Shape and isotopic differences between conspecific foraminiferal morphotypes and resolution of paleoceanographic events

[1]  W. Full,et al.  Fundamental problems associated with “eigenshape analysis” and similar “factor” analysis procedures , 1986 .

[2]  Douglas F. Williams,et al.  Morphometric Analysis of Sphaeroidinellopsis: New Biostratigraphic Information from Gradually Evolving Lineages: ABSTRACT , 1986 .

[3]  M. Sarnthein,et al.  Benthic foraminiferal δ13C and accumulation rates of organic carbon: Uvigerina Peregrina group and Cibicidoides Wuellerstorfi , 1986 .

[4]  Robert Ehrlich,et al.  Morphometric and stable isotopic evidence for subpopulations of Globorotalia truncatulinoides , 1985 .

[5]  A. Mix,et al.  North Atlantic surface-ocean control of Pleistocene deep-ocean circulation , 1985 .

[6]  B. Corliss Microhabitats of benthic foraminifera within deep-sea sediments , 1985, Nature.

[7]  B. Malmgren,et al.  Fourier shape analysis of Upper Cretaceous Normapolles from southern Sweden: Taxonomic implications , 1984 .

[8]  R. Thunell,et al.  Fourier shape analysis and planktonic foraminiferal evolution; the Neogloboquadrina-Pulleniatina lineages , 1984 .

[9]  J. Duplessy,et al.  13C Record of Benthic Foraminifera in the Last Interglacial Ocean: Implications for the Carbon Cycle and the Global Deep Water Circulation , 1984, Quaternary Research.

[10]  N. J. Shackleton,et al.  Carbon isotope data in core V19-30 confirm reduced carbon dioxide concentration in the ice age atmosphere , 1983, Nature.

[11]  Nancy Healy-Williams,et al.  Fourier shape analysis of Globorotalia truncatulinoides from late Quaternary sediments in the southern Indian Ocean , 1983 .

[12]  E. Boyle,et al.  Deep Circulation of the North Atlantic over the Last 200,000 Years: Geochemical Evidence , 1982, Science.

[13]  S. Rittenberg Bacteria. (Book Reviews: The Prokaryotes) , 1982 .

[14]  G. P. Lohmann,et al.  Carbon Isotopic Changes in Benthic Foraminifera from the Western South Atlantic: Reconstruction of Glacial Abyssal Circulation Patterns , 1982, Quaternary Research.

[15]  Robert Ehrlich,et al.  Some approaches for location of centroids of quartz grain outlines to increase homology between Fourier amplitude spectra , 1982 .

[16]  M. Bender,et al.  Carbon and oxygen isotopic disequilibria of recent deep-sea benthic foraminifera☆ , 1981 .

[17]  G. Keller,et al.  Miocene benthic foraminiferal isotope records: A synthesis , 1981 .

[18]  J. E. Klovan,et al.  EXTENDED QMODEL—objective definition of external end members in the analysis of mixtures , 1981 .

[19]  R. Matthews,et al.  Core-top evaluation of benthic foraminiferal isotopic ratios for paleo-oceanographic interpretations , 1981 .

[20]  Douglas F. Williams,et al.  Fourier analysis of test shape of planktonic foraminifera , 1981, Nature.

[21]  DOUGLAS F. Williams,et al.  Carbon isotopic compositions of Recent planktonic foraminifera of the Indian Ocean , 1977 .

[22]  S. Savin The History of the Earth's Surface Temperature During the Past 100 Million Years , 1977 .

[23]  S. Savin,et al.  Stable Isotope and Magnesium Geochemistry of Recent Planktonic Foraminifera from the South Pacific , 1973 .

[24]  R. Ehrlich,et al.  An Exact Method for Characterization of Grain Shape , 1970 .

[25]  L. Robbins,et al.  INTEGRATION OF PROTEIN BIOGEOCHEMISTRY, QUANTITATIVE MORPHOLOGY AND ISOTOPE GEOCHEMISTRY AS A POTENTIAL BIOSTRATIGRAPHIC TOOL , 1987 .

[26]  Nancy Healy-Williams,et al.  Quantitative image analysys: Application to planktonic foraminiferal paleoecology and evolution , 1984 .

[27]  W. Berggren,et al.  Neogene planktonic foraminifera: A phylogenetic atlas , 1983 .

[28]  S. Savin,et al.  Biological fractionation of oxygen and carbon isotopes by recent benthic foraminifera , 1980 .

[29]  E. Vincent,et al.  Sable isotopes in deep-sea carbonates - box core erdc-92, west equatorial pacific , 1978 .

[30]  N. Shackleton Attainment of isotopic equilibrium between ocean water and the benthonic foraminifera genus Uvigerina: isotopic changes in the ocean during the last glacial , 1974 .