Low-latitude sea-surface temperatures for the mid-Cretaceous and the evolution of planktic foraminifera: Reply

Geology

Volumn 27, Issue 9, 1999, Pages 858-

  Norris, R D ^a   Wilson, P A ^b  

^a WOODS HOLE OCEANOGRAPHIC INSTITUTION   (United States)

^b UNIVERSITY OF CAMBRIDGE   (United Kingdom)

Author keywords

[No Author keywords available]

Indexed keywords

ALTITUDINAL ZONATION; BIOSTRATIGRAPHY; CRETACEOUS; EVOLUTION; LITERATURE REVIEW; PALEOCEANOGRAPHY; PALEOCENE-EOCENE BOUNDARY; PLANKTONIC FORAMINIFERA; SEA SURFACE TEMPERATURE;

EID: 84871094609     PISSN: 00917613     EISSN: 19432682     Source Type: Journal    
DOI: 10.1130/0091-7613(1999)027<0859:SFEOIA>2.3.CO;2     Document Type: Letter

References (8)

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3. Caron, M., and Homewood, P., 1983, Evolution of early planktonic foraminifers: Marine Micropaleontology, v. 7, p. 435-462.
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7. Premoli Silva, I., and Sliter,W. V., 1995, Cretaceous planktonic foraminiferal biostratigraphy and evolutionary trends from the Bottaccione section, Gubbio, Italy: Palaeontographia Italica, v. 82, p. 1-89.
8. Price, G., Sellwood, B., Corfield, R., Clarke, L., and Cartlidge, J., 1998, Isotopic evidence for palaeotemperatures and depth stratification of Middle Cretaceous planktonic foraminifera from the Pacific Ocean: Geological Magazine, v. 135, p. 183-191.