Abrupt global-ocean anoxia during the Late Ordovician-early Silurian detected using uranium isotopes of marine carbonates. (2018)
Attributed to:
Ion Micro-Probe Facility (IMF)
funded by
NERC
Abstract
No abstract provided
Bibliographic Information
Digital Object Identifier: http://dx.doi.org/10.1073/pnas.1802438115
PubMed Identifier: 29784792
Publication URI: http://europepmc.org/abstract/MED/29784792
Type: Journal Article/Review
Volume: 115
Parent Publication: Proceedings of the National Academy of Sciences of the United States of America
Issue: 23
ISSN: 0027-8424