The Organic Geochemistry Laboratory at UIC
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    • Paleokarsts and sediment fills
    • Coring Douglas Lake (Michigan)
    • Antarctica 2002: CORING THE LAKES
    • Antarctica 2005: VIDA 1
    • Antarctica 2010: VIDA 2
    • Deep under for gold and biomarkers
    • Abu Dhabi sabkha and lagoon
    • Laguna Mendosa, Guatemala
    • Yellowstone Microbial films
    • Geological features at UIC
    • Geobiology Course 2015 - Luoth Chou
    • Just clouds and haloes
    • Flying over Greenland
    • Field trip to Missouri 2017
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  • AN ORGANIC GEOCHEMISTRY PRIMER
    • A brief history of Organic Geochemistry
    • From bio- to geo-molecules
    • Diagenesis: Stereoisomerism
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Research at the Organic Geochemistry Laboratory at UIC

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ASTROBIOLOGY
OGL will build a very high pressure experimental system allowing to train selected Archeae and Bacteria to grow in the conditions of Titan's liquid water ocean - up to eight times the pressure of the deepest part of Earth's ocean. First, organisms will be trained to grow at very high pressure; then at the temperatures and chemical conditions of Titan's liquid water ocean.  This research is  conducted in collaboration with Professor Meyer-Dombard (UIC). Our experimental system will allow for multiple experiments to be run in parallel for long periods of time. The project integrates lipid analysis, genomics and proteomics in an effort to determine the controls of the evolution of membrane lipids under very high pressure and cold temperatures.    
This project is funded via the "Habitability of hydrocarbon worlds: Titan and beyond" a NASA Astrobiology Institute based at the Jet Propulsion Laboratory (05/2018-04/2023). 
[Image credit: NASA/JPL-Caltech/Space Science Institute. View of Titan in front of Saturn.  Cassini Huygens mission]
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PALEOBIOLOGY 

Archean sediments of Timmins (Canada):  Are Archaean biomarkers myth or reality?
Collaborating with Luke Handley in the UIC Department of Chemistry, and using his full spectrum laser desorption with laser postionization-mass spectrometer (fs LDPI-MS), we will map organic compounds in Late Archaean samples from the Abitibi Greenstone Belt in Timmins Ontario, Canada. These samples were previously studied by Todd Ventura (see Ventura et al. 2008 PNAS 104, 14260-14265) so we have a good view of the existing contaminants and the compounds having potential for being Archaean. Using fs-LDPI-MS we will will be able to determine what represents original biomarkers and what represents post-depositional contamination in these 2.65 billion year old sediments. This project forms the basis of Joey Pasterskli's Ph.D. thesis.  This project is funded by the NASA Exobiology program.  
 
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BIOGEOCHEMISTRY

Metabolomics: Metabolomics is the study of metabolites for the purpose of identifying active processes in an ecosystems. This approach is applied to the cold brine (-13.4 ˚C) of Lake Vida (Victoria Valley, Antarctica), in which a very slow growing microbial ecosystem was characterized (Murray et al. 2012). This project will integrate metabolomics, metagenomics. and geochemistry; it is carried out by Luoth Chou as part of her Ph.D. research.   
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 ENVIRONMENTAL and FORENSIC

Natural attenuation and toxicity of parking and road crankcase oil stains: This project is led by Muna Zabarmawi and forms the basis of her PhD research. Muna Zabermawi  receives a fellowship from the Kingdom of Saudi Arabia. 
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PALEOKARSTS and SEDIMENT FILLS in the ORDOVICIAN of  ILLINOIS
The Paleokarsts and Sediment Fills project is driven by Roy Plotnick (UIC) and Fabien Kenig (UIC) with the collaboration of Andrew Scott (Royal Holloway, UK) and Ian Glasspool (FMNH at the time; now Colby College). This project led to many publications in the field of paleobotany, stratigraphy, and paleobiogeochemistry because of the excellent, uncompressed preservation of plant fossils and the remarkable preservation of plant and arthropod tissues.  We are continuing to monitor quarries of North East Illinois for paleokarst features.   
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PALEOCEANOGRAPHY
Biomarker reconstruction of water column structure and dynamics: Upper Devonian- Lower Mississippian of North America. This a long running project in the laboratory, with previous studies of the Cenomanian-Turonian Western Interior Seaway, and now a concentration on the frequency of photic zone anoxia in the depositional centers  of intracratonic basins of North America during  Upper Devonian-Lower Mississippian.  
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