Framboidal pyrite evidence for persistent low oxygen levels in shallow-marine facies of the Nanpanjiang Basin during the Permian-Triassic transition (2018)
Attributed to:
Ecosystem resilience and recovery from the Permo-Triassic crisis
funded by
NERC
Abstract
No abstract provided
Bibliographic Information
Digital Object Identifier: http://dx.doi.org/10.1016/j.palaeo.2018.08.012
Publication URI: http://dx.doi.org/10.1016/j.palaeo.2018.08.012
Type: Journal Article/Review
Parent Publication: Palaeogeography, Palaeoclimatology, Palaeoecology
ISSN: 0031-0182