MARS , PANSPERMIA , AND THE ORIGIN OF LIFE : WHERE DID IT ALL BEGIN ? by

During the nineteenth century, when steadystate cosmological theories were in vogue, Lord Kelvin, Svante Arrhenius, and other eminent scientists believed that the transfer of life from one planet to another was a process made inevitable by the infinite extent and duration of the universe. This hypothesis, known as panspermia, subsequently fell out of favor, partly as a result of the acceptance of the Big Bang theory. Most efforts to understand the origin of life have since been framed by the assumption that life began on Earth. However, in the last decade data have begun to accumulate suggesting that panspermia may in fact be a natural and frequently occurring process. Recent paleomagnetic studies on Martian meteorite ALH84001 have shown that this rock traveled from Mars to Earth without its interior becoming warmer than 40oC (Weiss et al. 2000) (Fig. 1). Experiments aboard the European Space Agency’s Long Duration Exposure Facility indicate that bacterial spores can survive in deep space for more than five years (Horneck et al. 1994; Horneck 1999), and laboratory experiments demonstrate that bacteria can survive the shocks and jerks expected for a rock ejected from Mars (Mastrapa et al. 2001). Finally, dynamical studies indicate that the transfer of rocks from Mars to Earth (and to a limited extent, vice versa) can proceed on a biologically short time scale, making it likely that organic hitchhikers have traveled between these planets many times during the history of the Solar System (Mileikowsky et al. 2000; Weiss and Kirschvink 2000). These studies demand a re-evaluation of the long-held assumption that terrestrial life evolved in isolation on Earth. Figure 1. Magnetic scan of a slice of ALH84001, superimposed on its optical image. Intensity of the perpendicular component of the magnetic field is depicted with a red and blue color scale (corresponding to field lines oriented out-of-the-page and into-the-page, respectively). Note the large magnetic anomaly centered on the fusion crust, and the baked zone that extends less than a few mm inwards from it. The center of the rock has a heterogeneous magnetic pattern, indicating that it has not been heated even to 40oC since before 15 Ma (Weiss et al. 2000). This implies that rocks can travel between Mars and Earth without being heat sterilized.

[1]  G. Reitz,et al.  Long-term survival of bacterial spores in space. , 1994, Advances in space research : the official journal of the Committee on Space Research.

[2]  D. Sumner Carbonate precipitation and oxygen stratification in late Archean seawater as deduced from facies and stratigraphy of the Gamohaan and Frisco formations, Transvaal Supergroup, South Africa , 1997 .

[3]  R. Huber,et al.  Early evolution of cytochrome bc complexes. , 2000, Journal of molecular biology.

[4]  J. Kasting,et al.  UV shielding of NH3 and O2 by organic hazes in the Archean atmosphere , 2001 .

[5]  P. Cloud Oasis in Space: Earth History from the Beginning , 1988 .

[6]  H. Melosh,et al.  Survival of bacteria exposed to extreme acceleration: implications for panspermia , 2001 .

[7]  J. Kasting,et al.  Greenhouse warming by CH4 in the atmosphere of early Earth. , 2000, Journal of geophysical research.

[8]  A. Anbar,et al.  A photochemical model of the martian atmosphere. , 1994, Icarus.

[9]  H. V. Lauer,et al.  Letter. A simple inorganic process for formation of carbonates, magnetite, and sulfides in martian meteorite ALH84001 , 2001 .

[10]  M. Wadhwa,et al.  Redox State of Mars' Upper Mantle and Crust from Eu Anomalies in Shergottite Pyroxenes , 2001, Science.

[11]  S. Mojzsis,et al.  Sulfur isotopic compositions of individual sulfides in Martian meteorites ALH84001 and Nakhla: implications for crust–regolith exchange on Mars , 2000 .

[12]  G. Horneck,et al.  Natural Transfer of Viable Microbes in Space: 1. From Mars to Earth and Earth to Mars , 2000 .

[13]  B. Cohen,et al.  Support for the lunar cataclysm hypothesis from lunar meteorite impact melt ages. , 2000, Science.

[14]  Carmen Ascaso,et al.  Chains of magnetite crystals in the meteorite ALH84001: Evidence of biological origin , 2001, Proceedings of the National Academy of Sciences of the United States of America.

[15]  K. Towe Earth's Early Atmosphere. , 1987, Science.

[16]  J. Kirschvink,et al.  Paleoproterozoic snowball earth: extreme climatic and geochemical global change and its biological consequences. , 2000, Proceedings of the National Academy of Sciences of the United States of America.

[17]  Tobias Owen,et al.  The composition and early history of the atmosphere of Mars , 1992 .

[18]  J. Schopf,et al.  CARBONACEOUS FILAMENTS FROM NORTH POLE , WESTERN AUSTRALIA : ARE THEY FOSSIL BACTERIA IN ARCHEAN STROMATOLITES ? A DISCUSSION , 2002 .

[19]  Ness,et al.  Global distribution of crustal magnetization discovered by the mars global surveyor MAG/ER experiment , 1999, Science.

[20]  Roger E. Summons,et al.  2-Methylhopanoids as biomarkers for cyanobacterial oxygenic photosynthesis , 1999, Nature.

[21]  J. Fox,et al.  Upper limits to the outflow of ions at Mars: Implications for atmospheric evolution , 1997 .

[22]  K. D. McKeegan,et al.  Evidence for life on Earth before 3,800 million years ago , 1996, Nature.

[23]  G. Horneck European Activities in Exobiology in Earth Orbit: Results and Perspectives, Exobiology in Earth Orbit , 1999 .

[24]  M. F. Mckay,et al.  Truncated hexa-octahedral magnetite crystals in ALH84001: Presumptive biosignatures , 2001, Proceedings of the National Academy of Sciences of the United States of America.

[25]  J P Wikswo,et al.  A low temperature transfer of ALH84001 from Mars to Earth. , 2000, Science.

[26]  Joseph L. Kirschvink,et al.  Magnetofossils, the Magnetization of Sediments, and the Evolution of Magnetite Biomineralization , 1989 .

[27]  Joseph L. Kirschvink,et al.  Records of an ancient Martian magnetic field in ALH84001 , 2001 .

[28]  M. Thiemens,et al.  Atmosphere-surface interactions on Mars: delta 17O measurements of carbonate from ALH 84001. , 1998, Science.

[29]  J. Crowley,et al.  Vestiges of life in the oldest Greenland rocks? A review of early Archean geology in the Godthabsfjord region, and reappraisal of field evidence for > 3850 Ma life on Akilia. , 2000, Precambrian research.

[30]  A. Knoll,et al.  Stromatolites in Precambrian carbonates: evolutionary mileposts or environmental dipsticks? , 1999, Annual review of earth and planetary sciences.

[31]  Hidemi Watanabe,et al.  A genomic timescale for the origin of eukaryotes , 2001, BMC Evolutionary Biology.

[32]  B. Runnegar,et al.  Megascopic eukaryotic algae from the 2.1-billion-year-old negaunee iron-formation, Michigan. , 1992, Science.

[33]  B. Jakosky,et al.  Impact of a paleomagnetic field on sputtering loss of Martian atmospheric argon and neon , 1997 .

[34]  R. Clayton,et al.  The Accretion, Composition and Early Differentiation of Mars , 2001 .

[35]  D. Moreira,et al.  Respiratory Chains in the Last Common Ancestor of Living Organisms , 1999, Journal of Molecular Evolution.

[36]  R. Phillips,et al.  Mars' volatile and climate history , 2001, Nature.

[37]  J. Kasting,et al.  Rise of atmospheric oxygen and the “upside‐down” Archean mantle , 2001 .

[38]  A. Nutman,et al.  Origin of life from apatite dating? , 1999, Nature.

[39]  J. Schopf,et al.  Microfossils of the Early Archean Apex Chert: New Evidence of the Antiquity of Life , 1993, Science.

[40]  J. Schopf,et al.  Early Archean (3.3-billion to 3.5-billion-year-old) microfossils from Warrawoona Group, Australia. , 1987, Science.

[41]  R. Rye,et al.  Atmospheric carbon dioxide concentrations before 2.2 billion years ago , 1995, Nature.

[42]  W. Doolittle,et al.  The nature of the universal ancestor and the evolution of the proteome. , 2000, Current opinion in structural biology.

[43]  M. Thiemens,et al.  Atmospheric influence of Earth's earliest sulfur cycle , 2000, Science.

[44]  J. Kirschvink,et al.  Elongated prismatic magnetite crystals in ALH84001 carbonate globules: potential Martian magnetofossils. , 2000, Geochimica et cosmochimica acta.

[45]  David E. Smith,et al.  Ancient Geodynamics and Global-Scale Hydrology on Mars , 2001, Science.

[46]  J. William Schopf,et al.  The Proterozoic biosphere : a multidisciplinary study , 1992 .