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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 the 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.
BADAWI, A., SCHMIEDL, G., and HEMLEBEN, C., Impact of late Quaternary environmental changes on deep-sea benthic foraminiferal faunas of the Red Sea.Marine Micropaleontology, v. 58, 2005, p. 1330, 7 figures, 3 tables, 1 appendix." Fluctuations in abundance, diversity and species composition of benthic foraminifera from two sites of the northern and southern Red Sea indicate strong variability of deep-sea ecosystems during the last four glacial to interglacial cycles. In total, five and four different benthic foraminiferal assemblages have been identified in the northern core and southern core, respectively. Comparison with recent faunas from the Red Sea and adjacent oceans allowed the reconstruction of temporal changes in deepwater ventilation, salinity and food availability at the seafloor. . ." (from Abstract).
FILIPSSON, H. L., and NORDBERG, K., Climate variations, an overlooked factor influencing the recent marine environment. An example from Gullmar Fjord, Sweden, illustrated by benthic foraminifera and hydrographic data.Estuaries, v. 27, 2004, p. 867881, 7 figures, 2 tables.". . . We investigated how the benthic environment, in the deepest part of the fjord, has varied during the 20th century, using benthic foraminifera and an extensive history of instrumental hydrographic data. The foraminifera have undergone one major faunal change and two minor modifications during this time. . ." (from Abstract).
FILIPSSON, H. L., NORDBERG, K., and GUSTAFSSON, M., Seasonal study of
18O and
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