dimensional armored dinosaur reveals insights into coloration and biology.” Current Biology, 27(16), 2514–2521.e3.

Voris, J. T., Zelenitsky, D. K., Therrien, F., & Brown, C. M. (2020). “A new tyrannosaurine (Theropoda: Tyrannosauridae) from the Campanian Foremost Formation of Alberta, Canada.” Cretaceous Research, 110, 104388.

Evans, D. C., Ryan, M. J., & Anderson, J. S. (2013). “A new basal pachycephalosaurid (Dinosauria: Ornithischia) from the Oldman Formation, Alberta, Canada.” Nature Communications, 4, 1828.

Thursday, 10 July 2025

MIGHTY EAGLE: KWIKW (KW-EE-KW)

Bald Eagle / Haliaeetus leucocephalus  @Paul McClure
A mighty Bald Eagle sitting with wings spread gazing intensely at his next potential snack.

Their wings are built for graceful soaring and gliding on updrafts of warm air called thermals. 

Their long feathers are slotted, easily separating so air flows smoothly and giving them the added benefit of soaring at slower speeds. 

As well as his wings, this fellow is also drying off his white head feathers. A bald eagle's white head can make it look bald from a distance but that is not where the name comes from. It is from the old English word balde, meaning white.

In the Kwak'wala language of the Kwakwaka'wakw, speakers of Kwak'wala — an eagle is known as kwikw (kw-ee-kw) and an eagle's nest is called a kwigwat̕si

Should you encounter an eagle and wish to greet them in Kwak'wala, you would just say yo. Yup, just yo. They would like your yo hello better if you offered them some fresh fish. They dine on all sorts of small mammals, fish and birds but are especially fond of pink salmon or ha̱nu'n (han-oon).

These living dinosaurs are a true homage to their lineage. They soar our skies with effortless grace. Agile, violent and beautiful, these highly specialized predators can catch falling prey mid-flight and dive-bomb into rivers to snag delicious salmon. 

Their beauty and agility are millions of years in the making. From their skeletal structure to their blood cells, today’s birds share a surprising evolutionary foundation with reptiles. 

Between 144 million and 66 million years ago, during the Mesozoic era, we see the first birds evolve. Eventually, tens of millions of years ago, an ancient group of birds called kites developed. Like today’s bald eagle, early kites are thought to have scavenged and hunted fish.

About 36 million years ago, the first eagles descended from kites, their smaller cousins. First to appear were the early sea eagles, which — like kites — continued to prey on fish and whose feet were free of feathers, along with booted eagles, which had feathers below the knee. Fossils of Bald Eagles are very rare and date to the late Pleistocene. Eagles are known from the early Pleistocene of Florida, but they are extinct species not closely related to the bald eagle.

Like the kites, bald eagles have featherless feet, but they also developed a range of other impressive adaptations that help them hunt fish and fowl in a watery environment. Each foot has four powerful toes with sharp talons. Tiny projections on the bottom of their feet called “spicules” help bald eagles grasp their prey. A bald eagle also has serrations on the roof of its mouth that help it hold slippery fish, and incredibly, the black pigment in its wing feathers strengthens them against breakage when they dive head first into water.

Obviously, there is much more than their striking white heads that sets these iconic raptors apart from the crowd. Their incredible physiology, built for life near the water, is literally millions of years in the making. 

The eagle in the photo you see here is a resident of Vancouver Island captured beautifully by photographer Paul McClure. Gilakas'la mula! 

Wednesday, 9 July 2025

TOP 10 FAMOUS CANADIAN FOSSIL FINDS

Canada, with its vast and varied landscapes, is a treasure trove of prehistoric wonders. 

From towering tyrannosaurs to exquisitely preserved marine creatures, the fossil record here is not only rich—it’s legendary. 

It is hard to choose our best fossils as there are so many. I have my personal favorites, some found by me, some by good friends and others that rank high simply by my having the good fortune to be there at the moment of discovery. 

These ten fossils stand out not only for their scientific value but also for the astonishing stories they tell about life on ancient Earth. Whether entombed in the Rocky Mountains, buried beneath Arctic permafrost, or hidden in coastal cliffs, each discovery shines a light on a world lost to time.

Honorable mentions are many for a list of this type. Dave Rudkin's find of the Isotelus rex, the largest known trilobite definitely ranks. There are some very fetching crabs and ammonites who deserve mention. As does the First Record of an Oligocene Chimaeroid Fish (Ratfish) Egg Capsule from Vancouver Island . 

The isopod found by the deeply awesome Betty Franklin that is getting ready for publication by Torrey Nyborg is another superb example and makes my personal list. He also has an unexpected fossil lobster in the cue to write up that I found in the South Chilcotin many moons ago, so I will add that here to remind him! 

On that note, Dr. Dave Evans has a paper in the works on the first dinosaur from Vancouver Island found by our own Mike Trask that will hopefully be out soon. There is a new paper by Phil Currie et al. on the fossil fauna from the Eager Formation near Cranbrook that bears mentioning as well as the work being done by Chris Jenkins, Chris New with Brian Chatterton on the Upper Cambrian fauna near there. We can add all the finds from Tumbler Ridge, Wapiti Lake and Miguasha National Park as well.

Oh, so many options!     

So, this is by no means a complete list, but if you are wanting to check out the fossil bounty that Canada has to offer, it is a wonderful place to start!

1. Scotty the T. rex (Saskatchewan)

Discovered in 1991 near Eastend, Saskatchewan, Scotty is the largest and most complete Tyrannosaurus rex ever found in Canada—and one of the oldest individuals known of its species. Weighing an estimated 8,800 kg and measuring over 13 meters, Scotty was a bruiser of a predator. The fossil is housed at the Royal Saskatchewan Museum.

Reference: Funston, G. F., Currie, P. J., & Persons, W. S. IV. (2019). An older and exceptional specimen of Tyrannosaurus rex.

2. The Burgess Shale Fauna (British Columbia)

This World Heritage Site near Field, BC, offers a snapshot of the Cambrian Explosion (~508 million years ago), preserving soft-bodied creatures with extraordinary detail. Marrella, Opabinia, and Anomalocaris are just a few of the iconic oddballs discovered here by Charles Walcott in 1909. The site reshaped our understanding of early animal evolution. The fossils from this site have the most wonderous, albeit wacky, body plans see the world over!

Reference: Conway Morris, S. (1986). The community structure of the Middle Cambrian phyllopod bed (Burgess Shale). Paleontology, 29(3).

3. The Courtenay Elasmosaur (British Columbia)

Unearthed by my good friend Mike Trask along the Puntledge River in 1988, this long-necked marine reptile from the Late Cretaceous is one of BC’s most famous fossils—and its first major marine reptile discovery. Now housed at the Courtenay and District Museum, it inspired a new wave of paleontological exploration on Vancouver Island. 

Mike gets the credit for this find and the founding of the first paleontological society in British Columbia (VIPS), the British Columbia Paleontological Alliance (BCPA) and inspired us all with his incredible curiosity and zest for life. He passed earlier this year and is incredibly missed!

Reference: Arbour, V. M., & Trask, M. (2023). A new elasmosaurid from the Late Cretaceous of British Columbia. Canadian Journal of Earth Sciences.

4. Dakota the Dinosaur Mummy (Alberta)

This extraordinary hadrosaur (Edmontosaurus annectens) found in 1999 features fossilized skin and soft tissue impressions. While partially excavated in North Dakota, it crossed into Canadian paleontological territory through the collaborative work between Canadian and American scientists. The mummy-like preservation gives unique insight into dinosaur musculature and skin texture.

Reference: Manning, P. L., et al. (2009). Mineralized soft-tissue structure and chemistry in a mummified hadrosaur. Proceedings of the Royal Society B.

5. Zuul crurivastator (Alberta)

Discovered in 2014 in Montana but now part of the Royal Ontario Museum collection due to fossil trade agreements, Zuul is an astonishingly complete ankylosaur with preserved skin and tail club armor. Named after the Ghostbusters demon-dog, it’s as fierce as it is beautifully preserved.

Reference: Arbour, V. M., & Evans, D. C. (2017). A new ankylosaurid with exceptional soft-tissue preservation. Royal Society Open Science, 4(5).

6. Tiktaalik roseae (Nunavut)

Found on Ellesmere Island in 2004, Tiktaalik bridges the gap between fish and land vertebrates. With its fish-like body and amphibian-style neck and limbs, it's a critical fossil in understanding the water-to-land transition in vertebrate evolution.

Reference: Daeschler, E. B., Shubin, N. H., & Jenkins, F. A. (2006). A Devonian tetrapod-like fish and the evolution of the tetrapod body plan. Nature, 440.

If you have not had the pleasure, also pick up a copy of Shubin's book, Your Inner Fish. It is a classic read with the amazing tale of this fossil's discovery and Shubin's journey in paleontology. 

7. Nodosaur from the Suncor Mine (Alberta)

In 2011, miners at a Fort McMurray oilsands site uncovered the best-preserved armored dinosaur ever found. The 110-million-year-old nodosaur is so well-preserved it looks like a sleeping dragon, with skin impressions, armor, and even stomach contents intact.

Reference: Brown, C. M., & Demarco, N. (2017). The rise of fossil preservation in Alberta’s oil sands. National Geographic, May Issue.

8. The Joggins Fossil Cliffs (Nova Scotia)

These coastal cliffs reveal the Carboniferous "Coal Age" (circa 310 million years ago) with fossilized trees, trackways, and even the oldest known reptile, Hylonomus lyelli. Declared a UNESCO World Heritage Site, Joggins provides unparalleled insight into early terrestrial ecosystems.

Reference: Carroll, R. L. (1964). The earliest reptiles. Journal of Paleontology, 38(1).

9. Parksosaurus (Alberta)

One of the lesser-known but scientifically significant dinosaurs from Alberta, Parksosaurus was a small, agile herbivore named after Canadian paleontologist William Parks. It contributes to our understanding of small ornithopods in the Late Cretaceous of North America.

Reference: Boyd, C. A. (2015). The systematic relationships and biogeographic history of ornithischian dinosaurs. Paleobiology, 41(3).

10. Blue Beach Fossils (Nova Scotia)

The Blue Beach site near Hantsport yields some of the oldest known tetrapod trackways in the world, from the Late Devonian to Early Carboniferous period. These fossils document early vertebrate life coming onto land.

Reference: Mansky, C. F., & Lucas, S. G. (2013). A review of tetrapod trackways from Blue Beach. New Mexico Museum of Natural History Bulletin, 61.

Canada’s fossil discoveries span more than half a billion years of life on Earth. They showcase evolutionary milestones—from the earliest invertebrates to apex dinosaurs, marine reptiles, and the first vertebrates on land. 

The fossils are the Rosetta stones of our country, unlocking the secrets of life's history.

Saturday, 5 July 2025

FOSSIL HUNTRESS PODCAST: DEAD SEXY SCIENCE

Geeky goodness from the Fossil Huntress. If you love paleontology, you will love this stream. Dinosaurs, trilobites, ammonites—you'll find them all here!

Close your eyes & fly with me as we head out together to explore Earth's rich history written in her rock. Travel to extraordinary places, sacred sites & unearth mysteries millions of years old on the Fossil Huntress Podcast.

This stream is for those who share an enduring passion for our world's hidden treasures, its wild places & want to uncover her beauty stone by stone.

This is the story of the making of our Earth and the many wonderful creatures who have called it home.

Join in the exploration of the fascinating science of paleontology — that lens that examines ancient animals, plants & ecosystems from wee single-celled organisms to big & mighty dinosaurs. Save the stream to your favorites to listen while you drive, head out fossil collecting or snuggle in for the night!

​To listen now, visit: https://open.spotify.com/show/1hH1wpDFFIlYC9ZW5uTYVL

Friday, 4 July 2025

FOSSIL FRESHWATER SALMON FROM KAMLOOPS, BRITISH COLUMBIA

Fossilized Salmon gifted to the Huntress by John Leahy
Nestled in the interior of British Columbia, the region around Kamloops is a dry, sagebrush-studded landscape—and home to some of Canada’s most remarkable fossil fish discoveries. 

It is also home to many rattlesnakes, so if you are up that way, step lively!

Among the most fascinating fossils found here are fossilized salmonids, distant ancestors of the modern Pacific salmon that are iconic to the rivers of British Columbia today.

The fossils of interest date back to the Eocene, approximately 50 million years ago, and are primarily found in the Tranquille Formation, a part of the Kamloops Group. 

This ancient lakebed is located at McAbee Fossil Beds, near Cache Creek just west of Kamloops, and also in the nearby Driftwood Canyon and Princeton fossil beds, which together form part of British Columbia’s Eocene fossil record.

The Tranquille Formation preserves what was once a large, subtropical freshwater lake surrounded by lush forests. 

Volcanic ashfalls and fine silt periodically buried aquatic organisms and plant matter, preserving them in astonishing detail. Among the insects, plants, and other fish fossils, paleontologists have discovered fossil remains of early salmonids, the group of fish that includes modern salmon and trout.

A significant discovery was Eosalmo driftwoodensis, the earliest known fossil representative of the salmon family (Salmonidae). 

First described in 1977 by Canadian ichthyologist Mark Wilson, Eosalmo was recovered from the Driftwood Canyon site in northern BC but its relatives have been found in similar-aged formations across the province, including near Kamloops.

These fossils show that salmonids had already begun to diversify during the early Eocene. Eosalmo displays characteristics linking it to both trout and salmon, suggesting that the divergence between these lineages was already underway. Its morphology includes features like a terminal mouth, forked tail, and well-developed fins, hallmarks of active freshwater swimmers.

What’s particularly interesting about fossil salmonids in British Columbia is that they appear to have lived exclusively in freshwater during the Eocene. 

This contrasts with today’s Pacific salmon, which are famously anadromous—born in freshwater, migrating to the ocean, and returning to spawn. The fossil record suggests this sea-run lifestyle evolved later, possibly as a response to tectonic shifts and changing ocean currents in the Miocene, around 20 million years ago.

The lakes of Eocene BC, including the one preserved at McAbee, would have supported thriving fish populations in a warm, relatively stable climate. Fossil finds include not just salmonids but also bowfins, suckers, and small freshwater herring-like fish, painting a picture of a rich and diverse aquatic ecosystem.

The McAbee Fossil Beds, now designated as a provincial heritage site, continue to yield new specimens. Though public access is currently restricted to protect the integrity of the site, ongoing research continues to uncover new details about the ancient ecosystems of interior BC.

Institutions such as the Royal BC Museum and the University of Alberta have studied and preserved these fossil fish. Scientific papers by Mark Wilson, and others have helped place these finds into a broader evolutionary context, revealing how ancient fish faunas of western North America evolved over tens of millions of years.

The fossil salmon of Kamloops bones, entombed in rock for 50 million years, speak to a time when the interior of British Columbia was lush, warm, and teeming with life. 

As research continues, these fossil salmonids help illuminate the early history of a fish group vital not just to ecosystems, but to cultures and economies across the Pacific Rim.

The beauty you see here is a fossil salmon skull gifted to me by the remarkable John Leahy, who is much missed!

References:

Wilson, M. V. H. (1977). Eosalmo driftwoodensis, a new genus and species of fossil salmonid fish from the Eocene of British Columbia. Canadian Journal of Earth Sciences, 14(5), 1213–1230.

Wilson, M. V. H., & Li, G. Q. (1999). Osteology and phylogenetic relationships of Eosalmo, the earliest known salmonid fish. Canadian Journal of Earth Sciences, 36(10), 1559–1573.

Archibald, S. B., Greenwood, D. R., Smith, R. Y., Mathewes, R. W., & Basinger, J. F. (2011). Great Canadian Lagerstätten 1. Early Eocene Lagerstätten of the Okanagan Highlands (British Columbia and Washington State). Geoscience Canada, 38(4), 155–164.

McAbee Fossil Beds Provincial Heritage Site: https://www2.gov.bc.ca

If you’re ever driving through Kamloops, it’s humbling to think that beneath your feet lie the ancestors of today’s salmon—timeless travellers of BC’s ancient waterways.

Wednesday, 2 July 2025

CRUISIN THE FOSSIL FREEWAY: ALASKAN PALEONTOLOGY

Alaska, often called the "Last Frontier," is not only home to staggering wilderness and modern megafauna like bears and moose—it’s also a treasure trove of prehistoric life. 

From marine reptiles that swam in the Arctic seas to duck-billed dinosaurs that thrived in polar forests, Alaska’s fossil record paints a vivid picture of life at high latitudes during deep time.

Alaska’s geological history is a complex collage of terranes—fragmented pieces of crust that accreted onto the North American plate. This makes the state an exceptionally diverse fossil site, with deposits spanning from the Paleozoic to the Cenozoic. 

Some of the most significant fossil discoveries in Alaska come from:

  • Prince Creek Formation (Late Cretaceous): One of the northernmost dinosaur-bearing formations on Earth, located along Alaska’s North Slope.
  • Liscomb Bonebed: A hotspot for Arctic dinosaurs, discovered in the 1960s and later explored in detail by Kirk Johnson and colleagues.
  • Tuxedni Group (Jurassic): Marine invertebrates, including ammonites and bivalves, are common here.
  • Chickaloon Formation (Paleocene): Known for its beautifully preserved fossil plants, including fossilized redwoods and Metasequoia.

One of the most astonishing aspects of Alaskan fossils is the presence of polar dinosaurs. During the Late Cretaceous, the Arctic Circle was a much warmer place than it is today, but still experienced months of darkness. 

Herbivorous dinosaurs such as Edmontosaurus, Ugrunaaluk kuukpikensis (a newly named hadrosaur species from the North Slope), and Pachyrhinosaurus lived in herds in this high-latitude environment, while predators like Nanuqsaurus hoglundi, a smaller relative of T. rex, prowled the dark forests.

These animals were uniquely adapted to life in extreme conditions. Evidence from bone histology suggests that these dinosaurs had growth cycles influenced by the harsh Arctic climate—some may have hibernated or experienced slowed metabolism during the winter months.

Kirk Johnson’s research, alongside collaborators such as Tony Fiorillo and Roland Gangloff, has been central in understanding how these polar ecosystems worked. Johnson has led expeditions into the Arctic wilderness, collecting fossils and reconstructing ancient environments based on plant fossils, sedimentology, and isotope analysis.

Fossil Plants and Climate Clues

While dinosaurs grab the headlines, the fossilized flora of Alaska is equally important. Johnson is particularly renowned for his work on fossil plants, which he has used to reconstruct past climates and landscapes. In the Chickaloon Formation, for instance, fossilized leaves, cones, and wood fragments tell the story of an ancient rainforest-like environment that thrived just after the age of dinosaurs, during the Paleocene.

A paper of interest he co-authored with Dr. David J. Nichols—a distinguished paleobotanist and palynologist with the U.S. Geological Survey whose research significantly advanced the understanding of fossil pollen, spores, and Cretaceous-Tertiary boundary events. 

Over his career, Nichols became known for his expertise in using fossilized plant micro remains—such as pollen grains and spores—to reconstruct ancient ecosystems and trace climatic and environmental shifts through geologic time. 

His collaboration with Dr. Kirk Johnson on the Prince Creek Formation in northern Alaska combined his palynological skills with Johnson’s macrofossil plant research, providing a comprehensive view of Late Cretaceous polar flora and their ecological significance. 

Nichols’ meticulous work helped illuminate how vegetation patterns responded to ancient climate change and extinction events, making his contributions invaluable to studies of high-latitude paleoecology and Earth system history.

  • Johnson, K. R., & Nichols, D. J. (2008). Plant fossils from the Prince Creek Formation, North Slope, Alaska: Implications for Late Cretaceous polar ecosystems. In: "Studies on Fossils in Arctic Environments." Geological Society of America Special Paper 442, pp. 155–170. DOI:10.1130/2008.442(10)

This paper documents high-latitude Cretaceous flora, revealing that Alaska once supported lush forests, with taxa such as Metasequoia (dawn redwood), ferns, and angiosperms flourishing under a warm polar regime. These fossils help scientists understand long-term climate dynamics and serve as analogs for future warming scenarios.

Marine Reptiles and Cretaceous Oceans

In southern Alaska, Jurassic and Cretaceous marine sediments have yielded remains of ichthyosaurs, plesiosaurs, and large ammonites. These fossils suggest that Alaska’s ancient seas were home to thriving marine ecosystems. Fossil localities near the Talkeetna Mountains and along the southern coast contain rich assemblages of mollusks and marine reptiles, providing a window into life in northern marine ecosystems during the Mesozoic.

The Role of Citizen Science and Indigenous Knowledge

Much of Alaska’s fossil record has been unearthed through the combined efforts of scientists, local fossil hunters, and Indigenous knowledge holders. Collaborative research involving Native Alaskan communities, especially in regions like the North Slope, has been critical in facilitating fieldwork, protecting fossil sites, and sharing discoveries with local schools and museums.

Kirk Johnson: Bringing Alaska's Fossils to the Public

Kirk Johnson’s contributions extend beyond fieldwork. He is known for making paleontology accessible and engaging to the public. He co-authored Cruisin’ the Fossil Freeway with artist Ray Troll, a visually wild and informative tour of North American paleontology, including Alaskan fossil stops. Johnson has also hosted PBS documentaries like Making North America, in which Alaskan geology and fossils play a key role. 

To get your copy of Cruisin' the Fossil Freeway, here is the link:  https://www.amazon.ca/Cruisin-Fossil-Freeway-Kirk-Johnson/dp/1555914519

Additional publications by Johnson and his work in Alaska include:

Johnson, K. R. (2002). A North American perspective on the Cretaceous-Tertiary boundary in terrestrial settings. Geological Society of America Special Paper 361.

Fiorillo, A. R., & Gangloff, R. A., & Johnson, K. R. (2000). The role of polar dinosaurs in Mesozoic ecosystems: A synthesis. Journal of Vertebrate Paleontology, 20(3), 34A.

Alaska’s fossil record is one of the most compelling in the world, telling stories of survival and adaptation in the face of darkness, isolation, and dramatic climatic shifts. 

Whether it’s a duck-billed dinosaur enduring polar nights or a fossil leaf bearing witness to ancient greenhouse climates, each discovery contributes to our evolving understanding of Earth’s history. Thanks to scientists like Kirk Johnson and their ongoing efforts, we can explore these icy time capsules and better appreciate the deep-time legacy of the Last Frontier.


Tuesday, 1 July 2025

KIRK JOHNSON: FOSSIL LEAVES TO ANCIENT ECOSYSTEMS

Dr. Kirk Johnson, the Sant Director of the Smithsonian National Museum of Natural History, is a paleontologist, science communicator, and fossil enthusiast with a knack for making ancient life come alive—sometimes with a punchline. 

Known for his wide-ranging contributions to paleontology, his energetic public outreach, and his collaborative work with Alaskan artist Ray Troll, Johnson is a dynamic force in bringing prehistoric life into the public imagination.

Before taking the helm of one of the world’s premier natural history institutions, Johnson was a prolific field paleontologist. 

He earned his Ph.D. in geology and paleobotany from Yale University, but his fieldwork spans far beyond ivory towers and academic journals. 

His scientific contributions include extensive work on fossil plants and the reconstruction of ancient climates and ecosystems. Much of his research focuses on the time just before and after the Cretaceous–Paleogene (K-Pg) extinction event, offering insight into how life recovered after the asteroid impact that ended the age of the dinosaurs.

One of Johnson’s most notable research projects took place at the Hell Creek Formation in North Dakota, a hotspot for Late Cretaceous fossils. Here, he and colleagues studied the extinction horizon in unprecedented detail. Johnson helped reconstruct the rich ecosystems of the time, painting a vivid picture of a world teeming with dinosaurs, turtles, crocodiles, and flowering plants—right up until it was abruptly ended 66 million years ago.

The Troll-Johnson Dream Team

Science can be serious business, but it doesn’t have to be dry—and few partnerships prove this better than the one between Kirk Johnson and Ray Troll. Troll is a wildly imaginative Alaskan artist known for his “scientifically accurate yet deeply weird” art. 

Johnson and Troll first teamed up in the early 2000s, united by a shared love of fossils, fish, and the good old American road trip.

Together, they co-authored Cruisin’ the Fossil Freeway and its sequel Cruisin’ the Fossil Coastline, books that blend science, art, and humor in a joyful celebration of paleontology. These works chronicle their fossil-fueled road trips across North America, meeting eccentric collectors, legendary scientists, and discovering unexpected fossil treasures. 

The books are peppered with Troll’s surreal illustrations and Johnson’s breezy-yet-accurate scientific commentary.

One of the standout aspects of their collaboration is how it brings out the human side of paleontology. You get the science, sure, but also the obsessive collectors who can spot a trilobite from 20 yards away, and the museums tucked behind gas stations with dinosaur bones in the backyard. 

It’s a mix of deep time and roadside kitsch—a combination that’s both hilarious and oddly profound.

Humor in the Bone Pile

Despite his lofty position at the Smithsonian, Johnson hasn’t lost his sense of humor or sense of wonder. He’s been known to give lectures dressed in head-to-toe fossil-print suits and frequently drops fossil puns into conversations with a perfectly straight face. 

In one memorable public event, while discussing the deep-time perspective of human evolution, he paused and said, “We’ve been around for such a short amount of time that if the history of Earth were a calendar, all of human history would happen in the last few seconds of December 31. So yes, geologically speaking, you just got here—and you’re already rearranging the furniture.”

His blend of scholarship and showmanship has made him a staple on PBS programs such as NOVA, Making North America, and Polar Extremes, where he leads viewers on immersive journeys through time, across continents, and into prehistoric oceans. 

With the enthusiasm of a kid showing off their favorite rock, Johnson makes even the most complex paleoclimatic data feel like an adventure story.

Leading the Smithsonian into the Future

Since 2012, Johnson has served as the Sant Director of the Smithsonian National Museum of Natural History, one of the most visited science museums in the world. Under his leadership, the museum has revitalized its fossil halls, culminating in the stunning new David H. Koch Hall of Fossils – Deep Time, which reopened in 2019. 

This exhibit weaves 4.6 billion years of Earth’s history into a powerful narrative about evolution, extinction, and the role humans now play in shaping the planet’s future.

The exhibit doesn’t just show fossils—it tells stories. You’ll find dinosaur skeletons locked in combat, ancient mammal fossils displayed alongside their modern counterparts, and immersive displays that explain how everything from volcanoes to shifting continents has shaped life on Earth. 

It’s this kind of storytelling, infused with Johnson’s signature humor and clarity, that helps make Deep Time feel like our time. 

For a peek at the exhibits visit: https://www.si.edu/newsdesk/factsheets/david-h-koch-hall-fossils-deep-time

Whether he’s digging up a 55-million-year-old palm leaf in Wyoming, cruising for fossils with Ray Troll in a beat-up van, or explaining climate change to a packed theater with jokes and jawbones in equal measure, Dr. Kirk Johnson is a rare kind of scientist. He’s not just interested in what the past can teach us—he’s committed to making that knowledge engaging, memorable, and meaningful.

And, if you ever catch him at a fossil event, be sure to ask him about the “world’s oldest fish fart.” Odds are, he’ll have a story—and a Ray Troll illustration—to go with it.

Join in for Kirk Johnson's Keynote Lecture at the 15th BCPA Symposium

Kirk is the Keynote speaker at the 15th BCPA Symposium in Courtenay, August 22-25, 2025. For tickets, head to:  https://www.eventbrite.ca/e/15th-bc-paleontological-symposium-2025-keynote-speaker-kirk-johnson-tickets-1025014525037

Fancy some late night reading? Check out some of Johnson's publications:

Johnson, K. R. & Troll, R. (2007). Cruisin’ the Fossil Freeway: An Epoch Tale of a Scientist and an Artist on the Ultimate 5,000-Mile Paleo Road Trip. Fulcrum Publishing.

Johnson, K. R. & Troll, R. (2018). Cruisin’ the Fossil Coastline: The Travels of an Artist and a Scientist along the Shores of the Prehistoric Pacific. Fulcrum Publishing.

Smithsonian Institution: https://naturalhistory.si.edu

PBS NOVA, Making North America and Polar Extremes (Available on PBS.org)

Sunday, 29 June 2025

GHOST CATS OF THE AMERICAS: COUGARS

Cougar, Puma concolor
Cougars, also known as mountain lions, pumas, or panthers—depending on where you live—are among the most elusive and adaptable predators in the Western Hemisphere. 

Sleek, solitary, and powerful, these big cats have a long evolutionary history and play a crucial role in the ecosystems they inhabit, including the dense rainforests of Vancouver Island.

Cougars, Puma concolor, belong to the Felidae family, which includes all wild cats, big and small. Their ancestors originated in Eurasia, but the earliest true cougars appeared in North America around 6 million years ago, during the late Miocene epoch.

Fossil evidence suggests that the cougar lineage diverged from its closest relative—the cheetah—millions of years ago. Interestingly, genetic research has shown that cheetahs once roamed North America before going extinct there. 

Today’s cougar is a descendant of that shared lineage and is thought to have recolonised North America from South America following the extinction of native North American cats during the last Ice Age—about 10,000 years ago.

Cougars have one of the widest ranges of any terrestrial mammal in the Western Hemisphere. Their habitat stretches from the Canadian Yukon all the way to the southern Andes in South America.

Despite this vast range, cougars are solitary and territorial animals, preferring rugged terrain, dense forests, or rocky mountains where they can stalk prey in relative seclusion. They are excellent climbers, swimmers, and can leap over 20 feet in a single bound.

Vancouver Island, off the coast of British Columbia, is home to one of the densest cougar populations in North America. Despite being separated from the mainland, cougars are thriving here thanks to the island’s abundant black-tailed deer population and remote, forested habitat.

On the north island, they are called badi, in Kwak'wala, the language spoken by my Kwakwaka'wakw family on my father's side.

There are some resident cougars in my neighbourhood on Vancouver Island. They hunt our small island deer, the Columbian black-tail deer. When we find the deer remains, there is generally a high overhang above the spot where they were taken down, suggesting that these were ambush kills. 

While 80-90% of their diet is deer, locals feast on raccoons, beavers, rabbits and rodents. And, interestingly, not the local cats and dogs. Our neighbour was driving home and saw one of the cougars nose to nose with her cat. It was a scene of curiosity but not predation.

Estimates vary, but wildlife biologists believe there are between 600 and 900 cougars on Vancouver Island. Given the island’s size (about 32,000 square kilometres), this is considered a high density for such a large predator.

Cougars are at the top of the island’s food chain. Wolves, which often compete with or challenge cougars on the mainland, are largely absent from the island. That, combined with plentiful prey, gives cougars a unique ecological niche here.

Though rarely seen by humans, cougars occasionally make headlines on the island due to their stealthy presence in rural or suburban areas. 

Cougars are not currently endangered, but they face growing pressures from habitat loss, road networks, and conflicts with humans. 

As apex predators, they play a vital role in keeping ecosystems balanced by controlling prey populations and influencing the behaviour of other species.

On Vancouver Island, conservationists and wildlife agencies monitor cougar populations and educate the public about coexistence. This includes safe hiking practices, securing livestock and pets, and respecting the wild spaces these animals need to survive. 

Fortunately, there are still vast tracks of forest and unpeopled places for them to wander and call home. Well, mostly unpeopled, as these are some of my favourite spots to hike as well.

Saturday, 28 June 2025

MIGWAT: SLEEK, PLAYFUL SEALS

Seals—those sleek, playful creatures that glide through our oceans and lounge on rocky shores—are part of a remarkable evolutionary story stretching back millions of years. 

Though we often see them today basking on beaches or popping their heads above the waves, their journey through the fossil record reveals a dramatic tale of land-to-sea adaptation and ancient global wanderings.

Seals belong to a group of marine mammals called pinnipeds, which also includes sea lions and walruses. All pinnipeds share a common ancestry with terrestrial carnivores, and their closest living relatives today are bears and mustelids (like otters and weasels). Their ancestors walked on land before evolving to thrive in marine environments.

The fossil record suggests that pinnipeds first emerged during the Oligocene epoch, around 33 to 23 million years ago. These early proto-seals likely lived along coastal environments, where they gradually adapted to life in the water. Over time, their limbs transformed into flippers, their bodies streamlined, and their reliance on the sea for food and movement became complete.

In Kwak'wala, the language of the Kwakwaka'wakw of the Pacific Northwest, seals are known as migwat, and fur seals are referred to as xa'wa.

Friday, 27 June 2025

PORT HARDY: TIME AND TIDE

One of the most beautiful areas of Vancouver Island is the town of Port Hardy on the north end of the island. 

Just outside Port Hardy further south on the west coast is the area known as Fort Rupert or Tsaxis—my home community. 

It was here that the Hudson's Bay Company built Fort Rupert both for trade with the local First Nation population and the allure of potential coal deposits. 

I headed up to the north island this past week to stomp around my old haunts, visit with family and get in a bit of late season kayaking. The town was much as I remembered it. There have been changes, of course. I lived up on Wally's hill above the reserve at Tsaxis beside the old cemetery. 

My wee childhood home is still there and I am very pleased to see that the earthly home of my ancestors is well maintained. The cemetery is groomed and cared for but the land surrounding it is overgrown and it took me a few minutes to orient myself to see where things used to be. Where the old Hudson's Bay Company Fort and its iconic chimney were in relation to the graveyard. 

A lifetimes worth of memories came flooding back. Those from my earliest years and then later when I returned to kayak, fish and scuba dive in these rich waters.

My plans of blissful days kayaking and taking photos of the scenery were altered by hurricane-force winds. Still beautiful, but chilly and choppy.

The beachhead here was clocking 120 km winds so I did a brief visit to the homestead, the graveyard and Jokerville then headed home to light the fire and hunker in as the storm blew through. 

Port Harty and Fort Rupert have an interesting history and how you read it or hear it truly depends on the lens that is applied. This has been the ancestral home to many First Nation groups. Mostly they were passing through and coming here to dig up delicious butter clams, roots, berries and other natural yummy goodness. Years before Port Hardy was settled at the turn of the century it was the home to the Kwakiutl or Kwagu’ł and part of my heritage. 

Alec and Sarah Lyon operated a store and post office on the east side of Hardy Bay. A 1912 land deal promoted by the Hardy Bay Land Co., put the area on the map and increased its population. By 1914, 12 families had settled, built a school, sawmill, church and hotel. 

The community of Port Hardy is situated within traditional Kwagu’ł First Nation territory. It is also home to the Gwa’sala-‘Nakwaxda’xw First Nation. In 1964 all the First Nations communities were amalgamated and forced to relocate from their traditional territories by the federal government, for administrative reasons. 

The First Nation families were told that it would cost less for education, easier for medical help, and the government would help with housing, but it turned out to be a hidden agenda designed to assimilate the various groups into Canadian society — or face extermination. Several years of threats and promises later, the Gwa’sala and ‘Nakwaxda’xw reluctantly gave in to the relocation, but the government didn’t keep their promise for adequate housing. 

There were five homes for over 200 people on the Tsulquate Reservation. The Gwa’sala traditional territory is Smith Inlet and surrounding islands. ‘Nakwaxda’xw traditional territory is Seymour Inlet, the Deserter’s Group, Blunden Harbour, and surrounding islands.

There was limited access to the community until the logging road connecting Port Hardy to Campbell River was paved in December of 1979. As a child, travelling to visit my grandmother in Nanaimo meant eating eating dust behind logging trucks all the way from Hardy to Campbell doing about 40 kilometres an hour, then a stop at the Dairy Queen in Campbell River for a banana split, and on again on the old Island Highway.

Port Hardy’s population grew to a little over 5,000 residents during the Island Copper Mine years (1971-1995). The former mine site is located 16 kilometres south of Port Hardy on the shores of Rupert Inlet. The open-pit porphyry copper mine employed over 900 employees from Port Hardy and the surrounding communities. Today, the former mine has been transformed into a wildlife habitat and pit lake biological treatment system (BHP Copper Inc., 2010). The Quatsino First Nation manage the property and their Economic Development Board is exploring options for its use. 

The Quatsino First Nations have conducted several feasibility studies around the implementation of a puck or brickett mill onsite, utilizing the existing infrastructure, which includes six industrial buildings.

Today, Port Hardy serves as the crossroads for air, ferry and marine transportation networks, and serves as the gateway to the fast-growing Central Coast, the Cape Scott and North Coast Trails, and BC Ferry’s northern terminus for the Discovery Coast run and Prince Rupert. It supports several traditional and emerging sectors and remains rich in natural resources and community spirit.

Every corner of the Port Hardy region is enriched with culture and history. Starting with the two welcome poles in Carrot Park, both carved and replicated by Calvin Hunt, a Kwagu’ł artist who is based in Tsax̱is. 

From here and along the seawall are interpretive signs with Kwak’wala words for various wildlife, such as salmon, bear, wolf, and orca. At the end of this walk is Tsulquate Park. 

From here you can see across Queen Charlotte Strait; the ocean highway and lands of the Kwakwa̱ka̱ʼwakw. Port Hardy was named after Vice-Admiral Sir Thomas Masterman Hardy (5 April 1769 – 20 September 1839) who served as the captain of H.M.S. Victory in the Royal Navy. 

He served at the Battle of Trafalgar and held Lord Nelson at the end of that battle where Nelson died in his arms. Though he never visited this island community, it bears his name today. 

A ten-minute drive from downtown Port Hardy, in the neighbouring community of Fort Rupert, is the village of Tsax̱is. This is the current home of the Kwagu’ł First Nation. Here lies elaborated totem poles and the big house; a venue where First Nations ceremonies take place, such as the potlatch. 

The potlatch is a First Nations constitution that determines our politics, our government, our education, our medicine, our territory, and our jurisdiction. Potlatch is a complex event with several ceremonies, which are still practiced in buildings like the Tsax̱is big house.

On the front porch of the village of Tsax̱is is Tayaguł (Storey’s Beach). Along this waterfront were several villages, which are depicted on map (pictured below) by Mervyn Child, a Kwagu’ł artist. 

Across the way and middle of K’ak’a (Beaver Harbour) are Atłanudzi (Cattle Island), Ḵ’ut’sa̱dze (Peel Island), Ḵ’a̱msa̱x̱tłe (Shell Island), and Uxwiwe’ (Deer Island). Once the words are broken down and translated; the names of these islands are unique to their environment, as they’re part of a story that belongs to the Kwagu’ł.

Where: Port Hardy, British Columbia. 50°43'27"N, 127°29'52"W

Monday, 16 June 2025

FOSSIL HUNTRESS PODCAST

Close your eyes & fly with me as we head out together to explore Earth's rich history written in her rock. Travel to extraordinary places, sacred sites & unearth mysteries millions of years old on the Fossil Huntress Podcast.

This stream is for those who share an enduring passion for our world's hidden treasures, its wild places & want to uncover her beauty stone by stone. This is the story of the making of our Earth and the many wonderful creatures who have called it home. 

Join in the exploration of the fascinating science of palaeontology — that lens that examines ancient animals, plants & ecosystems from wee single-celled organisms to big & mighty dinosaurs.

​Learn about the interwoven disciplines of natural history, ecology, geology, conservation & stewardship of our world. To listen to the stories of the Earth, visit: https://open.spotify.com/show/1hH1wpDFFIlYC9ZW5uTYVL


Sunday, 15 June 2025

GULLS ON THE FORESHORE: TSIK'WI

A gull cries in protest at not getting his share of a meal

Gulls, or colloquially seagulls, are seabirds of the family Laridae in the suborder Lari. 

The Laridae are known from not-yet-published fossil evidence from the Early Oligocene — 30–33 million years ago. 

Three gull-like species were described by Alphonse Milne-Edwards from the early Miocene of Saint-Gérand-le-Puy, France. 

Another fossil gull from the Middle to Late Miocene of Cherry County, Nebraska, USA, has been placed in the prehistoric genus Gaviota

These fossil gulls, along with undescribed Early Oligocene fossils are all tentatively assigned to the modern genus Larus. Among those of them that have been confirmed as gulls, Milne-Edwards' "Larus" elegans and "L." totanoides from the Late Oligocene/Early Miocene of southeast France have since been separated in Laricola.

Gulls are most closely related to the terns in the family Sternidae and only distantly related to auks, skimmers and distantly to waders. 

A historical name for gulls is mews, which is cognate with the German möwe, Danish måge, Swedish mås, Dutch meeuw, Norwegian måke/måse and French mouette. We still see mews blended into the lexicon of some regional dialects.

In the Kwak̓wala language of the Kwakwaka'wakw, speakers of Kwak'wala, of the Pacific Northwest, gulls are known as t̕sik̕wi. Most folk refer to gulls from any number of species as seagulls. This name is a local custom and does not exist in the scientific literature for their official naming. Even so, it is highly probable that it was the name you learned for them growing up.

If you have been to a coastal area nearly everywhere on the planet, you have likely encountered gulls. They are the elegantly plumed but rather noisy bunch on any beach. You will recognize them both by their size and colouring. 

Gulls are typically medium to large birds, usually grey or white, often with black markings on the head or wings. They typically have harsh shrill cries and long, yellow, curved bills. Their webbed feet are perfect for navigating the uneven landscape of the foreshore when they take most of their meals. 

Most gulls are ground-nesting carnivores that take live food or scavenge opportunistically, particularly the Larus species. Live food often includes crab, clams (which they pick up, fly high and drop to crack open), fish and small birds. Gulls have unhinging jaws which allow them to consume large prey which they do with gusto. 

Their preference is to generally live along the bountiful coastal regions where they can find food with relative ease. Some prefer to live more inland and all rarely venture far out to sea, except for the kittiwakes. 

The larger species take up to four years to attain full adult plumage, but two years is typical for small gulls. Large white-headed gulls are typically long-lived birds, with a maximum age of 49 years recorded for the herring gull.

Gulls nest in large, densely packed, noisy colonies. They lay two or three speckled eggs in nests composed of vegetation. The young are precocial, born with dark mottled down and mobile upon hatching. Gulls are resourceful, inquisitive, and intelligent, the larger species in particular, demonstrating complex methods of communication and a highly developed social structure. Many gull colonies display mobbing behaviour, attacking and harassing predators and other intruders. 

Certain species have exhibited tool-use behaviour, such as the herring gull, using pieces of bread as bait with which to catch goldfish. Many species of gulls have learned to coexist successfully with humans and have thrived in human habitats. Others rely on kleptoparasitism to get their food. Gulls have been observed preying on live whales, landing on the whale as it surfaces to peck out pieces of flesh. They are keen, clever and always hungry.

Tuesday, 10 June 2025

EXPLORING WRANGELLIA: HAIDA GWAII

Misty shores, moss covered forests, a rich cultural history, dappled light, fossils and the smell of salt air—these are my memories of Haida Gwaii.

The archipelago of Haida Gwaii lays at the western edge of the continental shelf due west of the central coast of British Columbia.

They form part of Wrangellia, an exotic tectonostratigraphic terrane that includes Vancouver Island, parts western British Columbia and Alaska.

The Geological Survey of Canada sponsored many expeditions to these remote islands and has produced numerous reference papers on this magnificent terrain, exploring both the geology and palaeontology of the area.

Joseph Whiteaves, the GSC's chief palaeontologist in Ottawa, published a paper in 1876 describing the Jurassic and Cretaceous faunas of Skidegate Inlet, furthering his reputation globally as both a geologist, palaeontologist as well as a critical thinker in the area of science.

The praise was well-earned and foreshadowed his significant contributions to come. Sixteen years later, he wrote up and published his observations on a strange Mount Stephen fossil that resembled a kind of headless shrimp with poorly preserved appendages. 

Because of the unusual pointed shape of the supposed ventral appendages and the position of the spines near the posterior of the animal, Whiteaves named it Anomalocaris canadensis. The genus name "Anomalocaris" means "unlike other shrimp" and the species name "canadensis" refers to the country of origin.

Whiteaves work on the palaeontology of Haida Gwaii provided excellent reference tools, particularly his work on the Cretaceous exposures and fauna that can be found there.

One of our fossil field trips was to the ruggedly beautiful Cretaceous exposures of Lina Island. We had planned this expedition as part of our “trips of a lifetime.” 

Both John Fam, the Vice Chair of the Vancouver Paleontological Society and Dan Bowen, the Chair of both the British Columbia Paleontological Alliance and Vancouver Island Palaeontological Society, can be congratulated for their efforts in researching the area and ably coordinating a warm welcome by the First Nations community and organizing fossil field trips to some of the most amazing fossil localities in the Pacific Northwest.

With great sandstone beach exposures, the fossil-rich (Albian to Cenomanian) Haida formation provided ample specimens, some directly in the bedding planes and many in concretion. Many of the concretions contained multiple specimens of typical Haida Formation fauna, providing a window into this Cretaceous landscape.

It is always interesting to see who was making a living and co-existing in our ancient oceans at the time these fossils were laid down. We found multiple beautifully preserved specimens of the spiny ammonite, Douvelleiceras spiniferum along with Brewericeras hulenense, Cleoniceras perezianum and many cycads in concretion.
Douvelliceras spiniferum, Cretaceous Haida Formation

Missing from this trip log are tales of Rene Savenye, who passed away in the weeks just prior. While he wasn't there in body, he was with us in spirit. I thought of him often on the mist-shrouded days of collecting. 

Many of the folk on who joined me on those outcrops were friends of Rene's and would go on to receive the Rene Savenye Award for their contributions to palaeontology. There is a certain poetry in that. 

The genus Douvilleiceras range from Middle to Late Cretaceous and can be found in Asia, Africa, Europe and North and South America. 

We have beautiful examples in the early to mid-Albian from the archipelago of Haida Gwaii in British Columbia. Joseph F. Whiteaves was the first to recognize the genus from Haida Gwaii when he was looking over the early collections of James Richardson and George Dawson.

My collections from Haida Gwaii will all be lovingly prepped and donated to the Haida Gwaii Museum in Skidegate, British Columbia.