Biology subjects

Jordan, S. F.

Publications and source records attributed to Jordan, S. F..

5 recordsLinked to original sources

bioRxiv2026

Protocells reproduce morphological and chemical signatures of early microfossils

Identification of early microfossils relies on morphological and chemical criteria assumed to be unique to life, but whether abiotic microstructures can satisfy these criteria has not been rigorously tested. Hydrothermal environments preserve microfossils but are also efficient geochemical reactors for abiotic reactions. Protocells form in hydrothermal conditions and represent a plausible abiotic analogue to early microfossils. Here we show that protocells form from simple organic molecules in low-temperature, alkaline hydrothermal conditions in the presence of silica and produce spheres, filaments, and lenticular structures that strongly resemble the morphology of purported microfossils in Archaean silica cherts. FTIR spectroscopy provides overlapping chemical signatures across protocells, microorganisms, and geologic microstructures. In addition, the FTIR R3/2 ratio, a chemometric index often used to discriminate domains and determine biogenicity, identifies eight different protocell systems as either bacterial, archaeal, or eukaryotic. These data suggest that protocells preserved in ancient hydrothermal deposits can satisfy current biogenicity criteria, undermining the reliability of interpretations of the early fossil record. As life detection is the primary objective for current space exploration endeavours, robust biogenicity protocols that account for abiotic signatures are essential.

paleontology↗

bioRxiv2025

Peptides at vesicle and mineral prebiotic interfaces

The origin of life likely involved a complex interplay between organic molecules and mineral surfaces, yet the molecular details of these interactions remain poorly understood. Over recent decades, considerable research has focused on the individual roles of key biomolecules - such as RNA, lipids, and proteins - in early abiogenesis. However, this reductionist view offers only a partial picture because the emergence of life likely involved networks of molecular interactions that collectively shaped early functional assemblies. In this study, we examine the ability of peptides - arguably one of the most abundant early polymers - to interact with mineral surfaces and lipid vesicles, prebiotic interfaces and compartments. Using peptide libraries constructed from either prebiotically plausible or contemporary amino acids, we demonstrate that while acidic residues drive peptide binding to mineral surfaces (such as fluorapatite, studied here), the inclusion of arginine - a basic residue that may have been accessible in specific prebiotic environments - synergistically enhances the mobilization of bioavailable phosphate from geological reservoirs. Furthermore, we observe a functional divergence in vesicle interactions: while prebiotic alphabets promote dynamic membrane behaviours such as budding, libraries with late canonical amino acids can help preserve vesicle integrity against salt-induced collapse. Our finding supports the view that interactions with peptides can elicit changes in both prebiotic minerals and vesicles, underscoring the importance of studying these systems collectively.

evolutionary biology↗

bioRxiv2025

Prototaxites was an extinct lineage of multicellular terrestrial eukaryotes

Prototaxites was the first giant organism to live on the terrestrial surface, reaching sizes of 8 metres in the Early Devonian. However, its taxonomic assignment has been debated for over 165 years1-7. Tentative assignments to groups of multicellular algae or land plants1,2,8-11 have been repeatedly ruled out based on anatomy and chemistry5,7,11-16 resulting in two major alternatives: Prototaxites was either a fungus5,6,17-22 or a now entirely extinct lineage 7,16,23. Recent studies have converged on a fungal affinity5-7,17-20,22. Here we test this by contrasting the anatomy and molecular composition of Prototaxites with contemporary fungi from the 407-million-year-old Rhynie chert. We report that Prototaxites taiti was the largest organism in the Rhynie ecosystem and its anatomy was fundamentally distinct from all known extant or extinct fungi. Furthermore, our molecular composition analysis indicates that cell walls of P. taiti include aliphatic, aromatic, and phenolic components most similar to fossilisation products of lignin, but no fossilisation products characteristic of chitin or chitosan, which are diagnostic of all groups of extant and extinct fungi, including those preserved in the Rhynie chert. We therefore conclude that Prototaxites was not a fungus, and instead propose it is best assigned to a now entirely extinct terrestrial lineage.

paleontology↗

bioRxiv2023

Prebiotic membrane structures mimic the morphology of purported early traces of life on Earth

Elucidating the most probable compositions of the first cell membranes prior to the origin of life, within a laboratory setting, requires experiments with organic molecules and chemical conditions representative of those present on the early Earth. As such, the membrane forming molecules used in these experiments are described as prebiotically plausible, i.e., they could have formed through abiotic reactions and be available for membrane formation prior to the emergence of biology. Similarly, the chemical properties of solutions in which these membranes are formed (e.g., pH, temperature, ionic strength) must represent the early Earth environmental conditions under investigation. Here, using a combined confocal and transmission electron microscopy approach, we show that prebiotically plausible organic molecules, in solutions representative of Hadean submarine alkaline hydrothermal vents, form aggregated structures with substantial morphological diversity. The structures hold the potential for use as traces of prebiotic processes in the ancient rock record. In addition, many of the structures are morphologically similar to those which are presented as early microfossils, thus highlighting the limitations of morphological interpretation in these types of studies. Detailed analyses of abiotic organic structures are essential for our understanding of the earliest living organisms on Earth, as well as for our interpretation of any potential biosignatures recovered in the future from extra-terrestrial bodies.

paleontology↗

bioRxiv2021

A prebiotic basis for ATP as the universal energy currency

ATP is universally conserved as the principal energy currency in cells, driving metabolism through phosphorylation and condensation reactions. Such deep conservation suggests that ATP arose at an early stage of biochemical evolution. Yet purine synthesis requires six phosphorylation steps linked to ATP hydrolysis. This autocatalytic requirement for ATP to synthesize ATP implies the need for an earlier prebiotic ATP-equivalent, which could drive protometabolism before purine synthesis. Why this early phosphorylating agent was replaced, and specifically with ATP rather than other nucleotide triphosphates, remains a mystery. Here we show that the deep conservation of ATP reflects its prebiotic chemistry in relation to another universally conserved intermediate, acetyl phosphate, which bridges between thioester and phosphate metabolism by linking acetyl CoA to the substrate-level phosphorylation of ADP. We confirm earlier results showing that acetyl phosphate can phosphorylate ADP to ATP at nearly 20 % yield in water in the presence of Fe3+ ions. We then show that Fe3+ and acetyl phosphate are surprisingly favoured: a panel of other prebiotically relevant ions and minerals did not catalyze ADP phosphorylation; nor did a number of other potentially prebiotic phosphorylating agents. Only carbamoyl phosphate showed some modest phosphorylating activity. Critically, we show that acetyl phosphate does not phosphorylate other nucleotide diphosphates or free pyrophosphate in water. The phosphorylation of ADP monomers seems to be favoured by the interaction between the N6 amino group on the adenine ring with Fe3+ coupled to acetyl phosphate. Our findings suggest that the reason ATP is universally conserved across life is that its formation is chemically favoured in aqueous solution under mild prebiotic conditions.

biochemistry↗