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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.

BARTELS-JONSDOTTIR, H. B., KNUDSEN, K. L., ABRANTES, F., LEBREIRO, S., and EIRIKSSON, J., Climate variability during the last 2000 years in the Tagus Prodelta, western Iberian Margin: Benthic foraminifera and stable isotopes. —Marine Micropaleontology, v. 59, 2006, p. 83–103, 10 figures, 4 tables, 1 appendix. —"A high resolution sedimentary sequence recovered in the Tagus Prodelta has been studied in order to reconstruct paleoenvironmental conditions. . . Benthic foraminiferal assemblages as well as stable isotopic composition of the benthic foraminifera Uvigerina sp. were investigated. Considerable environmental fluctuations are indicated by all these proxies. . ." (from Abstract).

CORNELIUS, N. and GOODAY, A. J., ‘Live’ (stained) deep-sea benthic foraminiferans in the western Weddell Sea: trends in abundance, diversity and taxonomic composition along a depth transect. —Deep-Sea Research II, v. 51, 2004, p. 1571–1602, 7 Figures, 7 tables, 1 Appendix. —". . . Many of the Weddell Sea species are typical bathyal and abyssal forms well known from the North Atlantic and elsewhere. The phytodetrital assemblages are strikingly similar to those reported from abyssal sites in the North Atlantic. Our observations suggest that . . . [Full Text of this Article]