ANOM Lab

From August 25^th to 31^st, Prof. Allison Daley, Dr. Damien Pas, Dr. Harriet B.B. Drage, PhD candidates Gaëtan Potin, and Valentin Jamart participated in the IGC 2024 meeting in Busan, South Korea. During the meeting, members of the ANOM Lab had the opportunity to present their research (through talks and/or posters), establish new connections, and experience the culture and cuisine of South Korea. Additionally, Prof. Allison C. Daley, Dr. Harriet B. Drage, and PhD candidates Gaëtan J.M. Potin and Valentin Jamart represented Switzerland at the IUGS council, where their responsibilities included participating in the election of the new IUGS committee and voting for the country that will host the next IGC meeting in 2028.

After the congress, A.C. Daley, H.B. Drage, G.J.M. Potin, and V. Jamart participated in the field trip, ‘The New Perspective of the Cambro-Ordovician of the Taebaksan Basin, Korea.’ This field trip gave ANOM Lab members the opportunity to explore the Lower Paleozoic geological wonders of South Korea.

From July 08^th to July 10^th, Dr. Damien Pas and Valentin Jamart (PhD candidate) participated in the Cyclostratigraphy Intercomparison Project 2.0 workshop in Brussels, Belgium. During the workshop, discussions and debates took place with cyclostratigraphers at all levels (from PhD students to senior professors) and from various universities across Europe, China, and the USA. Additionally, three case studies were analyzed to test the replicability of cyclostratigraphic studies.

Nora Corthésy published her first article in the Swiss Journal of Palaeontology this summer. The project was conducted with the invaluable help of Camille Thomas from the University of Bern, along with Farid Saleh, Allison Daley, and Jonathan Antcliffe. The paper explores how different clays influence bacterial community composition during shrimp decay and how this affects tissue preservation. Check it out!

Corthésy, N., Saleh, F., Thomas, C., Antcliffe, J. B., & Daley, A. C. 2024. The effects of clays on bacterial community composition during arthropod decay. Swiss journal of palaeontology, 143(1), 26.

This year, the ANOM Lab participated in the University’s open days, Les Mystères de l’Unil, by presenting an interactive workshop for children and families. Organized by Dr. Farid Saleh, the workshop aimed to introduce Ordovician ecosystems in a fun and engaging way. Children were tasked with identifying fossils on a large reconstruction and comparing the differences and similarities between fossils and modern animals to better understand their evolution and fossilization.

Modern scorpions, spiders and horseshoe crabs belong to the vast lineage of arthropods, which appeared on Earth nearly 540 million years ago. More precisely, they belong to a subphylum that includes organisms equipped with pincers used notably for biting, grasping prey, or injecting venom –the chelicerae, hence their name chelicerates. But what are the ancestors of this very specific group? This question has puzzled paleontologists ever since the study of ancient fossils began. It has been impossible to identify with certainty any form among early arthropods that shared enough similarities with modern species to be considered ancestors. The mystery was further compounded by the lack of fossils available for the key period between -505 and -430 million years ago, which would have facilitated genealogical investigation.

In a chapter of Lorenzo Lustri’s PhD thesis, published today in Nature Communications, we identify the synziphosurine from the ~480-million-year-old Fezouata Shale in Morocco as a pivotal fossil that fills the gap between modern chelicerates and species from the Cambrian period (505 million years ago). Fossils from the Fezouata Shale, including that synziphosurine, were discovered in the early 2000s. Many fossils have already undergone extensive analysis, yet despite being one of the most most abundant fossil in the deposit, this one had never been described before. Measuring between 5 and 10 millimeters in size, it has been named Setapedites abundantis. This animal makes it possible, for the first time, to trace the entire lineage of chelicerates, from the appearance of the earliest arthropods to modern spiders, scorpions and horseshoe crabs.

To obtain these results Lorenzo studied more than a hundred fossils, a couple of which were imaged using synchrotron X-ray computed tomography (CT) scanning at the TOMCAT beamline of the Swiss Light Source (Paul Scherrer Institut, Villigen, Switzerland) to reconstruct their anatomy in detail and in three dimensions.

By combining a detailed anatomical description of Setapedites abundantis with comparisons to numerous fossil and extant chelicerates as well as Cambrian arthropods, and using robust phylogenetic methods, we establish a new monophyletic clade at the base of Chelicerata, which also includes the Silurian synziphosurines Dibasterium and Offacolus. This new clade links Chelicerata with the Cambrian arthropod Habellia optata from the Burgess Shale, clarifying the origin of chelicerates and particularly the evolution of chelicerate gill opercula, which are shown to have originated from Habelia-like thoracic exopods.

Furthermore, we also identified potential homologies with the problematic vicissicaudatan arthropods, suggesting that Setapedites abundantis might have more secrets to reveal. This could lead to a deeper understanding of the early evolution of the chelicerate group and its relationships with other arthropods whose affinities remain highly debated.

Reference: Lustri L., Gueriau P. & Daley A.C. 2024. Lower Ordovician synziphosurine reveals early euchelicerate diversity and evolution. Nature Communications 15, 3808. Find the article (Open Access) here