Isotope data from Cretaceous chalks and foraminifera: Environmental or diagenetic signals?

Geology

Volumn 25, Issue 8, 1997, Pages 691-694

  Mitchell, Simon F ^a  

^a UNIVERSITY OF THE WEST INDIES   (Jamaica)

Author keywords

[No Author keywords available]

Indexed keywords

ISOTOPES; SCANNING ELECTRON MICROSCOPY; SEDIMENTS; STRATIGRAPHY; CEMENTS;

CEMENT SAMPLE; CENOMANIAN-TURONIAN; CRETACEOUS CHALK; ISOTOPE ANALYSIS; ISOTOPE DATA; MIXING LINES; SIMILAR DATUM; THIN SECTION; MICROFOSSILS;

CEMENTS; SEDIMENTS;

CENOMANIAN-TURONIAN BOUNDARY; CHALK; CRETACEOUS; DIAGENESIS; FORAMINIFERA; ISOTOPIC ANALYSIS; MICROFOSSIL; PALEOENVIRONMENT; SCANNING ELECTRON MICROSCOPY; CEMENT; SEM;

DOVER [KENT]; ENGLAND; KENT; UNITED KINGDOM; DOVER; UK;

EID: 0031458515     PISSN: 00917613     EISSN: None     Source Type: Journal    
DOI: 10.1130/0091-7613(1997)025<0691:IDFCCA>2.3.CO;2     Document Type: Article

References (1)

1. Ditchfieid, P. W., and Marshall, J. D., 1989, Isotopic variation in rhythmically bedded chalks: Paleo-temperature variation in the Upper Cretaceous: Geology, v. 17, p. 842-845.