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

****Please view the README4.txt file for more detailed documentation of data.****
Contact information:
Ashley E. Murphy
Rutgers University
Newark, New Jersey, U.S.A.
[e-mail]
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:

Table S1: Carbonate and organic carbon isotopic data and total organic carbon results
Table S2: Electronprobe Microanalysis (EPMA) dolomite spot analyses elemental results
Table S3a: Raman data from Cluster method
Table S3b: Raman data from Gaussian method
Table S3c: Raman data from Cluster method post deconvolution (Fit F) with thermometry
Table S3d: Raman data from Cluster method post deconvolution (Fit E) with thermometry
Figure S1a: Raman t-Test results (pre-deconvolution)
Figure S1b: Raman t-Test results (post-deconvolution)
Figure S2: Raman t-Test results for thermometry
Figure S3: XRD results in a waterfall plot
Figure S4: nonplanar microspar dolomite texture
Figure S5: Sample B14 microfractures infilled with saddle dolomite
Figure S6: SEM/EDS results for minor mineral phases
Figure S7: SEM/EDS results for dark black stromatolitic laminae
Figure S8a: D and G peaks from cluster analysis corresponding to Table S3a
Figure S8b: D and G peaks from Gaussian analysis corresponding to Table S3b