13 results match your criteria: "Carl Sagan Center for the Study of Life in the Universe[Affiliation]"

Several mass spectrometry and spectroscopic techniques have been used in the search for molecular biomarkers on Mars. A major constraint is their capability to detect and identify large and complex compounds such as peptides or other biopolymers. Multiplex immunoassays can detect these compounds, but antibodies must be produced for a large number of sequence-dependent molecular targets.

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Subaerial hydrothermal systems are of great interest for paleobiology and astrobiology as plausible candidate environments to support the origin of life on Earth that offer a unique and interrelated atmosphere-hydrosphere-lithosphere interface. They harbor extensive sinter deposits of high preservation potential that are promising targets in the search for traces of possible extraterrestrial life on Hesperian Mars. However, long-term quality preservation is paramount for recognizing biosignatures in old samples and there are still significant gaps in our understanding of the impact and extent of taphonomy processes on life fingerprints.

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Article Synopsis
  • Saturn's rings showcase the dynamics and history of the Saturn system, with insights gained from close-up observations by the Cassini spacecraft.
  • The rings exhibit detailed features created by embedded masses, banded textures, and the impact of material streams on the F ring.
  • Findings suggest that variations in the rings' structure are due to changes in particle properties rather than differences in composition.
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A review of Morlet wavelet analysis of radial profiles of Saturn's rings.

Philos Trans A Math Phys Eng Sci

August 2018

Department of Physics, University of Idaho, Moscow, ID 83844, USA.

Spiral waves propagating in Saturn's rings have wavelengths that vary with radial position within the disc. The best-quality observations of these waves have the form of radial profiles centred on a particular azimuth. In that context, the wavelength of a given spiral wave is seen to change substantially with position along the one-dimensional profile.

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Microbial pinnacles in ice-covered Lake Vanda, McMurdo Dry Valleys, Antarctica, extend from the base of the ice to more than 50 m water depth. The distribution of microbial communities, their photosynthetic potential, and pinnacle morphology affects the local accumulation of biomass, which in turn shapes pinnacle morphology. This feedback, plus environmental stability, promotes the growth of elaborate microbial structures.

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In this study, we report the distribution and abundance of cold-adaptation proteins in microbial mat communities in the perennially ice-covered Lake Joyce, located in the McMurdo Dry Valleys, Antarctica. We have used MG-RAST and R code bioinformatics tools on Illumina HiSeq2000 shotgun metagenomic data and compared the filtering efficacy of these two methods on cold-adaptation proteins. Overall, the abundance of cold-shock DEAD-box protein A (CSDA), antifreeze proteins (AFPs), fatty acid desaturase (FAD), trehalose synthase (TS), and cold-shock family of proteins (CSPs) were present in all mat samples at high, moderate, or low levels, whereas the ice nucleation protein (INP) was present only in the ice and bulbous mat samples at insignificant levels.

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Growth of modern branched columnar stromatolites in Lake Joyce, Antarctica.

Geobiology

July 2015

Carl Sagan Center for the Study of Life in the Universe, SETI Institute, Mountain View, CA, USA.

Modern decimeter-scale columnar stromatolites from Lake Joyce, Antarctica, show a change in branching pattern during a period of lake level rise. Branching patterns correspond to a change in cyanobacterial community composition as preserved in authigenic calcite crystals. The transition in stromatolite morphology is preserved by mineralized layers that contain microfossils and cylindrical molds of cyanobacterial filaments.

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Animal acoustic communication often takes the form of complex sequences, made up of multiple distinct acoustic units. Apart from the well-known example of birdsong, other animals such as insects, amphibians, and mammals (including bats, rodents, primates, and cetaceans) also generate complex acoustic sequences. Occasionally, such as with birdsong, the adaptive role of these sequences seems clear (e.

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Lake Vanda is a perennially ice-covered, closed-basin lake in the McMurdo Dry Valleys, Antarctica. Laminated photosynthetic microbial mats cover the floor of the lake from below the ice cover to >40 m depth. In recent decades, the water level of Lake Vanda has been rising, creating a "natural experiment" on development of mat communities on newly flooded substrates and the response of deeper mats to declining irradiance.

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Kepler-16: a transiting circumbinary planet.

Science

September 2011

Carl Sagan Center for the Study of Life in the Universe, SETI Institute, 189 Bernardo Avenue, Mountain View, CA 94043, USA.

We report the detection of a planet whose orbit surrounds a pair of low-mass stars. Data from the Kepler spacecraft reveal transits of the planet across both stars, in addition to the mutual eclipses of the stars, giving precise constraints on the absolute dimensions of all three bodies. The planet is comparable to Saturn in mass and size and is on a nearly circular 229-day orbit around its two parent stars.

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Discovery of large conical stromatolites in Lake Untersee, Antarctica.

Geobiology

May 2011

Carl Sagan Center for the Study of Life in the Universe, SETI Institute, Mountain View, CA, USA.

Lake Untersee is one of the largest (11.4 km(2)) and deepest (>160 m) freshwater lakes in East Antarctica. Located at 71°S the lake has a perennial ice cover, a water column that, with the exception of a small anoxic basin in the southwest of the lake, is well mixed, supersaturated with dissolved oxygen, alkaline (pH 10.

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Hundreds of impact craters on Mars contain diverse phyllosilicates, interpreted as excavation products of preexisting subsurface deposits following impact and crater formation. This has been used to argue that the conditions conducive to phyllosilicate synthesis, which require the presence of abundant and long-lasting liquid water, were only met early in the history of the planet, during the Noachian period (> 3.6 Gy ago), and that aqueous environments were widespread then.

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Energy transduction inside of amphiphilic vesicles: encapsulation of photochemically active semiconducting particles.

Orig Life Evol Biosph

April 2009

Carl Sagan Center for the Study of Life in the Universe, SETI Institute, Mountain View, USA.

Article Synopsis
  • Amphiphilic bilayer membranes, or vesicles, may have formed naturally on prebiotic Earth, potentially serving as the first compartments for the origin of life by containing and concentrating substances.
  • An important question in understanding the origin of life is how energy from light could be harnessed before complex enzymes evolved, with the hypothesis that vesicles developed the ability to capture and use light energy for chemical reactions.
  • Research indicates that encapsulating colloidal semiconducting particles, like TiO2, within vesicles can create conditions for energy transduction and facilitate early chemical processes, acting as a model for primitive photosynthesis.
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