Organic‐walled microfossils from the Ediacaran–Cambrian boundary stratotype section, Chapel Island and Random formations, Burin Peninsula, Newfoundland, Canada: Global correlation and significance for the evolution of early complex ecosystems-Reference-Cited by-同舟云学术

Organic‐walled microfossils from the Ediacaran–Cambrian boundary stratotype section, Chapel Island and Random formations, Burin Peninsula, Newfoundland, Canada: Global correlation and significance for the evolution of early complex ecosystems

Published:2017-09-15 Issue:5 Volume:53 Page:1728-1742
ISSN:0072-1050
Container-title:Geological Journal
language:en
Short-container-title:Geological Journal

Author:

Palacios Teodoro¹^ORCID,Jensen Sören¹,Barr Sandra M.²,White Chris E.³,Myrow Paul M.⁴

Affiliation:

1. Área de Paleontología, Facultad de Ciencias Universidad de Extremadura Badajoz Spain

2. Department of Earth & Environmental Science Acadia University Wolfville Nova Scotia Canada

3. Nova Scotia Department of Natural Resources Halifax Nova Scotia Canada

4. Department of Geology Colorado College Colorado Springs Colorado USA

Funder

Ministerio de Ciencia e Innovación

Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada

Publisher

Wiley

Subject

Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/gj.2998

Reference63 articles.

1. Lowermost Cambrian acritarchs from the Yanjiahe Formation, South China: implication for defining the base of the Cambrian in the Yangtze Platform

2. The Random Formation of southeastern Newfoundland; a discussion aimed at establishing its age and relationship to bounding formations

3. Proposed reassessment of the Cambrian GSSP

4. The oldest sequence of skeletal fossils in the Lower Cambrian of southeastern Newfoundland

5. Oxygen and carbon isotope stratigraphy of early Cambrian carbonates in southeastern Newfoundland and England

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