An integrated study (geochemistry, stable oxygen and carbon isotopes, nannofossils, planktonic foraminifera, inoceramid bivalves, ammonites and crinoids) of the Waxahachie Dam Spillway section, north Texas: a possible boundary stratotype for the base of the Campanian Stage

Cretaceous Research

Volumn 29, Issue 1, 2008, Pages 131-167

  Gale, Andrew S ^a   Hancock, Jake M ^g   Kennedy, W James ^b   Petrizzo, Maria Rose ^c   Lees, Jacqueline A ^d   Walaszczyk, Ireneusz ^e   Wray, David S ^f  

^a UNIVERSITY OF PORTSMOUTH   (United Kingdom)

^b UNIVERSITY OF OXFORD   (United Kingdom)

^c UNIVERSITY OF MILAN   (Italy)

^d UNIVERSITY COLLEGE LONDON   (United Kingdom)

^e UNIVERSITY OF WARSAW   (Poland)

^f UNIVERSITY OF GREENWICH   (United Kingdom)

^g NONE

Author keywords

Campanian; Foraminifera; Geochemistry; Inoceramids; Isotopes; Nannofossils

Indexed keywords

AMMONITE; BIOMARKER; BIOSTRATIGRAPHY; BIVALVE; CAMPANIAN; CARBON ISOTOPE; ECHINODERM; GEOCHEMISTRY; MARINE SEDIMENT; NANOFOSSIL; OXYGEN ISOTOPE; PLANKTONIC FORAMINIFERA; SEQUENCE STRATIGRAPHY; SPILLWAY; STABLE ISOTOPE; STRATOTYPE;

ELLIS COUNTY [TEXAS]; NORTH AMERICA; TEXAS; UNITED STATES; WAXAHACHIE LAKE;

BIVALVIA; CRINOIDEA; FORAMINIFERA; INOCERAMIDAE; PELMATOZOA;

EID: 39249085191     PISSN: 01956671     EISSN: 1095998X     Source Type: Journal    
DOI: 10.1016/j.cretres.2007.04.006     Document Type: Article

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