Herbarium Sheet Mounting: Adhesives Recommendations That Really Stick

In the summer of 2018 Jennifer Doubt, the museum’s botany curator, presented me with a challenge: find a better adhesive for mounting the museum’s botany specimens on herbarium sheets.

I was working in the museum’s Conservation lab as part of the Scientific Training Program, but my background is in fine arts, and conservation training with materials including metal, wood, textile, and paper conservation—not conserving ferns and flowers. Natural history conservation is specialized and rarely taught in conservation programs in Canada. So, I was excited for the opportunity to challenge myself in something new.

Having the best possible adhesive is critical because every year the botany team adds more than 5,000 specimens to the museum’s National Herbarium of Canada which includes more than 650,000 herbarium sheets in the vascular plant collection. At present, new specimens are attached to herbarium sheets using linen tape, a process that’s effective, but very time consuming. My task was to find a conservation glue that’s easy and quick to apply and keep specimens stuck for a long time.

Notice the missing section of this spreading wood fern (Dryopteris expansa). Over time the adhesive holding the specimen to the herbarium sheet aged and failed, resulting in the loss. Specimen collected in 1895. Catalogue number CAN 10005210. Image: © Canadian Museum of Nature.

This alpine hedysarum (Hedysarum americanum) is attached to its herbarium sheet with linen tape. This technique allows the plant to bend with the sheet, decreasing the risk of breakage and loss. But applying linen tape is a time-consuming process, with each piece of tape carefully cut and placed by hand. Specimens collected in 2016. Catalogue number CAN 10042881. Image: © Canadian Museum of Nature.

My core challenge was that in the conservation literature there’s no single recommended adhesive for herbarium collections. So, in my search for the best adhesive I considered the museum’s needs while exploring new research in adhesives.

Three of the key herbarium conservation needs are strength, flexibility, and neutral pH. Herbarium specimens must be conserved for decades, if not centuries. So an adhesive must have enduring strength to hold a specimen on its sheet and also flexibility to keep it held while the sheet’s handled by researchers.

A neutral pH keeps the surrounding substrate from becoming acidic, turning yellow, and prematurely aging.

This closeup image of a subalpine fir (Abies lasiocarpa) herbarium sheet shows that the adhesive has browned with age masking some of the specimen from view. The browning also indicates that the adhesive’s become acidic, which could cause damage to the area over time. Specimen collected in 1975. Catalogue number CAN 10005767. Image: © Canadian Museum of Nature.

In addition to these archival requirements, the adhesive I was looking for also needed to have other practical properties. It needed to be water-based, high tack, and clear when dry.

The Canadian Conservation Institute’s long-term study of commercially available adhesives, Adhesive Compendium for Conservation was an invaluable resource.

My research led me to recommend three neutral pH polyvinyl acetate (PVA) adhesives or “white” glue.  These adhesives have both great workability properties in the lab and long-term preservation qualities. They have stood the test of time while remaining strong, flexible, neutral, and exhibiting minimal yellowing.

My adhesive research truly stuck with me. It enabled me to more deeply appreciate how in the selection of conservation materials every small detail must be considered to ensure the preservation of collections.

Understanding material characteristics and their deterioration was a core concept in my conservation training. I’m proud to know that what I contributed to the museum’s herbarium will increase the chance that in the 22^nd century a museum botanist will hold a herbarium sheet prepared today—with its specimen still firmly attached.

In Jassa mating: A thumb matters

This year marks the 30^th anniversary of my Ph.D.-related publications about tiny, shrimp-like animals called Jassa. I set out to discover a way to tell the species apart based on their appearance. But soon I asked why they looked that way.

Blog author and museum scientist Kathy Conlan in 1980 searching for Jassa in a sample collected in southeastern Alaska. Image: Ron Long, © Canadian Museum of Nature

First, a little about Jassa. It’s a genus of 20 species of marine, colonial amphipods, in which each male or female lives in a self-made tube that it attaches to almost anything hard, from rocks and docks to boat hulls. Species of Jassa live on most rocky shores and harbours around the world from Newfoundland to the Antarctic (not yet in the Arctic, but see Cruising the Globe Undetected). Anchored in their tubes, they extend into the water to capture passing plants and animals or scrape up bits of dead organic material called detritus. Being without a tube could be a death sentence as Jassa is easy prey to fishes.

A female Jassa marmorata in her tube. Her four antennae are outstretched to capture passing phytoplankton, zooplankton and detritus. Image: Kathy Conlan, © Canadian Museum of Nature.

Yes, it’s mostly a sedentary life, but things get interesting when it comes time to mate.

Inside its tube, Jassa grows in stages, splitting its old outer “skin”, or cuticle, after it has grown a new, slightly larger one inside, a process called molting. For a mature female, this is the only time that her cuticle is flexible enough to allow the release of her unfertilized eggs into her external brood pouch. For a mature male, this is the only time that he can fertilize her eggs.

This opportunity to mate is very short, only a couple of hours long. So there is fierce competition among adult males to find a female that is receptive to mating. The females broadcast their receptiveness by releasing attractive chemicals. The adult males abandon their tubes, roving to find the receptive females. But the females are choosy. They will only accept males with the right look. These males have to have a thumb (an enlargement on a gnathopod, or pincer). The thumb signals an intent to mate. Thumbless males are intent on evicting the female from her tube, and so she drives them off.

The thumbed males fight to guard the receptive female until she is ready to molt and release her eggs. Once fertilized, the embryos grow inside the eggs until hatching as miniature Jassas.

Confrontation between two large-thumbed male Jassa marmorata. Image: Kathy Conlan, © Canadian Museum of Nature.

In my doctoral research, I discovered that not all Jassa thumbs are alike. In every species, big males had big thumbs but some little males had smaller thumbs than would be expected for their body size. Some also had ornaments that the big males did not have. I thought this might indicate that the little males behaved differently and follow-up studies by other scientists have confirmed this for Jassa marmorata.

The little males appear when there has been not much protein from phytoplankton and zooplankton to feed on, so they had to depend on a less healthy diet of bits of detritus. But what little thumbed males lack in size, they sometimes make up for in behaviour.

A male Jassa marmorata with a major thumb on its gnathopod (below and to the right of its head). The size of the adult male’s thumb seems to depend on its diet. A well-fed big “major” male produces a big thumb. Nutrient poor environments result in small “minor” males with smaller thumbs than expected for their body size. Image: Susan Laurie-Bourque, © Canadian Museum of Nature.

Faced with a big male with an over-sized thumb, the little males seemingly don’t stand a chance. But in fact, they do. They are quick to mature and their small thumbs are big enough to signal the female not to reject them. When they outnumber the big males, they win the mating. And females will accept more than one male to mate with, increasing the odds that little guys can succeed too.

So, different strategies work for different situations. The fascinating Jassa mating ritual dances to the rhythm of how a male presents his thumb.

 

A possible new species almost found — but lost

Several years ago a colleague sent me two specimens of blind cave fish collected in the Zagros Mountains of western Iran. I was intrigued. The specimens were small, just 2.5 centimetres long, and in very bad condition. But I could tell they belonged to the cyprinid genus Garra — and there were hints they are probably a new species to science. But, we’ll probably never know, and to explain why requires some background context.

Cave fishes are fascinating creatures whose habitat is usually the water in limestone caves, including tiny cracks between rock layers, and often occurring over very wide areas. Blind cave fish are related to species living in nearby streams and rivers. But, in the absence of light deep underground, there’s no advantage in maintaining eyes and sight. They’ve also lost skin pigmentation, appearing pink, a result of blood visible through their unpigmented skin. The blind cave fishes are thus different species, clearly defined by their DNA.

The Iranian cave barbs Garra lorestanensis and G. typhlops are blind cave fishes similar to the unidentified specimens sent to museum fish expert Brian Coad. Image : Ruhollah Mehrani, © Lorestan Research Centre of Natural Resources and Animal Science, Khorramabad, Iran.

Four species of blind cave fishes are known to exist in the Loven and Tashan caves in Iran, including three members of the Cyprinidae family (carps) and one of the Nemacheilidae family (loaches). However, these sites are respectively about 130 and 270 km away from where the new specimens were collected, heightening the possibility the specimens represented a new species.

Dip netting for fish at the Loven cave in Iran. Image: Brian Coad, © Canadian Museum of Nature.

Since the specimens were in poor condition, the only way to solve the mystery was to collect more. Unfortunately, this is no longer possible. They were collected from a shallow pool formed from water seeping from a rock face when a tunnel was drilled through a mountain during construction of the Simareh dam in 2005. The tunnel where they were collected in now buried, encased in concrete.

Faced with this dead-end, we thought we might be able to solve the question by examining the DNA of the specimens and comparing it to that of known Iranian cave fishes DNA available in an online database. Despite the valiant efforts of the museum’s DNA specialist Roger Bull, this route also failed. The fishes’ genetic material was damaged beyond recognition by time and its initial preservation in formalin.

Thus, it appears that this possible new species of blind cave fish may have been lost to science before it was truly found.

Yet, ironically, currently buried under hundreds of metres of rock and concrete, it may now be safe from any further ravages, whether natural or human-caused.

Champsosaurus: CT scanning reveals its ear openings really were on the bottom of its skull

At Ottawa’s Alta Vista Animal Hospital, when an animal gets a CT scan it’s usually a cat or dog and the vet is looking for broken bones or tumours.

But I brought a Champsosaurus, and I wanted a CT scan to look for its ears.

Let me explain. The up to two-meter long Champsosaurus was a genus of aquatic reptile that lived from 90 to 55 million years ago. Champsosaurus resembled modern crocodiles, but is only distantly related to them, and has no descendants alive today.

A large specimen of Champsosaurus natator, a species that lived in western North America from about 70 to 66 million years ago. On display in the Fossil Gallery at the museum. Catalogue number: CMNFV 8919. Image: Thomas Dudgeon, © Canadian Museum of Nature.

So, what we know about Champsosaurus comes from its fossil remains, and this leads to the ear problem.

Champsosaurus had a relatively delicate skull, with a long and slender snout and large arches of bone at the back of the skull that anchored jaw muscles. The skull was so fragile that few are well preserved, and thus little is known about the finer internal structures such as the braincase and the inner ear.

Top view of a well-preserved Champsosaurus skull in the Canadian Museum of Nature collection. Fun fact: Scientists call heart-shaped objects cordiform. Tilt your head to the right and see how the long snout and large arches of bone give Champsosaurus a heart-shaped skull. Catalogue number: CMNFV 8920. Image: Thomas Dudgeon, © Canadian Museum of Nature.

However, in the 1950s, museum palaeontologist L.S. Russell suggested that holes on the bottom surface of the Champsosaurus skulls were the ear openings. As you can imagine, this is a strange place for ear openings to be, and not all palaeontologists were convinced. Although some animals, like a few salamander species, have ear openings on the bottom of their skulls, most animals, including humans of course, have ears on the sides of their skulls.

So, as part of my Master’s thesis in Carleton University’s Department of Earth Sciences, I decided to tackle the mystery of whether the Champsosaurus’ ears really were on the bottom of its skull.

Fortunately, there are two well-preserved skulls of Champsosaurus in the Canadian Museum of Nature’s palaeo collection.

A Champsosaurus skull ready to go through a CT scanner at Ottawa’s Alta Vista Animal Hospital. Catalogue number: CMNFV 8919. Image: Thomas Dudgeon, © Canadian Museum of Nature.

I carefully transported one skull to the Alta Vista Animal Hospital for a much overdue check-up, and the other was sent to the University of Texas CT facility for scanning. CT scanning is a medical technique that uses X-rays to create hundreds of thin cross-sectional images, providing a detailed view of the internal structures.

When I examined the CT scans of the Champsosaurus skulls, to my surprise and excitement, I discovered that the openings on the bottom of the skull do indeed lead to the inner ear.

A line drawing of a Champsosaurus skull in bottom-view, ear openings highlighted in blue. Catalogue number: CMNFV 8920. Image: Thomas Dudgeon, © Canadian Museum of Nature.

This of course raises the question of why Champsosaurus’ ear openings were on the bottom of its skull. It may have been due to the fact that the large arches of bone at the back of the skull were so prominent they displaced the ear openings from the side to the bottom.

To explore other possibilities, and how this influenced its hearing, I’m now comparing Champsosaurus ear anatomy to that of modern reptiles and amphibians.

I hope it will give me a sense of what this intriguing Cretaceous creature could hear with ears on the bottom of its skull.

Zeroing in on Inuit origins through archaeology and ethnography

This past summer, after years of fieldwork mostly in the Middle East, I began my first archaeological research in the Arctic.

This represents quite a change for me, and not just because I was used to seeing camels rather than walrus.

Compared with the Middle East, archaeological sites in the Arctic are generally smaller, were occupied for relatively brief periods of time, and are more widely scattered across the landscape. This makes finding sites and interpreting the broader picture of the human story in the Arctic more difficult.

Museum archaeologist Scott Rufolo touring the Giza Plateau in Egypt, and (right) excavating the remains of a prehistoric house on an island near Igloolik, Nunavut. Images: © S. Rufolo (left); © S. P. A. Desjardins (right).

And it’s why my new research project, in collaboration with researchers at the University of Groningen’s Arctic Centre, is so interesting and valuable.

The Foxe Basin is rich in wildlife in part because local areas of ocean remain ice-free even during the depths of winter. This enables numerous species of birds and marine mammals, including walrus, to maintain relatively large year-round populations, ones that sustain human communities. Image: S. Rufolo, © Canadian Museum of Nature

The project is documenting a rare grouping of several densely concentrated archaeological sites located in the Foxe Basin. Together they contain remains spanning several cultural periods, providing a nearly continuous archaeological record documenting several thousand years.

This concentration of sites and multi-period representation is due in large part to the natural history of the Foxe Basin. The geography of the region contributes to a comparatively moderate climate with seasonal sea-ice patterns favourable to many forms of marine life, including large animals such as the walrus. In fact, walruses are able to live in the basin year-round, providing a valuable and stable food supply for humans.

Walruses (Odobenus rosmarus) in the Foxe Basin, such as this mother and calf, are able to reside in the area year-round due to the presence of polynyas, areas of open water within the winter ice. Other mammals, birds and fish in the region include: ringed seal, narwhal, beluga, and caribou; ptarmigan and geese; and Arctic Char and Cod. Image: © Ansgar Walk (CC BY-SA 3.0)

The rich archaeological remains preserved here provide a rare opportunity to explore the transition from ancient Thule to modern Inuit cultures. The Thule, the immediate ancestors of the Inuit, were a people who spread eastward from Alaska beginning around AD 1100, reaching Greenland within 200 years and displacing the earlier Dorset culture of the central and eastern Arctic.

Ethnogenesis is the emergence of a new cultural group who view themselves as ethnically distinct from previous societies, and surrounding contemporary ones. The ethnogenesis of Inuit from Thule culture started in the 17th century, but this transition is not well understood.

We began our three-year project with a field season at Avvajja. It’s an archaeological site on an island just to the west of Igloolik Island that represents the very end-point of the Thule-to-Inuit continuum. Avvajja was used as a winter settlement by the Inuit up to the early 1950s, when people relocated to the new hamlet of Igloolik. There are elders alive today who remember living at Avvajja as children.

A group of elders from Igloolik arrives at Avvajja to share their childhood memories of living there. Image: S. Rufolo, © Canadian Museum of Nature.

Project director Dr. Sean P. A. Desjardins and the team’s translator discuss responses from Inuit elders about how Avvajja living spaces and activity areas were used. Image: S. Rufolo, © Canadian Museum of Nature.

Two days of our fieldwork were devoted to interviewing elders on site so that they could share their memories of living at Avvajja as children. Combining mapping and excavations with these interviews will enable us to illuminate the archaeological record to a greater extent than would be possible through digging alone.

This coming summer, work will continue at the site of Uglit on the Melville Peninsula, where a longer season will connect the historic occupation at Avvajja to the immediately preceding centuries (AD 1600-1900) during which the Thule-to-Inuit transition occurred.

As we gather more data and deepen our chronological representation, we hope to contribute greater detail to our knowledge of the cultural shifts that signal the rise of Inuit society — a culture that I am discovering is just as fascinating and rich as those that initially drew my interest to the Middle East.

The remains of several Inuit winter houses, many in use up to the early 1950s, are present at Avvajja. This house is typical, with a low, stone foundation partially covered in the sod that formed the base of the home. Image: S. Rufolo, © Canadian Museum of Nature.

At the end of the field season, a community gathering was held at the site so that elders could relate their stories of life at Avvajja directly to their family and friends while seated around the remains of their former houses (inset). Traditional foods served included frozen fish, raw seal meat, and igunaq (ᐃᒍᓇᖅ), fermented walrus (the two large yellow and red masses on the right in the main photo). Image: S. Rufolo, © Canadian Museum of Nature.

Work at Avvajja included the excavation of a prehistoric house dating to the Late Dorset period, around 1,200 years ago. Collected sediments were sieved in order to recover small stone tools. The excavation produced a mystery artifact (inset). Now at the Canadian Conservation Institute in Ottawa for treatment, it may be the first known example of clothing from the Dorset culture. Image: S. P. A. Desjardins, © S. P. A. Desjardins (main photo); S. Rufolo, © Canadian Museum of Nature (inset)

Pyrite Disease: Keeping Fool’s Gold Challenges Museums

Pyrite, or fool’s gold, has duped prospectors for millennia, and now it’s providing a tricky challenge for museums.

Pyrite is a very common mineral found worldwide and in a very large variety of rocks. The Canadian Museum of Nature collection holds about 800 pyrite specimens. Each specimen has the identical chemical formula — iron disulfide, FeS₂. But slight differences in the conditions in which a pyrite specimen formed gives each a unique shape, with cubes being the most common.

An excellent pyrite specimen with a bright gold colour and cubic shapes. Catalogue number: CMNMC 43372. Image: Christian Capehart © Canadian Museum of Nature.

With its shiny yellow colour and metallic shine, pyrite closely resembles gold. Even more confusingly, it also commonly occurs with gold deposits. Many prospectors have thought they struck it rich when they actually just found a lode of pyrite, hence its common name.

Now, museum staff are dealing with another of the mineral’s challenging characteristics: pyrite can rust.

When exposed to humid air, pyrite reacts with oxygen and water to create iron sulfide (the rust), corrosive sulfuric acid and harmful sulfur dioxide gas. This chemical reaction, called pyrite disease, causes specimens to crack and crumble. Left unchecked, pyrite disease eventually destroys a specimen.

Moreover, the corrosive acid and gas can destroy the storage containers holding the pyrite and even damage surrounding minerals. This is why it’s called pyrite disease, because it acts like a contagious infection that can spread. The acid and gas are also a health hazard for museum staff.

A specimen of pyrite damaged by pyrite disease, resulting in cracks and discolouration. Image: Christian Capehart © Canadian Museum of Nature.

Since the museum holds pyrite specimens that are of great scientific interest and stunning beauty, it is of the utmost importance that we take proactive steps to preserve them.

Pyrite oxidation is triggered by humid air, so the best ways we have found to prevent pyrite disease are to lower the humidity of the collection room and keep the specimens in dry, impermeable containers.

With these steps, the museum’s pyrite specimens have the potential to keep fooling the unwary for millennia.

Triceratops skull delivers a Wow! of a Christmas gift

Removing dinosaur bone from rock is much like opening a Christmas gift: you never know what to expect. Sometimes, if you are really lucky, what’s revealed makes you take a step back and say, Wow!

And that’s exactly the early holiday surprise I got several weeks ago working on the museum’s one-of-a-kind Triceratops skull. It might contain the world’s first fossil evidence of this horned-dinosaur’s skin from the area of the neck frill.

When I last wrote about the partial skull of a large Triceratops prorsus in our collections, I had just started preparation work on the specimen. From reading Charles M. Sternberg’s 1929 original field notes, our expectations were already high. The complete frill and both horn cores he collected and preserved in two plaster jackets could be the world’s largest Triceratops.

Drawing of a Triceratops prorsus skull collected by the pioneering American palaeontologist Othniel Charles Marsh. The first fossils of this famous horned dinosaur were found in the late 19th century in Colorado, and have since been collected from Wyoming, South Dakota, Alberta and Saskatchewan. © Biodiversity Heritage Library (CC BY-SA 2.0)

Now, after five months of meticulous work on the backside of the bony frill, a completely unexpected find has emerged that could change our view of what Triceratops looked like.

A major challenge in preparing this Triceratops specimen is that much of the skull is fractured, and between these thin gaps in the fossil, tiny fragments and rock dust have accumulated. Before the fractures can be repaired, this accumulation must be removed.

A section of the bony shield that flared out around the neck of our Triceratops specimen, seen here sitting in a plaster jacket in the museum’s palaeontology workshop. The surface has been partially cleaned revealing many fractures. When C. M. Sternberg examined this fossil soon after its discovery in 1929, he made note of its exceptionally large size. Catalogue number: CMNFV 56508. Image: Alan McDonald, © Canadian Museum of Nature.

View of the frill section from above following complete exposure and cleaning of the numerous fractures that riddle the surface. One such fracture held a fragment containing a very interesting surprise — what appears to be preserved skin. Catalogue number: CMNFV 56508. Image: Alan McDonald, © Canadian Museum of Nature.

One afternoon in early October, as I was removing and sifting through the dust trapped in the fractures, I noticed a small, broken section of fossil.

A triangular-shaped piece of fossilized bone had separated from the main frill, but remained largely in place.  As I cleared the rock fragments and lifted out this small bit of fossil bone, what I saw underneath it made me quickly set down my brush.

To my surprise, there was a small section of what looks to be beautifully fossilized dinosaur skin.

This block of sediment covered a portion of the Triceratops frill and bears the impression of its surface features, including deep channels and pits. These may have once harboured blood vessels and other soft-tissue structures. One theory concerning the frills of horned dinosaurs is that they were covered in a hard sheath, perhaps composed of keratin, just like our fingernails. It’s possible that this protective covering was so dense and tight against the skull that the blood vessels providing oxygen and nutrients normally found in the soft tissue instead grew into the outer layers of the bone of the skull. Catalogue number: CMNFV 56508. Image: Alan McDonald, © Canadian Museum of Nature.

If so, it is the first evidence of skin from the head of this dinosaur species. Since it was first discovered in 1887, there has been no fossil material found to give any clear indication of what covered this horned dinosaur’s iconic frill. For more than a century, it was assumed that a mosaic of scales covered the surface of the frill, but others have more recently suggested that it was instead covered by a tough, horny sheath. Until now, we had no way to be sure.

The polygonal features seen in this photo appear to be the remains of fossilized skin preserved in association with the frill. The fossil has been removed for further study to confirm this initial identification. Once preparation of the top side of the frill is underway, it may finally provide some answers regarding the nature of the skin on a horned dinosaur’s neck shield, and perhaps also earn the specimen the title of the largest Triceratops skull ever described. Catalogue number: CMNFV 56508. Image: Alan McDonald, © Canadian Museum of Nature.

Taking a closer look at the section of distinctly patterned features with Dr. Jordan Mallon, the Canadian Museum of Nature’s dinosaur specialist, we decided we needed to re-examine how best to approach preparing the opposite side of the frill. We want to not only preserve any delicate fossilized skin it may retain, but if possible, also keep it from separating from the bone.

With this in mind, I am proceeding even more carefully and slowly in continuing the finer preparation and stabilization of the currently exposed side of the frill. Over the next few weeks, we will create a new plaster jacket to support the specimen, flip it over, and then see what new surprises the other side might have for us.

For now, though, I am quite content to enjoy this early, unique Christmas gift of probable fossilized Triceratops skin!

Cruising the Globe Undetected

Emeritus museum scientist Ed Bousfield (now deceased) found that Jassa marmorata’s native range in Atlantic North America was on wave-exposed, natural shores, far from harbours and other human-built structures. Image: Kathleen Conlan, © Canadian Museum of Nature

The little shrimp-like animal Jassa marmorata was never thought to be a hitchhiker until museum collections told us otherwise. Now we’re finding out that it has been using humans to cruise the globe for centuries.

Each individual Jassa lives in the ocean in a self-built tube which it glues to its neighbour’s tube. When thousands get together, they amass a gooey colony that fouls anything solid. As a result, Jassa is infamous for blocking water pipes, clogging aquaculture nets and coating oil rigs.

This ability to stick and hold has also made this little marine creature a global hitchhiker.

Two Jassa marmorata males on the left. Their large front claws are a signalling device. A Jassa marmorata female in her homemade tube on the right. Image: Kathleen Conlan, © Canadian Museum of Nature.

Early explorers started it. The hulls of wooden ships were ideal for Jassa to stick and go.

The collections of the Natural History Museum in London, England reveal that the H.M.S. Challenger was likely distributing Jassa marmorata from Europe to the Southern Hemisphere as it travelled around the world from 1872 to 1876. Jassa marmorata was found swimming beside the ship in the deep ocean off of South Africa and again near Chile, far from its natural rocky shore habitat. Probably it was living on the ship’s hull and periodically falling off, duping the naturalists aboard ship into thinking that it was a local.

Through decades of dispersion—including from oyster imports and emptied ballast water—the North Atlantic native, Jassa marmorata is now fouling harbours in South America, Asia, Russia, Australia, New Zealand, Africa, the Middle East, and most of Europe. Historical collections show that it has been fouling some of these harbours since the 1800’s, though ship commerce may have been distributing it much earlier.

As it circumnavigated the globe from 1872 to 1876, the H.M.S. Challenger unwittingly gave a North Atlantic native, Jassa marmorata, a round-the-world tour. Image: William Abbott Herdman, Public domain. Source: Wikipedia Commons

Unwitting scientists may still be giving Jassa a lift to new habitats.

A recent deep-sea expedition sampled the seabed from Europe to the North Pole. In collected samples, it found Jassa marmorata all the way there and back while no other species was so consistently found. Jassa marmorata has never been found in mud, or deeper than about 30 meters, and never in the Arctic.

Was it really living in mud at 4000 meters under the sea ice at the North Pole? Not likely.

I bet this world-class hitchhiker was living in the ship’s seawater system. Every time the hoses were used to sieve the mud from samples, a few Jassa were dislodged and contaminated the sample—and just maybe, dropped off Jassa at another destination.

Plant and animal life on a floating dock edge in Australia. The North Atlantic Jassa marmorata was first detected in Australia in 1881. The beautiful fan worms (upper half of the photo) are also an introduced species. Image: Kathleen Conlan, © Canadian Museum of Nature.

War Ornithologists

The two great wars that marked the first half of the 20th century saw a substantial number of recruits mobilized and sent to the front. Given that the recruits were from all walks of life, inevitably there were some who were passionate about the natural sciences. Despite harrowing living conditions, some soldiers tried to document the “natural” environment in which they were immersed. The Canadian Museum of Nature holds specimens dating from these difficult times; here are three examples.

Left: a magpie collected in Flanders in March 1917 by Major Allan Brooks. Catalogue number: CMNAV 13020. Eurasian Magpie (Pica pica). Image : Michel Gosselin © Canadian Museum of Nature Right: Major Allan Brooks. Image from the Biodiversity Heritage Library. Public domain.

Allan Brooks (1869–1946) was a wildlife artist living in British Columbia. He had joined the militia even before the start of the First World War, and spent the entire period from 1914 to 1918 in England and France.

In 1917, he was posted at Mont des Cats in Flanders (a place that would be the scene of a significant German offensive). It was there that he was able to collect some bird specimens, and pass them on to his colleague Percy Taverner, the first ornithologist of what is now the Canadian Museum of Nature. It is known that Brooks partly lost his hearing while at the front, to the point where he said he was “no longer able to hear the song of the skylark”

Upon his discharge, Allan Brooks had reached the rank of lieutenant-colonel. Back home, he contributed illustrations to Percy Taverner’s 1926 Birds of Western Canada. Brooks deposited many of his European specimens with the Canadian Museum of Nature.

Birds in the War-Zone, written in October 1916, describes his ornithological observations in Europe. Notably, he wrote that some birds did not seem to be unduly affected by artillery fire, which sometimes lasted for hours.

The Canadian Museum of Nature has specimens from both sides of the front. Here, a quail collected in Russia in 1943 by a soldier of the German army. Catalogue number: CMNAV 68810. Common Quail (Coturnix coturnix). Image: Michel Gosselin © Canadian Museum of Nature.

The young Viennese ornithologist Rudolf Tomek (1913–1943) was an employee of the Provincial Museum of Lower Austria. When Germany annexed Austria, he was conscripted into the army and sent to the front, in Russia, in 1942. The following year, he was killed during a Russian counteroffensive in the Orel region, south of Moscow.

Tomek had managed to send some birds collected in Russia to the Vienna Museum of Natural History. By a singular combination of circumstances, one of these specimens (a Common Quail) was part of a 1979 exchange of specimens between this Austrian museum and the Canadian Museum of Nature.

This hawk is among the specimens collected by Corporal Allan R. Phillips as part of research on Japanese encephalitis vectors on Okinawa Island after the US landing in 1945. Catalogue number: CMNAV 96710. Grey-faced Buzzard (Butastur indicus). Image: Michel Gosselin © Canadian Museum of Nature.

Allan R. Phillips (1914–1996) was a biologist best known for his work on the birds of Arizona and Mexico. In 1942, while a doctoral student in ornithology at Cornell University (New York, USA), he was enlisted in the US Army.

After surviving the Normandy landing in 1944, he was dispatched to Japan during the invasion of Okinawa Island in 1945. On the island, he met by chance a Cornell colleague, Sergeant Frank Cassell, who assigned Phillips to medical research

Corporal Phillips thus found himself studying the birds of Okinawa Island as potential vectors of Japanese encephalitis. Some of the specimens collected during this period now belong to the Canadian Museum of Nature which acquired part of Phillips’ collections in 1980.

(Translated from French)

One Hundred Lichens New to Quebec, Canada, and North America from the Gaspé Peninsula

In 2007, during an alpine ski touring trip in the backcountry of Parc national de la Gaspésie on the Gaspé Peninsula in eastern Quebec, I noticed a surprisingly rich lichen diversity. This discovery inspired me to begin an ongoing study of the park’s lichens.

I was not the first scientist drawn to Gaspé to explore lichens. In the late 1800’s, John Macoun, Canada’s first Dominion Botanist (and a lichenologist), collected specimens in the area that is now the park. In the early 1900’s, Merrit Fernald, a Harvard University professor and botanist, lead several trips to the region to study its plants and lichens.

Merritt Fernald (furthest left) and his 1923 expedition team to the Gaspé Peninsula. Image: © Gray Herbarium Archives, Harvard University.

These pioneering collectors were the first of more than 40 researchers who have studied the park’s lichens. When I began my study, almost 300 lichen species were known in the park. There are now over 600 species, ranking the park among North America’s richest lichen locales.

Many of the new discoveries were made with the help of my colleagues during our annual gathering of lichenologists, the Tuckerman Workshop. We found 100 lichens in the park that had never been reported from Quebec. Twelve of these species are new to Canada and six of those are new to North America.

The North American distribution of the limestone sunshine lichen, Vulpicida juniperinus. The population in Parc national de la Gaspésie is marked with a red triangle. Image: R. Troy McMullin © Canadian Museum of Nature.

The rich lichen biota in Parc national de la Gaspésie is due to its diverse habitats, including old-growth woodlands, different forest types, lush river valleys, and a coastal influence. The mountain summits also have arctic-alpine environments and contain species that otherwise only grow in the western mountains and the Arctic. For example, the limestone sunshine lichen Vulpicida juniperinus is at its southern range limit in eastern North America in the park. The closest population occurs over 1000 km to the north.

Parc national de la Gaspésie from the summit of Mount Albert. Image: R. Troy McMullin © Canadian Museum of Nature.

My lichen study in the park will continue until all corners have been explored and the discovery of new species becomes infrequent.