Genetic Profiling of Oncoid Stromatolites from the Phosphorus- Limited Rio Mesquites in Cuatro Cienegas, MX Alisa Glukhova NASA Space Grant Symposium April.

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Presentation transcript:

Genetic Profiling of Oncoid Stromatolites from the Phosphorus- Limited Rio Mesquites in Cuatro Cienegas, MX Alisa Glukhova NASA Space Grant Symposium April 21 st 2012 Mentors: Amisha Poret-Petterson & Ariel Anbar

Introduction Phosphorus (P) is an essential element for all organisms P is an important component of biological molecules and often a limiting nutrient DNA RNA ATP Phospholipids

Introduction Stromatolites are layered microbial mats Biological growth and mineral deposition Interaction between microbial growth, calcification, and P availability

Introduction Rio Mesquites stromatolites live in an environment with the lowest P content (0.6  mol L -1 ) reported in continental waters Stromatolites thrive in Rio Mesquites because P limitation has decreased the population of snails and other grazers

Hypotheses 1.The microbial community is P- limited and will remain the same, but increase in size due to growth (alleviation of P- limitation) 2.The microbes are adapted to low P conditions and a species composition change may occur with addition of P. 3.There could also be a combination of both. Original Community 1 2 3

Methods Treatments: Control (no addition) Low Phosphorus (5 µM N 2 HPO 4 ) High Phosphorus (10 µM N 2 HPO 4 ) Carbon (53 µM acetate + 53 µM glucose) Low P + Carbon High P + Carbon

Methods PCR (8FFAM/1492R) Restriction Digest of PCR Products Capillary Electrophoresis T-RFLP Microbial Community Fingerprint T-RF Fluorescence

Results

Control LP HP CLP CHP T-RFs become more complex with C addition Growth ofheterotrophic bacteria

Summary & Future Directions PCR-amplified and restricted bacterial 16S rRNA genes from oncoid stromatolites incubated with additions of C and P Most complex T-RF patterns were obtained with organic C addition, suggesting that the population of heterotrophic microbes in stromatolites increased. Perform a detailed analysis of these T-RF profiles to confirm these initial findings Compare T-RFLP patterns to stromatolite chemical compostion data (C, N, and P)

Acknowledgements Jessica Corman James Elser Ariel Anbar Christie Sabin Zuri Martinez