New insights into the Precambrian fossil record using correlative electron and ion beam microscopy
Notice bibliographique
Résumé
Earth's rock record holds great potential for decoding the origin and early diversification of life on our planet. However, the interpretation of the Precambrian (older than ~541 million years ago) fossil record is fraught with difficulties. These include: the fragmentary nature of the sedimentary rock record with large periods of time unrepresented and certain habitats under‐represented; and the nature of the organisms, being microscopic, morphologically simple and often only subtly different from co‐occurring non‐biological organic material. Distinguishing between true signs of life and abiotic artefacts requires analytical techniques with excellent spatial resolution in two and three dimensions, in order to accurately analyse key features of putative cells such as cell wall ultrastructure, biochemistry, and interaction of cell walls with the minerals that have fossilised them [1]. Likewise, distinguishing different grades of life (for example, simple prokaryotes versus more complex eukaryotes) requires similar techniques, in order to identify putative multi‐cellularity and specific types of cell contents and cell wall architecture. We here demonstrate how a protocol combining focused ion beam (FIB) milling, SEM, TEM and nano‐scale secondary ion mass spectrometry (SIMS) can reveal unprecedented nanometer to micrometer scale details of Precambrian fossilised organisms, providing more robust biosignatures for both prokaryotes and eukaryotes for future studies on Earth or other planets. FIB milling was used to prepare ultrathin (c. 100 nm) wafers from standard geological thin sections for TEM analysis, plus slightly thicker wafers (c. 150‐200 nm) that could be used for both TEM and NanoSIMS analysis. The latter meant that both TEM and NanoSIMS data could be collected from a single candidate microfossil: TEM data included ChemiSTEM elemental mapping of major elements, STEM‐EELS analysis of the bonding and structure of organic material, and electron diffraction to identify mineral phases; NanoSIMS data included targeted analysis of trace elements in organic material (e.g., N, S, P) and in the fossilising mineral phases. Analysis of FIB‐milled wafers counteracts the problems previously associated with surface analysis techniques such as NanoSIMS (i.e. surface contamination and polishing effects). FIB‐milling was also combined with SEM imaging (3D slice and view) in order to obtain accurate 3D visualisations of candidate microfossils. Data will be presented from three geological formations that play an important role in our understanding of the origin and evolution of early life on Earth: 1, The 1878 Ma Gunflint Formation of Canada, containing an iconic suite of diverse microfossils used as a benchmark for high quality preservation of early life in marine environments [2]; 2, The 1000 Ma Torridon Group of northwest Scotland (Fig. 1) that is renowned for exceptional three‐dimensional preservation of both prokaryotes and eukaryotes in phosphate and clay minerals in a terrestrial (lake) setting [3]; 3, The 850 Ma Bitter Springs Formation of central Australia that shows exquisite microfossil preservation (including putative cell contents) in micro‐quartz [4].
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Prédiction distillée sur la base complète
Imitation des enseignantsNi prévalence calibrée, ni vérité terrain. Validation humaine à venir. Apprise à partir de 10 348 étiquettes directes de Codex et de 10 348 étiquettes directes de Gemma. Le mode candidate est l'union des têtes enseignantes seuillées; le consensus est leur intersection. Ces sorties portent le statut machine_predicted_unvalidated et ne sont ni des étiquettes humaines ni des étiquettes directes de modèles de pointe.
Scores Codex et Gemma par catégorie
| Catégorie | Codex | Gemma |
|---|---|---|
| Métarecherche | 0,000 | 0,000 |
| Méta-épidémiologie (sens strict) | 0,001 | 0,000 |
| Méta-épidémiologie (sens large) | 0,001 | 0,000 |
| Bibliométrie | 0,000 | 0,000 |
| Études des sciences et des technologies | 0,001 | 0,001 |
| Communication savante | 0,000 | 0,000 |
| Science ouverte | 0,001 | 0,000 |
| Intégrité de la recherche | 0,000 | 0,001 |
| Charge utile insuffisante (le modèle a refusé de juger) | 0,001 | 0,000 |
Scores machine (provisoires)
Les deux têtes enseignantes du modèle étudiant, lues sur ce travail. Un score ordonne la base pour la relecture; il n'affirme jamais une catégorie, et le statut de validation accompagne chaque rangée tel quel.
Scores de référence d'un modèle non mature (critères de maturité non atteints, 7 itérations). Un score ordonne; il n'affirme jamais une catégorie.
score_only:v0-immature-baseline · tel quel depuis la passe de notation : score_only signifie que le nombre peut ordonner les travaux, et qu'aucune étiquette de catégorie n'en découleClassification
machine, non validéePrédiction automatique; un appel candidat d’une seule tête enseignante, pas un consensus.
Le détail, modèle par modèle et score par score, se trouve en fin de page sous « Comment cette classification a été obtenue ».