Biosignatures of modern and fossil cyanobacteria

• Main Authors: Demoulin, Catherine, Lara, Yannick, François, Camille, Javaux, Emmanuelle
• Format: Conference Object
• Language: English
• Published: 2018
• Subjects: Physical; chemical; mathematical & earth Sciences; Earth sciences & physical geography; Physique; chimie; mathématiques & sciences de la terre; Sciences de la terre & géographie physique; Belcher Islands; Hudson Bay
• Online Access: https://orbi.uliege.be/handle/2268/221672; https://orbi.uliege.be/bitstream/2268/221672/1/Abstract_CDemoulin_COST21-2018.pdf

peer reviewed The Proterozoic is an important eon for the evolution of early life on Earth, and especially for the diversification of cyanobacteria, a major group of photosynthetic microorganisms. In paleontology, much effort and work are devoted to the study of cyanobacteria, due to their key-role in the oxygenation of the atmosphere and oceans during the GOE (Great Oxidation Event, around 2.4 Ga). Moreover, the development of oxygenated ecological niches is one of the factors linked to the diversification of eukaryotes. However, identifying extremely old microfossil structures as cyanobacteria remains often disputed. The oldest fossil cyanobacterium (~ 1.9 Ga) determined so far with certainty is Eoentophysalis belcherensis Hofmann, a microorganism forming mats and colonies in silicified stromatolites from the Belcher Islands, Hudson Bay, Canada [1]. Its identification as a cyanobacterium relies mainly on morphological comparison to a modern cyanobacterium, Entophysalis Ercegović [2]. In this context, our research project, financed by the ERC StG ELiTE, mainly aims at characterizing the biosignatures of Proterozoic cyanobacteria in order to get new insights into the origin and early evolution of cyanobacteria and oxygenic phtosynthesis. Methodologically, we are using optical microscopy, electron microscopy (SEM and TEM) and Raman and FTIR microspectroscopy techniques, applied on modern specimens and microfossils. This approach is expected to test the biological nature of Paleoproterozoic and younger microstructures, to resolve the affinities of possible prokaryotic microfossils and, thus, to assess their taxonomic placement among cyanobacteria.