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Dr. Steven J. Hageman
hagemansj@appstate.edu

Ph: 1+(828) 262-6609
Fax:
1+(828) 262-6503

Department of Geology Appalachian State Univ.
PO. Box 32008
Boone, NC  28608


 geologo

 

 

Steve Hageman
Associate Professor of Geology
Appalachian State University



Research Program

 My research efforts have been divided between two programs:
 

  • The first is an investigation of microevolutionary patterns and processes.  I use morphometric methods applied to fossil invertebrates (Bryozoa) to document subspecific morphologic variation and incorporate empirical observations into revised models for microevolution and speciation.  The colonial nature of bryozoans allows for study of the sources of morphologic variation, which are not possible to resolve with solitary fossil organisms. Work to date has demonstrated that remarkably high-level resolution of morphologic variation from fossil material can contain meaningful signals about genetic and microenvironmental influences.
  •  The second part of my research involves the distribution and ecology of Bryozoa.  This study differs from the first in that the level of interest is spacio-temporal taxic variation (species and genera).  The modern southern Australian continental shelf provided the opportunity to evaluate the ecology and distribution of an extremely diverse bryozoan fauna (400+ species, 77+ families, 3 orders in one study).  Bryozoa play a dominant role in the benthic ecosystem and carbonate sediment production in this province.  I have used Bryozoa from this province to develop a multi-dimensional, morpho-ecological space which can be used to characterize and evaluated life modes of this Phylum (refined derivative of traditional growth form analysis).  This approach has proved viable and effective in the study of broader ecological patterns in the southern Australian Temperate Province.  This methodology was integral in recognizing and understanding ephemeral substrates (host animals with cuticular or spiculate skeletons) as a primary source of sediment production in this cool-water carbonate province.

    I plan to continue both phases of my research (subspecific-morphologic and taxic-ecologic), with the intention of integrating them into a unified program.
    I have an ongoing research project with colleagues in Scotland (C. Todd and M. Bayer), who have grown replicate, cloned bryozoan colonies in controlled environmental conditions.  The morphometric work we are doing with this material will provide important insights about phenotypic and genotypic controls over morphogenesis.  This type of data is key to understanding microevolution and speciation (implications well beyond Bryozoa).  In the future I would like to perform such studies on a larger scale, with an even greater control on the genetics involved.
    The Australian work has provided me with a standardized mopho-ecological frame-work (based on species-level observations), with which to map bryozoan life-modes through time and space.  I have begun to apply this to the fossil record (Miocene of southern Australia).  I have several projects planned which will track important sediment forming cheilostome bryozoan life modes (~clades) from their origins in the Late Cretaceous and Early Tertiary, through their development as important carbonate sediment formers and major players in the benthic ecosystem of large areas.  This study is important both for an understanding of a the evolution of our modern ecosystem and comparison to the important stenolaemate bryozoan sediments of the Paleozoic of North America.
    I am continuing studies of geographic variation, community succession and paleoecology in cyclic shelf and epeiric marine sediments: Oligo-Miocene of southern Australia and Permo-Carboniferous of the mid-continent of North America.