Sulfate-rich eolian and wet interdune deposits, Erebus crater, Meridiani Planum, Mars. Find 744 Understanding Earth 7th Edition by Grotzinger et al at over 30 bookstores. 4, Appendix 4) 2. The presence of water is an indicator of potential habitability as well as of formerly different climatic conditions. Grotzinger, J. P. , Watters, W. and Knoll, A. H., 2000, Calcified metazoans in thrombolite-stromatolite reefs of the terminal Proterozoic Nama Group, Namibia. Butterfield, N. J., and Grotzinger, J. P., 2012, Palynology of the Huqf Supergroup, Oman. In Comparative Climatology of Terrestrial Planets (S. J. Mackwell et al., eds. Bontognali TRR, Sessions AL, Allwood AC, Fischer WW, Grotzinger JP, Summons RE, Eiler JM (2012) Sulfur isotopes of organic matter preserved in 3.45 Gyr-old stromatolites reveal microbial metabolism, Proceedings of the National Academy of Sciences, 109, 15146-15151. Grotzinger, J. P., and Jordan, 2010, Understanding Earth, 6th Edition, Freeman, 582 pp. Measurement of the carbon isotope ratios in ancient carbonate rocks provides the principal basis by which the fluxes of reduced and oxidized carbon are determined over the course of Earth's history. McLennan, S. M., Bell III, J. F., Calvin, W., Grotzinger, J. P., and 28 others, 2005, Provenance and diagenesis of the evaporite-bearing Burns formation, Meridiani Planum, Mars. Milliken, R., Grotzinger, J., and Thomson, B., 2010, The paleoclimate of Mars from the stratigraphic record in Gale Crater. Springer, London, 763 pp. Freeman, 567 pp. Lee C, Fike DA, Love GD, Sessions AL, Grotzinger JP, Summons RE, Fischer WW (2013) Carbon isotopes and lipid biomarkers from organic-rich facies of the Shuram Formation, Sultanate of Oman, Geobiology, doi: 10.1111/gbi.12045. ), p. 439-472 Univ. A long-standing goal of Mars environmental studies has been to understand the role of water throughout its geologic history. ), Early Life on Earth, Columbia University Press, p. 245-258 . Buy, rent or sell. Grotzinger, J.P., and Vasavada, A., 2012, Reading the red planet. Grotzinger, J. P. Trends in Precambrian carbonate sediments and their implication for understanding evolution. 550-543 Ma), Namibia. Scientific American, July, 2012, p. 40-43. However, we can now directly examine the record of past surface processes, including the role of water, through sedimentologic studies of the stratigraphic record of Mars. Globally distributed carbonate rocks of middle Ediacaran age (ca. Sequence stratigraphy in Proterozoic Successions. Nature, v. 347, p. 64-66. Schröder, S. and Grotzinger, J. P., 2007, Evidence for anoxia at the Ediacaran-Cambrian boundary: The record of redox-sensitive trace elements and rare-earth elements in Oman. Jordan, T.H., and Grotzinger, J.P., 2008, Essential Earth, 1st Edition, Freeman, 384 pp. An abiotic model for stromatolite morphogenesis. Geology, v. 24, p. 119-122. of Arizona, Tucson. Science, v. 343, DOI: 10.1126/science.1242777. The Shuram carbon isotopic excusion - the largest known in Earth history - has been the subject of intensive research at Caltech. Grotzinger, J. P. and Rothman, D. H., 1996. He was Project Scientist for the Mars Science Laboratory (MSL) Curiosity rover mission, a Participating Scientist for the Mars Exploration Rover (MER) mission, and a Participating Scientist for the High Resolution Science Experiment (HiRISE) camera, on board the Mars Reconnaissance Orbiter (MRO). Grotzinger, J. P., Jordan, T. H., Press, F., and Siever, R., 2006, Understanding Earth, 5th Edition, Freeman, 579 pp. Nature, 474, 68-72. Farley, K.A., Malespin, C., Mahaffy, P., Grotzinger, and 29 others (2014), In-situ Radiometric and Exposure age dating of the Martian surface. These results highlight the biological viability of fluvial-lacustrine environments in the post-Noachian history of Mars. Journal of the Geological Society of London, v. 164, p. 175-187. How We Study Earth (Ch. Nature, v. 383, p. 423-425. The rover landed in Gale Crater on August 5, 2012. Grotzinger's research has applied a process-based approach, oriented toward deconvolving the replacement textures of ancient stromatolites. Though the accretion process is commonly regarded to result from the sediment trapping or precipitation-inducing activities of microbial mats, only rarely is evidence of this process preserved in Precambrian stromatolites. Journal of Sedimentary Research, 79, p. 247-264. Stromatolites: Evolutionary mileposts or environmental dipsticks? Grotzinger, J. P., and Miller, R., 2008, The Nama Group.
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