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Grant S. Boardman, PhD Candidate
Figure 1. Myself in the Bighorn Basin, Wyoming. |
Vertebrate
Paleontologist and Stable Isotope Geochemist |
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Figure 2. Summer field crew 2011 in Toadstool Geologic Park, from
left to right: Ross Secord, Jason Moore (Dartmouth), myself, and Jason's
students from Dartmouth College. |
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Department of Earth and Atmospheric Sciences (UN-L) Office: 211 Bessey Hall University E-mail: gboardman80@huskers.unl.edu Personal Email: grant128@hotmail.com
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About Me: I am
currently a PhD Candidate in Earth and Atmospheric Sciences at UN-L. I was born and raised in the Metro-New
Orleans area. I do not have a “Southern” accent, but I can affect one if you
ask nicely. I do say “Y’all” on occasion, but that is about
as Southern as I get. I am married and
I have three siblings. I love the
educational process, and hope to become a better teacher. I have been interested in vertebrate
paleontology and collecting fossils ever since I was a very small child (and
YES, there are fossils in Louisiana).
I also love to collect (and skin if fresh) and skeletonize any critter
I can get my hands on. Vita available upon request. |
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Education: BS
Geology and Geophysics, Louisiana State University (LSU) 2004 MS
Biological Sciences, East Tennessee State University (ETSU) 2009 |
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Research Interests: At this point in time I am specifically interested
in Eocene-Oligocene mammalian paleoecology. My current research with Dr. Ross Secord focuses
on interpreting and tracking changes in diet and habitat preference in several
ungulate (i.e. hoofed mammal) groups from the latest Eocene into the early Oligocene
(a period of global climate change associated with the onset of glaciation in
Antarctica) of Nebraska using enamel stable isotopes, dental mesowear, dental
microwear
texture (done in Peter Ungar’s lab at
the University of Arkansas), and hypsodonty index analyses. If you have questions about my research feel
free to drop me an email.
Figure 3. Results of isotopic analysis for selected Eocene-Oligocene
ungulates from Nebraska. Fieldwork: For
the last several years I have been collecting in latest Eocene-earliest
Oligocene deposits in northwestern Nebraska and assisting Dr. Secord in
collecting latest Paleocene-earliest Eocene fossils in the Bighorn Basin and Togwotee Pass areas of Wyoming. Prior to that I had years
of experience collecting and excavating in Neogene
deposits in the southeastern U.S. (Louisiana, Texas, Florida, and Tennessee).
Figure 4. A Clarkforkian (latest Paleocene)
outcrop in the Bighorn Basin of Wyoming. |
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Lab Experience: Prior
to the large part of my experience in vertebrate paleontology I was a student
worker in the Invertebrate Paleontology Lab at Louisiana State University.
For over a year I worked toiling with washing samples from the Gulf of Mexico
to collect foraminifera for study by such giants in the field as Dr. Barun Sen Gupta. I gained appreciable experience in
micropaleontology and its practices during this period. Teaching and Outreach Interests: For
several years I have taught the Geology 103 (Historical Geology) Lab and on
occasion the lab for Geology 101 (Physical Geology). When I was a Masters
student and NSF GK-12 Fellow at ETSU I gained a lot of experience working
with elementary school students and had a direct hand in building an outdoor
classroom for the students, including a fossil dig pit [See Outdoor Classroom in News and
Events]. Selected Recent Publications, Presentations, Abstracts: Boardman, G.S. and R. Secord. [in review for Palaeogeography,
Palaeoclimatology, Palaeoecology]
Stable isotope
paleoecology of White River ungulates during the Eocene-Oligocene climate
transition in northwestern Nebraska. Boardman, G.S. and R. Secord. 2012. A multi-proxy reappraisal of diet and habitat in Chadronian and Orellan
ungulates from Nebraska based on stable isotopes, mesowear, and hypsodonty
index. Journal of Vertebrate Paleontology 32,
Abstracts:64A. Boardman, G.S., R. Secord, and W.E. Lukens. 2012. Minimal change in vegetation structure
across the Eocene-Oligocene boundary in Nebraska as indicated by stable
isotopes in mammals. Geological Society of America, Abstracts with Programs
44 (6):6. [Link] Lukens, W.E., D.O. Terry Jr., and G.S. Boardman. 2012. Early Oligocene paleosols and fluvial
channels at Toadstool Geologic Park, northwest Nebraska: evidence for static
climate through changing style of sedimentation. Geological Society of
America, Abstracts with Programs 44 (6):6. Boardman, G.S. and B.W. Schubert.
2011. Salamanders of the
Gray Fossil Site, Pp. 15-17 in B.W.
Schubert and J.I. Mead (eds.), Gray Fossil Site: 10 Years of Research, West
Press. Boardman, G.S. and R. Secord. 2011. Reconstructing the diets and
microhabitats of four latest Eocene-earliest Oligocene perissodactyls (mammalia) based on stable isotopes, dental mesowear, and
dental microwear texture. Journal of Vertebrate Paleontology 31, Abstracts:73A. Boardman, G.S. and B.W. Schubert. 2011. First Mio-Pliocene salamander fossil
assemblage from the southern Appalachians. Palaeontologia
Electronica 14:1-19. [PDF] Boardman, G. and R. Secord. 2010.
Paleoenvironmental interpretation of three Chadronian(Late
Eocene) mammalian faunas from the mid-continental U.S., based on body size
distributions. Journal of Vertebrate Paleontology 30, Abstracts:61A. Stout, J. and G. Boardman. 2010. Morphology and
systematics of dinosaur eggshells and the identification of problematic oospecies. Journal of Vertebrate Paleontology 30,
Abstracts:171A. Boardman, G.S. 2008. First Lamine Camel (cf. Palaeolama) reported from the Tunica Hills of
Louisiana. Current Research in the Pleistocene 25:163-165. Schiebout, J.A., P.D. White, G.S.
Boardman. 2008. Taphonomic Issues Relating to Concentrations of Pedogenic Nodules and Vertebrates in the Paleocene and
Miocene Gulf Coastal Plain: Examples from Texas and Louisiana. Pg.17-30 in
J. Sankey and S. Baszio
(eds.), Vertebrate Microfossil Assemblages: Their Role in Paleoecology and Paleobiology, Indiana University Press. |
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