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MRC-121 Department of Paleobiology, P.O. Box 37012, 10th and Constitution Ave NW, Washington, DC 20013 USA
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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.
ADABI, M. H., ZOHDI, A., GHABEISHAVI, A., and AMIRI-BAKHTIYAR, H. W., Surface and deep water changes in the northeast Indian Ocean during the last 60 ka inferred from carbon and oxygen isotopes of planktonic and benthic foraminifera. — Palaeogeography, Palaeoclimatology, Palaeoecology, v. 262, doi:10.1016/j.palaeo.2008.03.007, 2008, p. 182–188, 4 figures, 3 tables. — "Stable carbon and oxygen isotopic records of planktonic (Globigerinoides ruber) and benthic foraminifera (mostly Cibicidoides wuellerstorfi) from a deep-sea core in the northeast Indian Ocean are used to infer surface and deep water characteristics for the last ~ 60 kyr. The gravity core (SK-157-14) studied here was retrieved from the Ninetyeast Ridge (5°11'N; 90°05'E) at a water-depth of 3306 m. . .." (from Abstract).
BALLENT, S. C. and CARIGNANO, A. P., Morphological abnormalities in Late Cretaceous and early Paleocene foraminifer tests (northern Patagonia, Argentina). — Marine Micropaleontology, v. 67, doi:10.1016/j.marmicro.2008.02.003, 2008, p. 288–296 1 figure, 2 plates, 3 tables. — "The sedimentology of the sections and the character of the accompanying faunas indicate that the abnormalities in the two benthic foraminiferal taxa were most probably caused by hypersalinity and/or fluctuations in salinity. The fossil occurrence of assemblages with abundant deformed specimens suggests that investigators should carefully look at many aspects of the environment before concluding that anthropogenic pollution is the only cause of deformations of living benthic foraminifera." (from
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