Conodont apatite δ18O signatures indicate climatic cooling as a trigger of the Late Devonian mass extinction

Geology

Volumn 30, Issue 8, 2002, Pages 711-714

  Joachimski, Michael M ^a   Buggisch, Werner ^a  

^a UNIVERSITY OF ERLANGEN NUREMBERG   (Germany)

Author keywords

18O 16O; Apatite; Late Devonian; Mass extinction; Paleotemperature

Indexed keywords

PALEOTEMPERATURES;

CARBON DIOXIDE; CLIMATOLOGY; OXYGEN; SURFACE WATERS;

GEOLOGY;

APATITE; BIOSTRATIGRAPHY; DEVONIAN; MASS EXTINCTION; PALEOCLIMATE; PALEOTEMPERATURE; SEA SURFACE TEMPERATURE;

EID: 0036693771     PISSN: 00917613     EISSN: None     Source Type: Journal    
DOI: 10.1130/0091-7613(2002)030<0711:CAOSIC>2.0.CO;2     Document Type: Article

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