22 Soils in Medical Geology
Monday, 26 August 2013
1:50 PM - 5:30 PM
Washington I
THE CELLULAR INFLAMMATORY STRESS RESPONSE GENERATED BY SELECT MARTIAN, LUNAR AND ASTEROIDAL METEORITE SAMPLES – IMPLICATION FOR HUMAN SPACE EXPLORATION
Paper number: 22-9
Program: Sessions
Time: 4:30 PM – 4:50 PM
Authors
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Francis M. McCubbinUniversity of New Mexico, Albuquerque, NM
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Alexander SmirnovDowling College, Oakdale, NY
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Jillian NissenStony Brook University, Stonybrook, NY
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Martin A.A. SchoonenStony Brook University, Stonybrook, NY
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Styliani-Anna E. TsirkaStony Brook University, Stonybrook, NY
Abstract
In this study, the oxidative stress generated by selected meteorite samples is examined and compared to terrestrial mid-ocean ridge basalt (MORB). The primary marker utilized in the study is the cellular inflammatory stress response (ISR) of A549 human lung epithelial cells, defined as the cellular upregulation of ROS (indicator of future apoptosis) normalized by cellular viability (necrosis). The MORB is non-reactive and generated the lowest ISR, followed by the Vesta HED meteorites (NWA 2060 and Berthoud), which are also essentially non-reactive. Only one of the lunar meteorites (NWA 4734) is reactive, while the second one (NWA 7611) generates in ISR lower than the HED meteorites. Both Martian meteorite samples (NWA 7034 and Tissint) generated a significant ISR, with NWA 7034 generating a response similar to terrestrial soil contaminated with high levels of trace elements (NIST 2710).
The ISR generated by the Martian meteorite samples is likely due to their higher iron contents. Although more samples (primary, secondary or simulants) are needed in order to fully understand the hazards at the surface of each planetary body, the meteorite samples selected offer a basis for evaluating the risk of human exploration to these types of planetary bodies.