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      Molecular fingerprints resolve affinities of Rhynie chert organic fossils

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          Abstract

          The affinities of extinct organisms are often difficult to resolve using morphological data alone. Chemical analysis of carbonaceous specimens can complement traditional approaches, but the search for taxon-specific signals in ancient, thermally altered organic matter is challenging and controversial, partly because suitable positive controls are lacking. Here, we show that non-destructive Fourier Transform Infrared Spectroscopy (FTIR) resolves in-situ molecular fingerprints in the famous 407 Ma Rhynie chert fossil assemblage of Aberdeenshire, Scotland, an important early terrestrial Lagerstätte. Remarkably, unsupervised clustering methods (principal components analysis and K-mean) separate the fossil spectra naturally into eukaryotes and prokaryotes (cyanobacteria). Additional multivariate statistics and machine-learning approaches also differentiate prokaryotes from eukaryotes, and discriminate eukaryotic tissue types, despite the overwhelming influence of silica. We find that these methods can clarify the affinities of morphologically ambiguous taxa; in the Rhynie chert for example, we show that the problematic “nematophytes” have a plant-like composition. Overall, we demonstrate that the famously exquisite preservation of cells, tissues and organisms in the Rhynie chert accompanies similarly impressive preservation of molecular information. These results provide a compelling positive control that validates the use of infrared spectroscopy to investigate the affinity of organic fossils in chert.

          Abstract

          It can be challenging to identify extinct organisms with morphology alone. Here, the authors use non-destructive Fourier Transform Infrared Spectroscopy to determine the molecular fingerprints of eukaryotes and prokaryotes from the 407 Ma Rhynie chert fossil assemblage of Aberdeenshire, Scotland.

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          Kerogen origin, evolution and structure

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            Early fungi from the Proterozoic era in Arctic Canada

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              Analyses of extracellular carbohydrates in oomycetes unveil the existence of three different cell wall types.

              Some of the most devastating plant and animal pathogens belong to the oomycete class. The cell walls of these microorganisms represent an excellent target for disease control, but their carbohydrate composition is elusive. We have undertaken a detailed cell wall analysis in 10 species from 2 major oomycete orders, the Peronosporales and the Saprolegniales, thereby unveiling the existence of 3 clearly different cell wall types: type I is devoid of N-acetylglucosamine (GlcNAc) but contains glucuronic acid and mannose; type II contains up to 5% GlcNAc and residues indicative of cross-links between cellulose and 1,3-β-glucans; type III is characterized by the highest GlcNAc content (>5%) and the occurrence of unusual carbohydrates that consist of 1,6-linked GlcNAc residues. These 3 cell wall types are also distinguishable by their cellulose content and the fine structure of their 1,3-β-glucans. We propose a cell wall paradigm for oomycetes that can serve as a basis for the establishment of cell wall architectural models and the further identification of cell wall subtypes. This paradigm is complementary to morphological and molecular criteria for taxonomic grouping and provides useful information for unraveling poorly understood cell wall carbohydrate biosynthetic pathways through the identification and characterization of the corresponding enzymes.
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                Author and article information

                Contributors
                v1cloron@ed.ac.uk
                sean.mcmahon@ed.ac.uk
                Journal
                Nat Commun
                Nat Commun
                Nature Communications
                Nature Publishing Group UK (London )
                2041-1723
                13 March 2023
                13 March 2023
                2023
                : 14
                : 1387
                Affiliations
                [1 ]GRID grid.4305.2, ISNI 0000 0004 1936 7988, UK Centre for Astrobiology, School of Physics and Astronomy, , University of Edinburgh, ; Edinburgh, UK
                [2 ]GRID grid.7886.1, ISNI 0000 0001 0768 2743, UCD School of Earth Sciences, , University College Dublin, ; Dublin, Ireland
                [3 ]GRID grid.4305.2, ISNI 0000 0004 1936 7988, EastCHEM and School of Chemistry, , University of Edinburgh, ; Edinburgh, UK
                [4 ]GRID grid.422302.5, ISNI 0000 0001 0943 6159, Natural Sciences Department, , National Museums Scotland, ; Edinburgh, UK
                [5 ]GRID grid.4305.2, ISNI 0000 0004 1936 7988, School of Geosciences, , University of Edinburgh, ; Edinburgh, UK
                Author information
                http://orcid.org/0000-0002-3317-4029
                http://orcid.org/0000-0003-2316-5660
                http://orcid.org/0000-0003-4408-4640
                http://orcid.org/0000-0001-8589-2041
                Article
                37047
                10.1038/s41467-023-37047-1
                10011563
                36914650
                b790d703-7d42-4265-bf86-e3b8c34e4d55
                © The Author(s) 2023

                Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.

                History
                : 12 July 2022
                : 1 March 2023
                Funding
                Funded by: FundRef https://doi.org/10.13039/501100000288, Royal Society;
                Funded by: FundRef https://doi.org/10.13039/501100010978, Wallonie-Bruxelles International (WBI);
                Categories
                Article
                Custom metadata
                © The Author(s) 2023

                Uncategorized
                palaeontology,biogeochemistry,eukaryote,prokaryote
                Uncategorized
                palaeontology, biogeochemistry, eukaryote, prokaryote

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