This work is a part of the PhD of the first author, developed at Universidade Federal do Rio Grande do Sul (UFRGS) and University of Aberdeen (UoA). The authors gratefully acknowledge support from Shell Brasil through the “BG05: UoA-UFRGS-SWB Sedimentary Systems” project at UFRGS and the strategic importance of the support given by ANP through the R&D levy regulation. BGS and LAMIR staffs are also acknowledged for assisting with stable isotope analysis. We also would like to tank Dr. Duncan McIlroy for all his help during the field work, and Dr. Marc Laflamme, Dr. Pedro Jose Marenco and an anonymous reviewer for their help in improving the manuscript.Peer reviewedPostprin
The lower part of the Martin Point section (~ 110 m - rhythmites) spans the uppermost Shallow Bay a...
The lower part of the Martin Point section (~ 110 m - rhythmites) spans the uppermost Shallow Bay a...
The late Cambrian witnessed one of the largest positive carbon isotope (δ13C) excursions of the Phan...
In many basins, Upper Cambrian carbonate successions display intervals with a positive carbon isotop...
In many basins, Upper Cambrian carbonate successions display intervals with a positive carbon isotop...
Geochemical models have suggested that the late Cambrian was characterized by a greenhouse climate w...
The Steptoean Positive Carbon Isotope Excursion (SPICE) of earliest late Cambrian (Furongian) age is...
[ACCESS RESTRICTED TO THE UNIVERSITY OF MISSOURI AT REQUEST OF AUTHOR.] Several positive carbon isot...
© The Author(s), 2015. This is the author's version of the work and is distributed under the terms o...
This study illustrates the usefulness of carbon isotopes in stratigraphic interpretations of poorly ...
The marine carbon isotope record (δ13C) used for chemostratigraphy and reconstruction of carbon cycl...
The marine carbon isotope record (δ13C) used for chemostratigraphy and reconstruction of carbon cycl...
The marine carbon isotope record (δ13C) used for chemostratigraphy and reconstruction of carbon cycl...
The Steptoean Positive Isotopic Carbon Excursion (SPICE) is a large (≥4‰ shift) positive carbon isot...
The marine carbon isotope record (δ13C) used for chemostratigraphy and reconstruction of carbon cycl...
The lower part of the Martin Point section (~ 110 m - rhythmites) spans the uppermost Shallow Bay a...
The lower part of the Martin Point section (~ 110 m - rhythmites) spans the uppermost Shallow Bay a...
The late Cambrian witnessed one of the largest positive carbon isotope (δ13C) excursions of the Phan...
In many basins, Upper Cambrian carbonate successions display intervals with a positive carbon isotop...
In many basins, Upper Cambrian carbonate successions display intervals with a positive carbon isotop...
Geochemical models have suggested that the late Cambrian was characterized by a greenhouse climate w...
The Steptoean Positive Carbon Isotope Excursion (SPICE) of earliest late Cambrian (Furongian) age is...
[ACCESS RESTRICTED TO THE UNIVERSITY OF MISSOURI AT REQUEST OF AUTHOR.] Several positive carbon isot...
© The Author(s), 2015. This is the author's version of the work and is distributed under the terms o...
This study illustrates the usefulness of carbon isotopes in stratigraphic interpretations of poorly ...
The marine carbon isotope record (δ13C) used for chemostratigraphy and reconstruction of carbon cycl...
The marine carbon isotope record (δ13C) used for chemostratigraphy and reconstruction of carbon cycl...
The marine carbon isotope record (δ13C) used for chemostratigraphy and reconstruction of carbon cycl...
The Steptoean Positive Isotopic Carbon Excursion (SPICE) is a large (≥4‰ shift) positive carbon isot...
The marine carbon isotope record (δ13C) used for chemostratigraphy and reconstruction of carbon cycl...
The lower part of the Martin Point section (~ 110 m - rhythmites) spans the uppermost Shallow Bay a...
The lower part of the Martin Point section (~ 110 m - rhythmites) spans the uppermost Shallow Bay a...
The late Cambrian witnessed one of the largest positive carbon isotope (δ13C) excursions of the Phan...