Ordovician Trilobite Development and Moulting – New Paper in Paleobiology

This week: two members of the ANOM Lab – Harriet Drage and Lukáš Laibl – published a new paper in the journal Paleobiology. The paper describes the development of an Ordovician trilobite Dalmanitina from their tiny babies to mature adults. Dalmanitina is an basal member of a successful trilobite group called Phacopina. Adult phacopines are recognised by their fused facial sutures, which in other trilobites are non-fused and used during the moulting process. However, because of this fusion, adult phacopines unusually had to also moult their heads to be able to escape their old exoskeleton. Baby phacopines, still moulted like “normal” trilobites because they retained unfused facial sutures. The fusion of facial sutures between the baby and adult modes usually occurred at a very particular time during the development of most Phacopina. However, in this new paper, the authors show that Dalmanitina did not obey this rule, with facial suture fusion occurring variably in ontogeny. This is exciting because it confirms the hypothesis that basal members of major clades have less contrained developmental programs.

 

Read more about the research here:

Drage, Laibl & Budil – Postembryonic development of Dalmanitina, and the evolution of facial suture fusion in Phacopina.

 

It’s synchrotron week!

Members of the ANOM Lab are spending this week at the Soleil Synchrotron (near Paris. Postdoc Pierre Gueriau is leading the project, which aims to tease out new anatomical details from Fezouata Biota fossils using the Synchrotron for x-ray fluorescence (XRF) elemental mapping. Francesc Perez Peris, Lorenzo Lustri, Lukas Laibl and Farid Saleh are all on site lending a hand with the research. Synchrotron – it’s not just for 3D tomography anymore!

 

 

ANOM Lab is growing!

A big welcome goes out to our new lab members, who joined us in Lausanne during the last few months. Pierre Gueriau is our new postdoctoral researcher, working on Fezouata Biota bivalved arthropods and developing new imaging and analytical techniques for looking at exceptionally preserved fossils. Frances Pérez Peris and Lorenzo Lustri are both starting 4-year PhDs here. Fran will be working on Ordovician trilobites, and Lorenzo will be studying fossil horseshoe crabs. We look forward to working with you!

Fieldwork at the Emu Bay Shale

In April, Harriet Drage from the Anom Lab joined the team from the South Australian Museum, Adelaide, Australia, for their field season at the Emu Bay Shale Konservat-Lagerstätte on Kangaroo Island. This is one of the most significant early Cambrian (~514 million years ago) fossil localities in the world, which preserves soft tissue and rare species but also a high diversity and abundance of invertebrate fossils. The crew spent 9 days splitting rocks in a private quarry, collecting important material to expand the Museum’s research collections.
Harriet works on the trilobites from the Emu Bay Shale, in particular looking at their exoskeleton moulting behaviour. She managed to collect data from over 200 trilobite individuals in the field, and the same again from the amazing collections at the South Australian Museum. For most of the time temperatures in the quarry soared to over 35 degrees, but despite the heat they had a fun and profitable trip!
Harriet’s field work was funded by a research grant from the King’s College London Menzies Centre for Australian Studies.

Arthropod evolution & the Cambrian Explosion – Perspective in PNAS

This week in PNAS, the ANOM Lab (Daley, Antcliffe, Drage & Pates) published a Perspective that examines multiple sources of fossil data – including exceptionally preserved BST-type fossils, shelly fossils, microfosssils and trace fossil – to describe the timing of the origin and evolution of euarthropods. By comparing the modes of preservation between the Cambrian and Precambrian, we concluded that there is no evidence for euarthropods in the Precambrian. Using this comprehensive approach, we suggest that the first appearance of euarthropods was between 537 and 550 million years ago. There was no deep Precambrian root to the origin of euarthropods, and instead this evolution played out during the first 30 to 40 million years of the Cambrian. Read about it here:

 

Original PNAS article:

Daley et al. 2018 Euarthropod evolution and the Cambrian Explosion

 

News coverage:

Mail Online article

Newsweek

PhysOrg article

Xinhua Net News

Science Daily

Eurasia Review

 

Radio interview with Allison Daley for CQFD, Radio Télévision Suisse: