Quick Search:    advanced search

GSW Home   GeoRef Home   My GSW Alerts   Contact GSW   About GSW   Journals List   Help

This Article Full Text Full Text (PDF) Submit a response Alert me when this article is cited Alert me when eLetters are posted Alert me if a correction is posted Services Email this article to a friend Similar articles in this journal Alert me to new issues of the journal Download to citation manager Citing Articles Citing Articles via Google Scholar Google Scholar Articles by Jett, J. A. Search for Related Content GeoRef GeoRef Citation

RECENT LITERATURE ON FORAMINIFERA

Department of Paleobiology, MRC-121, P.O. Box 37012, 10th and Constitution Ave., NW Washington, DC 20013-7012

The first 20% of the full text of this article appears below.

Below are given some of the more recent works on foraminifera. To have a publication included in this section, please send a reprint to address given at the end of this section. All reprints will be incorporated into the Todd Library of Foraminiferal Research at the National Museum of Natural History in Washington, D. C., for the use of the scientific community.

HAYWARD, B. W., Foraminifera-based estimates of paleobathymetry using Modern Analogue Technique, and the subsidence history of the early Miocene Waitemata Basin. —New Zealand Journal of Geology and Geophysics, v. 47, 2004, p. 749–767, 8 figures, 3 tables, 2 appendices. —"Cluster and Canonical Correspondence Analyses were used to group 52 early Miocene (Waitemata Group) benthic foraminiferal faunas into eight associations and relate them to proxies for paleobathymetry and bottomwater energy. Modem Analogue Technique (MAT) was used to estimate the paleodepth of each fossil fauna by comparing their generic composition with 371 modem New Zealand faunas. . ." (from Abstract).

HAYWARD, B. W., GRENFELL, H. R., NICHOLSON, K., PARKER, R., WILMHURST, J., HORROCKS, M., SWALES, A., and SABAA, A. T., Foraminiferal record of human impact on intertidal estuarine environments in New Zealand’s largest city. —Marine Micropaleontology, v. 53, 2004, p. 37–66, 13 figures, 4 tables, 2 appendices. —"Fossil foraminiferal faunas were studied in four, short, late Holocene cores (two localities) from the low tidal, estuarine fringes of the Waitemata Harbour, which is surrounded by New Zealand’s largest city, Auckland. All cores record similar major changes in their fossil content since the arrival of humans (ca. 1300 AD), with faunal changes continuing through to the 1970s. . ." (from Abstract).

HAYWARD, B. W., GRENFELL, H. R., SABAA, . . . [Full Text of this Article]