Preservation of Organic Carbon in Dolomitized Cambrian Stromatolites and Implications for Microbial Biosignatures in Diagenetically Replaced Carbonate Rock: Supplementary Materials

Published: 24 April 2020| Version 1 | DOI: 10.17632/k57gbw78d9.1
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****Please view the README.txt file for more detailed documentation of data.**** Contact information: Ashley E. Murphy Rutgers University Newark, New Jersey, U.S.A. ashley.murphy@rutgers.edu Dates of data collection: 2017/02 - 2020/01 Geographic location: New Jersey, U.S.A. Funding sources: NASA ASTEP; NASA NAI ENIGMA – Rutgers University. License: CC BY 4.0CC BY 4.0 This directory contains the following supplementary materials: Murphyetal2020_Allentown_SuppMaterials.xlsx: supplement of text and additional figures and tables Table S1: Inductively Coupled Plasma - Optical Emission Spectrometry (ICP-OES) carbonate geochemistry results table Table S2: Electronprobe Microanalysis (EPMA) dolomite spot analyses elemental results Table S3: Carbonate and organic carbon isotopic data and total organic carbon results Table S4a: Raman data from Cluster method including geothermometry Table S4b: Raman data from Gaussian method including geothermometry Figure S1: XRD results in a waterfall plot Figure S2: SEM/EDS results for minor mineral phases Figure S3a: D and G peaks from cluster analysis corresponding to Table S4a Figure S3b: D and G peaks from Gaussian analysis corresponding to Table S4b Figure S4: Raman t-Test results of D and G band variations

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Geochemistry, Raman Spectroscopy, Fossil Preservation, Isotope Geochemistry, Diagenesis, X-Ray Diffraction, Scanning Electron Microscopy-Energy Dispersive X-Ray, Cathodoluminescence, Geothermometry, Amorphous Carbon, Cambrian Period, Carbonate Mineral, Raman Microscopy, Electron Microprobe

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