by Russell Garwood*1
“Increasing knowledge leads to triumphant loss of clarity” — Palaeontologist Alfred Romer
Some areas of life and human endeavour have the luxury of certainty. Along these paths of discovery, there are things we can know to be true or false. In others, it is impossible to assess the concept of truth: it can’t be established, or just isn’t a consideration. And between these extremes is a whole mess of important stuff. Palaeontology almost always lies somewhere on this gradation. Researchers studying past life are often juggling multiple layers of uncertainty. We try to balance the need to say something useful — something with meaning, that moves a field and its consensus closer to the truth — with the risk of over-interpreting our data. If the data is t
by Gabriel Santos1
In the world of education, we often hear complaints that people know more about celebrities and fictional characters than about science. Taking a moment to scroll through Twitter or Instagram, it can be easy to agree with such complaints. It can be a constant struggle for educators to find a way to make abstract concepts from science more interesting than ideas from fiction, like the Force or giant robots. But what if there were a way to use people’s fascination with pop culture as a tool for education? What if there were a way to use pop culture to make science relatable and accessible? What if there were a way to use pop culture to make scientists and educators more approachable? That is where the Cosplay for Science Initiative comes in.
The Cosplay for Science I
by Amy P. Jones1
Calcareous nannofossils — words that are, perhaps, unfamiliar to you. You might never have stumbled upon them before … So what are they? They are the fossil remains of coccolithophores: single-celled marine algae from the phylum Haptophyta and division Prymnesiophyceae. They exist in great abundance around the world in the oceans, and have done for over 200 million years. They are also known as the grass of the sea, and are regarded as one of the most important phytoplankton groups in the oceans owing to their relationship with the carbon cycle. They provide valuable proxies to help us understand conditions throughout geological history, because their evolution shows consistent and resilient patterns.
Nannofossils are composed of calcium carbonate, also
by Maggie R. Limbeck*1
The oceans of the Palaeozoic era (541 million to 252 million years ago) were full of animals that we are familiar with, such as fish, snails, and coral, but also included many organisms that look almost nothing like their living relatives. The further back in time we go, for instance to the Cambrian and Ordovician periods (541 million to 444 million years ago), the greater the difference in body plans, or morphologies, compared to modern species. Echinoderms are an excellent example of this — living members of the group, such as starfish and sea urchins, are easily recognizable, but many of their extinct, fossilized relatives from hundreds of millions of years ago look very different. Understanding these different body forms is important to palaeontol
by Emma Dunne*1
Life on Earth is incredibly diverse. More than 1.7 million species have already been described and estimates suggest that there could be as many as 9 million in total. But exactly how this rich biodiversity has developed over the last 542 million years since the Cambrian remains the subject of debate amongst palaeontologists. Did biodiversity increase steadily from one geological period to the next, or did it wax and wane without any overall direction? These questions are crucial in a modern context: today, we are flooded with urgent reports on the state of biodiversity worldwide, with many scientists stating that we are in the middle of a biodiversity crisis driven by human impact, leading to what is being called the sixth mass extinction. To understand and
by Jennifer E. Bauer*1
The ancient seas of the Palaeozoic era (541 million to 252 million years ago) teemed with unusual creatures that would be almost unrecognizable to us today. Although these animals look very peculiar, they often have living relatives that we are more familiar with. Consider echinoderms, such as sea stars and sea urchins: these marine animals can be recognized easily by scientists and the general public alike due to their distinctive five-fold symmetry and often vibrant colours. However, the Palaeozoic fossil record of echinoderms includes a wide range of forms that are radically different from living species. Indeed, there are only 5 major living groups of echinoderms, but about 20 extinct groups known only from the Palaeozoic. This means that the foss
by Thomas Clements*1
What are coleoids?
The coleoid cephalopods (Fig. 1), squids, cuttlefish and octopuses2, are an extremely diverse group of molluscs that inhabits every ocean on the planet. Ranging from the tiny but highly venomous blue-ringed octopus (Hapalochlaena) to the largest invertebrates on the planet, the giant and colossal squids (Architeuthis and Mesonychoteuthis respectively), coleoids are the dominant cephalopods in modern oceans. For humans, they are a vital dietary and economic resource and have an important role in our culture. Cephalopods have intrigued and been revered by humans from ancient times and, more recently, during the nineteenth and twentieth centuries, they became part of pop-culture. Stories of gargantuan poulpes attacking the submarine ‘Nautilus’ in Jule
by Mark T. Young*1, Sven Sachs2 & Pascal Abel3
To most people, crocodilians are large-bodied carnivores that have been unchanged since the age of the dinosaurs. However, during their 230 million-year history, modern crocodilians and their extinct relatives evolved a stunning diversity of body plans, with many looking very different from those alive today (crocodiles, alligators, caimans and gharials).
The first crocodylomorphs (the term used for living crocs and various fossil groups) are known from the Late Triassic Period, approximately 235 million to 237 million years ago. These animals lived on land and looked much more like a greyhound than a crocodile, with long legs and a skull that was deep like that of a meat-eating dinosaur, rather than flattened like that
by Andrew Cuff*1
One of the biggest challenges palaeontologists face is how to reconstruct whole animals from their fossils. Most fossil remains are just bones, so how do we go from the bones to the soft tissues? For extinct species, we make deductions by looking at their nearest living relatives. This process is called the extant phylogenetic bracket (EPB).
A good example of using the EPB is in reconstructing dinosaurs. Dinosaurs are alive today as their descendants, birds, but the non-avian dinosaurs we all know and love from Jurassic Park look very different from modern birds. Dinosaurs also have other living relatives: the crocodilians. Along with the dinosaurs and some other extinct groups, these are part of a group called the archosaurs (which means ‘ruling reptile
by Amelia Penny*1
Introduction and background
The ability to build and maintain a skeleton is one of the major innovations in the history of life. During the Cambrian explosion, which began around 540 million years ago, diverse animal (metazoan) skeletons appeared suddenly in the fossil record. This is also when we first see evidence for predation, the ability to move around and most of the animal body plans we would recognize today. The ability to grow a resistant skeleton was a major factor in the evolutionary arms races of the Phanerozoic eon — the time since the Cambrian explosion — and it made possible the dizzying variety of shells, bones and teeth scattered throughout the Phanerozoic fossil record. But the origin of skeletons has a much deeper root, in the Proterozoic eon (2,500 m