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Heather
McCarren Dr. Brian Huber, Ph.D.
"Before my research here at the National Museum of Natural History, I could never have imagined feeling so at home working in the Cushman room. This experience has truly been an honor and a privilege." |
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Phylogeny
and depth ecology of Late Cretaceous planktonic foraminifer species
of Globigerinelloides At
least eight species of foraminifera, a group of marine protists that
comprise an important part of the fossil record, in the genus Globigerinelloides
(G. multispinus, G. prairiehillensis, G. messinae,
G. subcarinatus, G. volutus, G. alvarezi, G.
aspensis, and G. impensus) are frequently identified in
various studies of Late Cretaceous marine sediments, but opinions
vary as to which of these species names are accurate and should be
retained. In an effort to stabilize the taxonomy, or naming, of this
group, primary type specimens of most of these species were compared
with Globigerinelloides morphotypes from ODP Site 690 (Weddell
Sea), DSDP, Sites 463 and 465 (tropical Pacific), and DSDP Site 511
(Falkland Plateau). Morphometric data, coiling metrics, and shape
analysis based on high-resolution x-ray images from umbilical and
edge views were extremely useful in characterizing population variability
for each of these planispirally coiled morphotypes. Results indicate
that Late Cretaceous Globigerinelloides include two distinct
lineages, one with 10 to 15 chambers and the other with 20 to 25 chambers
in adult specimens. Identification has been made of what may represent
a new species from this latter group, which will be described at a
later date. Differences in chamber shape, chamber size increase rates,
and external shell ornamentation are used to delineate species populations
within these two lineage groups. Stable isotope analyses of the biometrically
differentiated Globigerinelloides taxa will be obtained to
determine their relative depth ecologies. Earlier Globigerinelloides
taxa will be similarly analyzed to reconstruct their Late Cretaceous
evolutionary history. This research was supported by a grant from the National Science Foundation Research Experiences for Undergraduates program, Award Number DBI 9820303. |