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Past Lectures |
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2007 |
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Nov. 7 |
Frank DrakeThe End of the Habitable Zone: Lessons from the Solar System |
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Nov. 14 |
Jason BarnesTitan's Sand Dunes: Window to a New World |
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Despite theoretical predictions that Titan would not be able to support sand dunes on its surface, the Cassini orbiter has found an extensive set of sand seas astride the equator. The dunes are longitudinal in nature and resemble Earth's dunes in Namibia, the Sahara, and Arabia in height and spacing. Their spectra are consitent with hydrocarbon grains, not water ice as might be expected from erosion of an icy crust. Even with the total dune coverage of ~20%, though, the visible dune sands cannot alone account for the missing hydrocarbons expected to have been produced photochemically from atmospheric methane. With present understanding of the nature of Titan's surface and the processes that operate there still in its formative stages, the discovery of these familiar forms allows us a window into the global geology of this newly revealed world. |
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Dec. 5 |
Rocco MancinelliExtremophiles: What it takes for life to survive beyond the home planet |
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Recently we have come to realize that where there is liquid water on Earth, virtually no matter what the physical conditions, no matter where, there is life. Environments we previously thought of as having insurmountable physical and chemical barriers to life, such as extremes in temperature, pH, and radiation, are now seen as yet another niche harboring "extremophiles". This realization, coupled with new data on the survival of microbes in the space environment, and modeling of the potential for transfer of life between planets suggests that life could be more common than previously thought. Data from recent Mars missions support the notion that Mars had abundant liquid water on its surface in the past, and has salts in its regolith. It could also have brine pockets that may either be an "oasis" for an extant biota, or the last refuge of an extinct biota. Characteristics that are important to better understand how life may survive conditions on Mars include radiation and desiccation resistance, as well as the ability to survive freeze/thaw cycles. To better understand what it takes to survive these conditions we study microbes and how they live, survive and die from the lagunas in the Bolivian altiplano to the space environment in Earth orbit. We have shown that terrestrial life can survive away from Earth in a simulated Mars environment and in the space environment. This research represents the first step in understanding what it takes for life to survive away from its home planet. |
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Dec. 19 |
Devon BurrPlanetary Habitability of Mars and of Titan: A Tale of Two Worlds |
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Planetary geology provides critical information of other
worlds, including their astrobiological potential. By that term, I mean
not only their specific potential to harbor life but their more general
potential to tell us something about life. As we expand our
understanding of life – where it is, what it is, how it is –
beyond Earth, geomorphology complements compositional data in giving us clues
as to planet habitability. Mars is a case in point: the earliest to
most recent data show extensive geomorphic evidence of water, the sine qua
non for all life that we know. These remote and (recently) in situ data
indicate large volumes of water in the surface, subsurface and atmosphere
throughout Mars’ history. Yet compositional evidence in the spectral
data for organic materials is stubbornly lacking. As a converse
example, data of Titan, Saturn’s largest moon, show a near-total lack of
liquid water, as expected from its size and position relative to the
Sun. Yet this world is drenched in organic compounds. As part of its
hydrocarbon cycle (analogous to Earth’s hydrologic cycle), Titan forms
organic molecules in the upper atmosphere, which apparently result on the
surface in extensive aeolian (wind-formed) dunes. Thus, Mars and Titan
each provide disparate but important astrobiological information. In
this talk, I will give an overview of some of the most recent geologic
discoveries regarding water on Mars and organics on Titan.
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2008 |
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Jan. 2 |
Bo ThideOn the extraction of all information embedded in radio siganls: Implications for SETI |
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A new idea for utilizing all of the information in photons for communication involves a little-know electromagnetic property: the photon's orbital angular momentum (POAM). The communication and computer industries are actively looking at the possibilities. We will discuss current research and the implications for SETI. | |
Jan. 9 |
Laurance DoyleQuantum Astronomy: Extending the Weirdness of Modern Physics to Cosmic Scales |
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Is the weirdness of aspects of quantum physics confined to the microscopic? Can one trade off information at the detector, thereby changing events that should have already taken place in the past? By increasing ignorance can one actually learn something new that could not have been learned with less ignorance? Does quantum physics recognize time as defined by general relativity, and vice versa? In this seminar we'll discuss how to use the uncertainty principle as a quantum eraser in a cosmic-scale double-slit experiment -- the double-slits being gravitational lenses millions to billions of light years distant. Hopefully by the time of the seminar, our first official paper will have been accepted by The Astrophysical Journal. Anyway, if history can be changed, it won't matter.
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Jan. 16 |
Jill TarterThe Allen Telescope Array: A Wide-angle, Panchromatic Radio Camera for SETI and Radio Astronomy |
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According to Jerry Ostriker (Plumian Professor, Cambridge;
Professor of Astrophysics, Princeton; Provost, Princeton), "Surveys
aren’t just something that astronomers do, they are the only thing
astronomers do." These words are understandable, given Prof. Ostriker’s
intimate association with the Sloan Digital Sky Survey that is presently
transforming our view of the optical universe. The ability to systematically
survey one quarter of the sky, with the dynamic range and spatial resolution
to zoom in to study individual objects, is providing us with the first truly
3-dimensional map of the nearby cosmos. The optical portion of the spectrum
unveils the moderately energetic and hot components of the universe, but the
physics of the cool constituents is probed at radio wavelengths. [New
Paragraph] The Allen Telescope Array (ATA) of 350 telescopes, each 6.1 m in
diameter, will do for the radio sky what the Sloan Digital Sky Survey has
done for the optical sky. And it will do it so rapidly that it will also
provide the first systematic look at the transient radio universe. The ATA
provides simultaneous access to any frequency between 500 MHz and 11.2 GHz,
with four separate frequency channels feeding a suite of signal processing
backends that can produce wide-angle radio images of the sky in 1024 colors,
and at the same time, study up to 32 point sources of interest within its
large field of view. This new approach to commensally sharing the sky allows
SETI (the Search for ExtraTerrestrial Intelligence) and traditional radio
astronomical science to both use the telescope nearly all the time: our tools
are beginning to be commensurate with the size of the vast explorations of
the radio sky that we wish to undertake. [New Paragraph] This talk will put
the ATA into context with the rest of the SETI activities around the world
and describe the initial SETI observations we intend to conduct.
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Jan. 18 |
Francis NimmoGeodynamics of Icy Satellites |
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There are at least 37 objects in this solar system with masses greater than 1020 kg, two thirds of which have surfaces made primarily of water ice. The handful of icy bodies studied by spacecraft have revealed an enormous diversity of bizarre and unanticipated features, from geysers on Triton and Enceladus, to the peculiar shapes of Iapetus and 2003 EL61. I will discuss three aspects of icy body geodynamics: using surface observations to constrain their thermal evolution; the role of tidal heating; and their potential to undergo reorientation.
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Jan. 23 |
Adrian BrownCRISM Observations of the seasonal recession of the Martian southern polar cap |
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In this, the International Polar Year 2007-2008, it is a
satisfying time to consider our understanding of Extraterrestrial Polar
environments. On Mars, they're celebrating summertime in the austral
hemisphere, and have just gone through a big defrosting known as the
'spring recession'. Luckily, we humans had an emissary there to catch all
the action. [New Paragraph] Dr. Adrian Brown reports on the latest results
back from the Compact Reconnaissance Imaging Spectrometer for Mars (CRISM)
and explains how the unanticipated discovery by CRISM of small ephemeral
water ice deposits, common in winter areas on Earth, are of vital interest to
Mars polar science.
For more information, go to: http://abrown.seti.org |
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Jan. 30 |
Ashok SrivastavaAnomaly Detection in Data Streams and its Implications for Radio Astronomy and SETI |
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Recent advances in data mining have enabled the detection of anomalies in massive time series data sets. These techniques range from analysis of individual time series to multidimensional analysis of streaming data. [New Paragraph] A key issue in anomaly detection is characterizing the expected signal from the unexpected signal. In many situations, these characterizations can be made based on a physical understanding of the data generating process. In the context of SETI@home, the software searches for spikes in the power spectra, Gaussian rises and falls in transmission power, triplets, and pulsing signals. While these signals are well motivated based on our current knowledge of communications systems, we discuss methods of anomaly detection that do not rely on strong assumptions of the data generating process. [New Paragraph] This talk will cover recent algorithmic developments in anomaly detection with applications to SETI. | |
Feb. 6 |
Ross BeyerHiRISE views of Martian Strata and Slope Streaks |
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Ross will give a brief overview of the HiRISE instrument and then discuss how its high-resolution color imaging is contributing to an improved understanding of the geologic history of Mars as exposed in its layered outcrops. Ross will also discuss recent work regarding the enigmatic streaks observed on many slopes on Mars, and possible hypotheses regarding how these streaks change from dark to bright, and then fade away. | |
Feb. 8 |
Paul Gazis & Creon LevitViewpoints: a Fast, Interactive, Multi-platform Visualization Tool for Exploring Large Multivariate Data Sets |
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Finding effective ways to visualize of large multivariate data sets has become a significant challenge as data
volumes have grown. Modern astrophysical data sets can easily exceed millions of samples that involve hundreds
or thousands of variables. While it may be possible to plot subsets of these data using scripted languages
sch as MATLAB or IDL, this presupposes that one already knows what one wishes to plot. This is rarely
the case during the initial phases of data exploration.
Viewpoints is a fast interactive visualization and analysis tool for large, complex, multidimensional data sets. It runs on most common platforms and operating systems to produce multiple linked scatterplots that can be changed, rescaled, modified, and processed in real time in a variety of powerful and informative ways. It was originally developed for internal use by the informal ARC Cluster Group to examine data from the Sloan Digital Sky Survey, but as requests for the package arrived from a growing number of outside users, we discovered that it had considerable potential as a data exploration tool for applications ranging from aeronautical engineering, quantum chemistry, and computational fluid dynamics to virology, computational finance, and aviation safety. It should also have considerable potential for use by members of the SETI community. We will present a brief overview of viewpoints, followed by a live hands-on demonstration. We invite you to bring your own data sets (as conventional ASCII flat files) for the latter. Copies of viewpoints are also available from the project WWW site at http://astrophysics.arc.nasa.gov/~pgazis/viewpoints.htm. |
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Feb. 13 |
Elisa QuintanaTerrestrial Planet Formation and Habitability in Binary Star Systems |
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Most stars reside in binary/multiple star systems. Perturbations from a companion star can disrupt the formation and long-term stability of planets. More than 40 extrasolar planets have been detected in binary star systems, including 3 with stellar separations of only ~20 AU, well within the region spanned by planets in our Solar System. I will present results from a large suite of numerical simulations that explore the final stages of terrestrial planet formation in main sequence binary star systems. Planetary accretion is examined around one star of widely separated (> 5AU) binary stars, and also around both members of close (< 0.5 AU) binary stars, in order to determine whether/where Earth-like planets can form. I will also review the dynamics of planetary habitability via the delivery of volatiles, and examine the likelihood of a habitable world with two Suns. | |
Feb. 20 |
Baruch BlumbergHepatitis B Virus. Discovery, the Present, and the Future. |
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Hepatitis B virus was discovered as a result of a basic science project on inherited biochemical variation related to disease susceptibility. It was not, initially, directed to the discovery of hepatitis B virus (HBV), the development of a vaccine, and the prevention of a common cancer. It is an example of non-targeted basic research leading to important clinical and business outcomes. HBV is one of the most common and deadly viruses. About 400 million people worldwide are currently infected. Infection can lead to acute disease, chronic hepatitis, and primary cancer of the liver. The vaccine was invented in 1969 using an unusual process in which the vaccine protein was isolated from the blood of HBV< carriers. It is now one of the most widely used vaccines worldwide and has resulted in a striking decrease in infection and in a reduction in the incidence of liver cancer. It is the first cancer prevention vaccine and has encouraged the development of another vaccine to prevent cancer of the cervix. It is also possible to greatly decrease the risk of cancer and life-shortening chronic liver disease by the use of antivirals. There are likely to be many cancers that can be prevented and/or treated in a similar manner that could, in time, greatly decrease the burden of human cancer. The virus also has non-pathological effects; the ratio of males to females among offspring is related in a complex manner to the response of parents to infection with HBV. |
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Feb. 27 |
Javiera GuedesFormation and Detectability of Planets around Alpha Cen B |
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We simulate the formation of planetary systems around Alpha Centauri B. The N-body accretionary evolution of a 1/r disk populated with 400-900 lunar-mass oligarchs is followed for 200 Myr. All simulations lead to the formation of multiple-planet systems with at least one planet in the 1-2 Msun mass range at 0.5-1.5 AU. We examine the detectability of our simulated planetary systems by generating synthetic radial velocity observations including noise based on the radial velocity residuals to the recently published three planet fit to the nearby K0V star HD 69830. Using these synthetic observations, we find that we can reliably detect a 1.8 Msun planet in the habitable zone of Alpha Centauri B after only three years of high cadence observations. We also find that the planet is detectable even if the radial velocity precision is 3 m/s, as long as the noise spectrum is white. Our results suggest that the most significant barrier to a characterization of the Alpha Cen system is the degree of frequency dependence exhibited by the noise. | |
Mar. 5 |
Mate AdamkovicsCondensed-phase methane and tropospheric meteorology on Titan |
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| Methane is near its triple point at Titan’s surface. On the icy-cold moon of Saturn this hydrocarbon is a fluid analog of water on Earth. Transitions among the phases of methane give rise to various meteorological phenomena that can intimately link the atmosphere and surface. Despite the evidence for solid and liquid methane in Titan’s atmosphere, spectroscopic retrievals of aerosol haze opacities, cloud properties, and surface reflectivities have not included opacity due to condensed-phase methane. I will describe how a significant discrepancy between observations and radiative transfer models of near-IR spectra can be resolved by a rudimentary treatment of large methane droplets or solid methane particles. I will present observations from VLT/SINFONI, Keck/OSIRIS, and Cassini/VIMS, while explaining a technique for enhancing contrast in haze-obscured and surface-contaminated images of the lower atmosphere. Ongoing work regarding the interaction of clouds and precipitation will be cautiously presented with a handful of speculations regarding Titan’s weather patterns. | ||
Mar. 12 |
LPSC No Colloquium |
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Mar. 19 |
Tori HoehlerThe Energetics of Habitability |
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| Energy is required by all living things. Known organisms exhibit two distinct requirements, analogous to the voltage and power requirements of electrical devices, which must be met simultaneously in order to support metabolism. Quantification of these requirements, and of their sensitivity to environmental factors and organismal specifics, establishes energetic boundary conditions on ‘habitability’. These constraints are likely among the chief determinants of the possible distribution of life in the deep subsurface and in other energy-starved systems. The biochemistry of energy metabolism has largely been understood through laboratory models, but quantification of the minimum biological requirements for energy must rely on study of natural populations that are adapted to chronic energy starvation. This talk will present a general energy-balance formulation of habitability and describe the quantification of microbial minimum free energy requirements in a natural ecosystem. | ||
Mar. 21 (Friday) |
Fred SharpeHumpback Whales and the Social Intelligence Hypothesis |
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| The Drake Equation predicts a positive correlation between a silent cosmos and a tendency for intelligent life to self extinguish. Alternatively, we simply may not be able to detect or recognize intelligence life in the cosmos --or on planet earth. Humpback whales provide interesting test case, as they appear to exhibit high levels of social intelligence. In Alaska, groups of non-kin form large hunting teams with enduring bonds, specialized tasks, tool use, and gender equity. Their haunting songs and social chatter also suggest that an un-deciphered intelligence echoes through our oceans. Dr. Fred Sharpe of the Alaska Whale Foundation has teamed up with Dr. Laurance Doyle of the SETI Institute, and Dr. Brenda McCowan and Sean Hanser at the University of California, Davis. This team brings the signal processing prowess developed for interstellar inquiry to focus on the phonations of these ocean dwelling societies. We seek to define universal rules of communication and understand how humpback whales fit into the Drake Equation. We also seek to understand how intelligent societies endure or self-extinguish by balancing beneficent behaviors with bellicosity. | ||
Mar. 26 |
Jay MeloshRedox Chemistry in Large Impacts and the Origin of Life |
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| All material affected by close proximity to large impacts, for example, tektites and microkrystites, is chemically reduced compared with the starting material. In her PhD research, Abby Sheffer demonstrated that this chemical reduction is the inevitable consequence of the high temperature equilibrium between liquid and gas phases in the hot vapor plume. In parallel work on his PhD, Matt Pasek demonstrated that only the reduced form of Phosphorous can participate in aqueous reactions that lead to the precursors of life. Although Pasek sought the source of this reduced Phosphorous in the relatively rare mineral Schreibersite, I will argue that the conditions for reduction are far more general. In this talk I will discuss the thermodynamic conditions that exist in an impact vapor plume, show how reduction occurs and argue that the principal source of reduced Phosphorous on the early earth was probably material vaporized in large impacts and globally distributed in the fast distal ejecta of large impact events. All life on earth may thus owe its birth to the capacity of large asteroid impacts to perform chemical reduction. | ||
Apr. 2 |
Art WeberSugars as the Source of Energized Carbon for the Origin of Life |
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What were the chemical processes that started life on Earth? Biochemist Art Weber is trying to answer this question by studying prebiotically plausible chemical reactions in the lab – reactions that might have been responsible for biogenesis.
Art’s experiments have shown that sugars are unsurpassed in their ability to undergo spontaneous self-transformation reactions in water. Consequently, for the past decade he’s been investigating the prebiotic synthesis of sugars and their subsequent reactions in the presence of ammonia that yield a complex mixture of chemical products whose activities are essential to the origin of life, and even combine to form semi-solid microspherules that could have provided a primitive cell-like, catalytic environment. The ultimate goal of his research effort is to develop a model, self-replicating system that resembles the birth of life on Earth, and can be artificially evolved to a more dynamic and complex state. |
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Apr. 9 |
Tom PiersonSETI Institute - History, the Institute Today, and Plans for the Future |
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The Colloquium Series changes pace from our normal scientific discussions as SETI Institute CEO Tom Pierson invites everyone to join in a conversation. How did the Institute spring to life? What events punctuated its evolution? Why does the Institute have a Carl Sagan Center? What is the state of the Institute today? And what might the future bring?
From humble beginnings in a trailer at Ames Research Center, to modern facilities on Whisman Road in Mountain View, the SETI Institute truly has evolved over the past 24 years. From the beginning, the Institute’s mission has been to conduct, support, and encourage a broad range of research and educational activities intended to improve humankind’s understanding of the nature, prevalence, and distribution of life in the universe. This work encompasses SETI, astrobiology, and science education efforts funded from a wide variety of public and private sources. Tom will survey the past and present of the SETI Institute, and also provide some thoughts on how he sees the future, highlighting some of the things that senior management and the Board of Trustees are focusing on. It is hoped that this colloquium will truly be a conversation with the plenty of audience participation. All SETI Institute staff and interested supporters or collaborators are welcome and encouraged to attend. |
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Apr. 11 |
Claudio MacconeThe Statistical Drake Equation |
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We provide the statistical generalization of the Drake equation.
From a simple product of seven positive numbers, the Drake equation is now turned into the product of seven positive random variables. We call this “the Statistical Drake Equation”. The mathematical consequences of this transformation are then derived. The proof of our results is based on the Central Limit Theorem (CLT) of Statistics. In loose terms, the CLT states that the sum of any number of independent random variables, each of which may be ARBITRARILY distributed, approaches a Gaussian (i.e. normal) random variable. This is called the Lyapunov Form of the CLT, or the Lindeberg Form of the CLT, depending on the mathematical constraints assumed on the third moments of the various probability distributions. In conclusion, we show that:
Finally, a practical example is given of how our statistical Drake equation works numerically. We work out in detail the case where each of the seven random variables is uniformly distributed around its own mean value and has a given standard deviation. For instance, the number of stars in the Galaxy is assumed to be uniformly distributed around (say) 300 billions with a standard deviation of (say) 100 billions. Then, the resulting log-normal distribution of N is computed numerically by virtue of a MathCad file that the author has written. This shows that the mean value of the log-normal random variable N is actually of the same order as the classical N given by the ordinary Drake equation, as one might expect from a good statistical generalization. |
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Apr. 16 |
AbSciCon No Colloquium |
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Apr. 23 |
Norm SleepAnoxygenic photosynthesis, evolution, and the origin of continents and cyanobacteria |
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Pre-photosynthetic niches were meager with productivity << 10-4 of modern photosynthesis. Serpentinisation, arc volcanism, and ridge-axis volcanism reliably provided H2. Methanogens and acetogens reacted CO2 with H2 to obtain energy and make organic matter. These skills preadapted a bacterium for anoxygenic photosynthesis, probably starting with H2 in lieu of an oxygen acceptor. Use of ferrous iron and sulphide followed as abundant oxygen acceptors, allowing productivity to approach modern levels. The “photo-bacterium” proliferated rooting much of the bacterial tree. Land photosynthetic microbes faced a dearth of oxygen acceptors and nutrients. A consortium of photosynthetic and soil bacteria aided weathering and access to ferrous iron. Weathering led to formation of shales and, and ultimately to granitic rocks. Already oxidized and Fe-poor sedimentary rocks and low-Fe granites provided scant oxygen acceptors. So did fresh water in their drainages. Cyanobacteria evolved di-oxygen production that relieved them of these vicissitudes. They did not immediately dominate the planet. Eventually anoxygenic and oxygenic photosynthesis oxidized much of the Earth’s crust and supplied sulphate to the ocean. Anoxygenic photosynthesis remained important until there was enough O2 in downwelling seawater to quantitatively oxidize massive sulphides at ridge axes.
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Apr. 30 |
Stefanie MilamFollowing Carbon's Evolutionary Path from Nucleosynthesis to the the Solar System |
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Observations at millimeter/submillimeter wavelengths of various species can be used to trace the cyclic nature of molecular material, specifically carbon-based, throughout stellar evolution. Studies have shown that the carbon isotopic composition of the interstellar medium suggest a strong dependence upon nearby evolved stars and distance to the Galactic center. However, this can also be affected by the chemical composition, carbon-rich or oxygen-rich, and evolutionary status of these old stars. Observations have recently shown that oxygen-rich circumstellar envelopes have a more complex carbon-chemistry than once considered and may have played a role in interstellar carbon enrichment. As large stars evolve into planetary nebulae, molecular material shed from these objects has been shown to endure this highly destructive phase. Additionally, matter may survive from planetary nebulae into the diffuse interstellar medium as the inventories of both regions are now converging. Once gas and dust condense into new stars and planetary systems, the material is potentially recycled in a molecular form and on some level preserved. This is traced by the pristine composition of comets, meteors, and interplanetary dust particles. It has also been shown that comets undergo fragmentation events that release organic material into the solar system and may potentially “seed” planets for prebiotic chemistry. I will present some of these observational results and discuss laboratory experiments underway to help trace interstellar/cometary chemistry.
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May 7 |
Rusty Schweickart and Ed Lu
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May 14 |
Diane WoodenProbing the Meteorology of our Protoplanetary Disk with Cometary Mineralogy Our planetary system formed out of a rotating accretion disk of gas and dust, often called the solar nebula. In the outer disk where temperatures were cold enough to harbor ices and interstellar materials, comet nuclei accreted. Yet, comets also accreted Mg-rich crystalline silicate mineral grains that formed in the hot inner disk close to the young Sun. Hence, cometary Mg-rich crystalline silicates are the touchstone for radial transport of grains that formed in the inner protoplanetary disk out to the comet-forming zone. Mg-rich crystalline silicate minerals are the expected condensates from the "arid" canonical solar nebula, i.e., condensates from a gas of solar composition. In comparison to Mg-rich crystalline silicates, Fe-rich crystalline silicates are recently discovered in Stardust Mission return samples from comet 81P/Wild 2 and in the Deep Impact coma of comet 9P/Tempel 1. We discuss how Fe-rich crystalline silicates, as well as phyllosilicates (aqueous minerals) can form in more "humid" weather conditions (higher oxygen fugacity) than Mg-rich crystalline silicates. The inward migration of cometesimals (small icy bodies) can raise the humidity of the solar nebula and allow these more oxidized minerals to condense. By comparing the relative abundances of Mg- and Fe-rich crystalline silicates in comets with those in chondrites (asteroidal samples), and by looking at recent dating of chondrules, we derive a picture of the solar nebula as initially arid that then suffers fluctuating epochs of humid weather by 0.6 Myr to 3Myr after the formation of the first condensates. Cometary mineralogy probes the meterology of the solar nebula. This idea that fluctuating solar nebula "weather" caused the formation of a variety of recently discovered cometary materials challenges recent assertions that cometary Fe-rich crystalline silicates, carbonates, and phyllosilicates are aqueously altered asteroidal materials (selective tiny bits of asteroids that were accreted by comets), or products of selective aqueous alteration on submicron scales in comet nuclei. Instead, if comets do not contain aqueous alteration products from asteroids, then cometary dust grains that formed in the disk are pre-accretionary with respect to asteroids. If comets contain pre-accretionary nebular grains then comets indeed probe the earliest planet-forming processes. Comets contain both the interstellar ingredients for and the products of transmutation in the inner nebula.
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May 21 |
Sienny ShangJets and Outflows from Young Stars: How They Help Shape the Early Solar SystemJets and outflows from young forming stars are among the most spectacular and energetic phenomena in the night sky. They are ubiquitous in star forming regions, and signal the birth of stars like our own. Similar phenomena exist around new higher massive stars, compact objects, and even black holes. They may differ in dynamics, energetics or emission mechanisms, yet they share the striking similarities in their highly-collimated appearance and high-velocity outflowing motion of gas. Jets and outflows play important roles in the early lives of a newborn star and help shape the early evolution of a young forming planetary system. We review status of theoretical modeling from the point of view of young stellar objects, and the multiwavelength observations of the outflow phenomena. We discuss emission mechanisms of jets and the formation of molecular outflows at the interface of theoretical interpretation and observational confrontations. We present synthetic images from the X-Wind models at the highest-angular resolution as an atlas for future planning of observations. We will touch on the connection of the highly collimated jets to the earliest processing of planetary material, and the large-scale transportation and mixing events that have been inferred to exist from the Stardust return mission. |
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May 28 |
William S. MarshallAn Insider's View of NASA Ames Lunar Skunkworks
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June 2008 |
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June 4 |
Robert SmithLiverpool Telescope: Development and science results from a fully autonomous common-user telescope
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June 11 |
Prof. Donald A. Glaser, UC Berkeley (Nobel Prize in Physics, 1960 for the invention of the "bubble chamber")The Role of Cortical Noise in Brain Function
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June 18 |
Mario Parente, Department of Electrical Engineering, Stanford University and SETI InstituteExploratory data analysis of planetary hyperspectral datasets - use of
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June 25 |
Jon Rask and Erin Tranfield:Toxicological effects of moon dust - how humans will react in the lunar environment
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July 2 |
Greg Delory, Space Sciences Laboratory, UC BerkeleyAn Electromagnetic Sounder to Detect Subsurface Liquid Water on Mars: Field Test Results
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July 9 |
Jessica Marquez, NASA Ames Research CenterPeople and Automation: Implications for Long Duration Lunar and Planetary Exploration
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July 16 |
Eli Silver, UC Santa Cruz, Earth and Planetary SciencesCreation and Destruction of Continental Crust at Subduction Zones
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July 30 |
Josh Emery, SETI Institute
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Aug. 6 |
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