Oxygen isotopes from conodont apatite of the midcontinent, US: Implications for Late Ordovician climate evolution

Palaeogeography, Palaeoclimatology, Palaeoecology

Volumn 404, Issue , 2014, Pages 57-66

  Quinton, Page C ^a   MacLeod, Kenneth G ^a  

^a UNIVERSITY OF MISSOURI   (United States)

Author keywords

Conodonts; Late ordovician; Late ordovician glaciation; Oxygen isotopes; Paleoclimatology; Paleothermometry

Indexed keywords

APATITE; CLIMATE VARIATION; CONODONT; GLACIATION; ICE SHEET; MASS EXTINCTION; ORDOVICIAN; OXYGEN ISOTOPE; PALEOCLIMATE; PALEOTEMPERATURE; PHOSPHATE;

MIDCONTINENT; UNITED STATES;

EID: 84907422309     PISSN: 00310182     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.palaeo.2014.03.036     Document Type: Article

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