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MRC-121 Department of Paleobiology, 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
ALEGRET, L., Recovery of the deep-sea floor after the Cretaceous-Paleogene boundary event: The benthic foraminiferal record in the Basque–Cantabrian basin and in South-eastern Spain. — Palaeogeography, Palaeoclimatology, Palaeoecology, v. 255, 2007, p. 181–194, 6 figures. — "A detailed analysis of the Upper Cretaceous and lower Paleogene benthic foraminiferal assemblages (>63 µm) from the middle bathyal Loya section (Basque–Cantabrian Basin, Southwestern France) has been carried out. The benthic foraminiferal and palaeoenvironmental turnover across the K/Pg boundary at Loya has been compared to that observed in the nearby Bidart section. . ." (from Abstract).
ALLEN, A. P., and SAVAGE, V. M., Setting the absolute tempo of biodiversity dynamics. — Ecology Letters, v. 10, 2007, p. 637–646, 5 figures, 1 table, 1 appendix. — "Setting the absolute tempo yields quantitative predictions on biodiversity dynamics that can be tested using contemporary and fossil data. Allowing incipient-species abundances greater than one individual yields predictions on how these dynamics, and the form of the species-abundance distribution, are affected by multiple speciation modes. We apply this new model to contemporary and fossil data that encompass 30 Myr of macroevolution for planktonic foraminifera. . ." (from Abstract).
BASSI, D., HOTTINGER, L., and NEBELSICK, J. H., Larger Foraminifera from the Upper Oligocene of the Venetian area, North-East Italy. — Palaeontology, v. 50, 2007, p. 845–868, 9 figures, 4 plates. — "A moderately diverse larger foraminiferal
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