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Randolph De La Garza

I am a palaeontology Ph.D. student that started as of January 2018. My primary research focus is molecular palaeontology, an emerging interdisciplinary field of geobiology that that incorporate the principles of molecular biology and analytical chemistry with palaeontology. Over the last few decades, the discovery of ancient organic compounds such as melanin pigments and proteins in multimillion-year-old fossilized tissues of various organisms have spurred much interest in the palaeontological community. These biomolecules, although at times controversial, are a surprise due to the readily labile nature of the organic materials that produced by organisms. However, as increasing evidence suggest that a variety of geo- and biochemical pathways are responsible for the preservation of these biological materials, along with this came the realization of their potential to divulge crucial information about the biology of long extinct animals.

 

The aim of my dissertation is to assess the preservation of biomolecules within the fossilized soft tissues of vertebrates using an integrated experimental approach of microscopy (SEM, TEM, conventional microscopes), immunostaining, mass spectrometry (ToF-SIMS), and spectroscopy (FTIR) methods, with a particular emphasis on integumentary (skin) tissues of marine reptiles. Fossilized skin is second to bone in terms of the most commonly fossilized tissue in the geological record and is an incredibly versatile organ that is in constant flux with organism’s environment. As a result, this organ has evolved a variety of appendages (e.g. scales, hair, and feathers) that integrate degradation-resistant biomolecules such as keratin (a tough, waterproof skin protein) and melanin (a biochrome pigment that give animals colouration). Detection of these biopolymers in fossils would have possible implications on behavioural biology, ecology, physiology, and evolutionary history of ancient reptiles. I currently work with a Palaeogene (Eocene, 54-million-year-old) sea turtle from the Fur Formation in Denmark and a Jurassic ichthyosaur from the Posidonia Shale, Germany. Both specimens are extraordinarily preserved with skin residues, and have come from well-known lagersätten beds that previously yielded other spectacular specimens with cellular, sub-cellular, and biomolecule constituents.

Advisor: Johan Lindgren

Co-advisor: Mats Eriksson

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E-mail: randolph [dot] de_la_garza [at] geol [dot] lu [dot] se

Doctoral student

Lithosphere and Biosphere Science

Sölvegatan 12, Lund

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