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Last modified
8/16/2009 3:06:22 PM
Creation date
10/4/2006 7:01:37 AM
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Board Meetings
Board Meeting Date
1/12/1998
Description
CF Section - Proposed Non-Reimbursable Projects - Denver Museum of Natural History - Denver Basin Aquifers Research Project
Board Meetings - Doc Type
Memo
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<br />. <br /> <br />Project Summary from the National Science Foundation Research proposal' <br />submitted on December 1, 1997 <br /> <br />PALEOBIOLOGICAL AND GEOLOGICAL FRAMEWORK OF THE <br />DENVER BASIN: FLORAL EVOLUTION AND ECOLOGY ON AN <br />EVOLVING SYNOROGENIC LANDSCAPE. <br /> <br />The Denver Museum of Natural History (DMNH) proposes to develop an integrated <br />paleobiological and geological framework for the Upper Cretaceous and lower Tertiary <br />rocks in the Denver Basin using a multi-disciplinary approach of paleontology (plant <br />megafossils and palynomorphs), magnetostratigraphy, and lithostratigraphy. The study <br />will be based on a multitude of surface observations and fossil sites tied to a new cored <br />well to be drilled by this project in cooperation with local, state, and government agencies. <br />The well will be located in the center of the Denver Basin at the Elbert County Fairgrounds <br />in Kiowa. Magnetostratigraphy, lithostratigraphy, and palynostratigraphy of the 6 10m well <br />supported by this proposal will be used to erect a reference geochronology and <br />biostratigraphy for the Denver Basin. This master section will be used to correlate basin- <br />wide surface fossil sites and observations. <br /> <br />. <br /> <br />The resulting data framework will be used to test three major hypotheses. <br />. The fIrst hypothesis is the Denver Basin contains two distinct unconformity-bounded <br />sequences of synorogenic strata. <br />. The second hypothesis is that the Cretaceous-Tertiary (K-T) boundary impact event at <br />Chicxulub in Mexico caused greater biotic damage proximal to the impact site than <br />distal to it. <br />. The third hypothesis is that the evolution and inf1lling of the Laramide Denver Basin <br />was driven by sediment supply and subsidence rather than by climate change. <br /> <br />The intrinsic benefIts of this research will be seen in the fIelds of sequence stratigraphy, <br />basin tectonics, paleobotany, magnetostratigraphy, paleoclimarology, biostratigraphy, and <br />extinction studies. The project will also have direct and immediate extrinsic benefIts and <br />will provide superb educational opportunities. The 6lOm sequence to be studied contains <br />the majority of the aquifers that provide water for the rapidly growing populations in the <br />central Denver Basin. The location of the reference well is such that it will provide much <br />needed data on water quality and aquifer characteristics. The local, state, and government <br />agencies that will cost share to help fund the drilling of the reference well will benefIr not <br />only from the science funded by this proposal but will also undertake their own <br />hydrological research on the well core. The USGS Division of Water Resources will <br />coordinate this aspect of the research. The well itself has the potential to be developed as a <br />water resource for the town of Kiowa and for Elbert County. <br /> <br />As the umbrella organization for the project, DMNH will coordinate the basic research and <br />educational endeavors resulting from this research. Educational opportunities of this project <br />are immense since they will link popular science, such as dinosaur extinction and fossil <br />rainforests, with local resource utilization issues in one of the fastest growing urban areas <br />in the country. Educational products focusing on the topics of paleontology, geology, <br />hydrology, and resource utilization could include such diverse products as teacher training <br />workshops, adult education symposia, temporary exhibits, and outreach exhibits. <br /> <br />. <br /> <br />, <br />
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