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Friday, 30 January 2009
Stem Cell Transplant Reverses Early-stage Multiple Sclerosis
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Wednesday, 28 January 2009
Stem Cells Used to Reverse Paralysis in Animals
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Tuesday, 27 January 2009
Human iPS Cells Reprogrammed into Germ Cell Precursors
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Scientists See Progress in FDA Stem Cell Trial Approval
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Friday, 23 January 2009
Geron Get FDA Clearance for First Test of Human Embryonic Stem Cell Therapy
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Monday, 19 January 2009
Parasites in the Genome

“It is difficult to believe that the massive integration of LINE-1 and Alu sequences remained without consequences on human evolution. Thus it is surprising how little we know so far about the mechanism of retrotransposition and about the proteins and nucleic acids involved in this process“, says Oliver Weichenrieder, leading scientists at the Max Planck Institute for Developmental Biology. The researchers therefore try to gain new insights via the biochemical characterisation of the involved molecules and via the determination of their molecular structures. This provides the basis for a detailed functional analysis and reveals similarities to already known proteins, especially similarities that are not obvious from a simple comparison of the respective amino acid sequences. In the present work Elena Khazina und Oliver Weichenrieder characterize one of two proteins that are encoded by the human LINE-1 retrotransposon. This so-called L1ORF1p protein binds to LINE-1 RNA, which was transcribed from a LINE-1 element in the genomic DNA. Subsequently, L1ORF1p likely supports the following reverse transcription of LINE-1 RNA into DNA. This process happens directly at the genomic integration site of the new LINE-1 element. The researchers show that the L1ORF1p protein consists of three parts. The first part causes a self-association such that always three molecules come together to form a trimer. The other two parts are necessary for binding LINE-1 RNA. “Especially surprising was the identification of a so-called RRM domain in the middle part of the protein, since this part was believed so far to be rather unstructured”, says Elena Khazina. “Our crystal structure clearly proves the existence of this domain. Meanwhile we identified RRM-domains also in other retrotransposons, in a variety of animal and plant species“, adds the structural biologist.

RRM-domains (RNA Recognition Motif) occur frequently in the cell, particularly in RNA-binding proteins. The existence of an RRM-domain in L1ORF1p now explains why L1ORF1p binds LINE-1 RNA and how this could happen in detail. The insight into the structure of the L1ORF1p protein provides a new perspective and a good basis for future investigations of those cellular processes that are exploited by the LINE-1 element for its own propagation, and also for those mechanisms that are available to the cell to prevent the excessive propagation of retrotransposons. Reference: Non-LTR retrotransposons encode noncanonical RRM domains in their first open-reading frame. Elena Khazina, Oliver Weichenrieder PNAS, 12 January 2009, vol. 106 (3), 731-736, doi: 10.1073/pnas0809964106 ......... ZenMaster
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Large DNA Stretches, Not Single Genes, Shut Off as Stem Cells Mature
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Friday, 16 January 2009
Discovery of Methane Reveals Mars Is Not a Dead Planet
This image shows concentrations of Methane discovered on Mars. The first definitive detection of methane in the atmosphere of Mars indicates the planet is alive in the sense that it still has geologic activity powered by heat from its interior, according to a team of NASA and university scientists.
The team used spectrometer instruments attached to several telescopes to detect plumes of methane that were emitted from specific sites during the warmer seasons – spring and summer.
Though nothing conclusive can yet be determined, it is possible that the detected methane was either produced by geologic processes such as the oxidation of iron (serpentinization) or by microscopic Martian life below the planet’s surface. The methane released today could be produced currently, or it could be ancient methane trapped in ice 'cages' called clathrates or as gas below a sub-surface ice layer.
Credit: NASA/Goddard Space Flight Center Scientific Visualization Studio.
"At northern mid-summer, methane is released at a rate comparable to that of the massive hydrocarbon seep at Coal Oil Point in Santa Barbara, Calif." Mumma is lead author of a paper describing this research that will appear in Science Express on Thursday.
Methane, four atoms of hydrogen bound to a carbon atom, is the main component of natural gas on Earth. Astrobiologists are interested in these data because organisms release much of Earth's methane as they digest nutrients. However, other purely geological processes, like oxidation of iron, also release methane.
"Right now, we do not have enough information to tell whether biology or geology — or both — is producing the methane on Mars," Mumma said.
"But it does tell us the planet is still alive, at least in a geologic sense. It is as if Mars is challenging us, saying, 'hey, find out what this means.' "
If microscopic Martian life is producing the methane, it likely resides far below the surface where it is warm enough for liquid water to exist. Liquid water is necessary for all known forms of life, as are energy sources and a supply of carbon.
"On Earth, microorganisms thrive about 1.2 to 1.9 miles beneath the Witwatersrand basin of South Africa, where natural radioactivity splits water molecules into molecular hydrogen and oxygen," Mumma said.
"The organisms use the hydrogen for energy. It might be possible for similar organisms to survive for billions of years below the permafrost layer on Mars, where water is liquid, radiation supplies energy, and carbon dioxide provides carbon. Gases, like methane, accumulated in such underground zones might be released into the atmosphere if pores or fissures open during the warm seasons, connecting the deep zones to the atmosphere at crater walls or canyons."
It is possible a geologic process produced the Martian methane, either now or eons ago. On Earth, the conversion of iron oxide into the serpentine group of minerals creates methane, and on Mars this process could proceed using water, carbon dioxide and the planet's internal heat. Although there is no evidence of active volcanism on Mars today, ancient methane trapped in ice cages called clathrates might be released now.
"We observed and mapped multiple plumes of methane on Mars, one of which released about 19,000 metric tons of methane," said co-author Geronimo Villanueva of the Catholic University of America in Washington.
"The plumes were emitted during the warmer seasons, spring and summer, perhaps because ice blocking cracks and fissures vaporized, allowing methane to seep into the Martian air."
Plumes appeared over the Martian northern hemisphere regions such as east of Arabia Terra, the Nili Fossae region, and the south-east quadrant of Syrtis Major, an ancient volcano about 745 miles across.
Credit: NASA/Goddard Space Flight Center Scientific Visualization Studio.
According to the team, the plumes were seen over areas that show evidence of ancient ground ice or flowing water. Plumes appeared over the Martian northern hemisphere regions such as east of Arabia Terra, the Nili Fossae region, and the south-east quadrant of Syrtis Major, an ancient volcano about 745 miles across.
One method to test whether life produced this methane is by measuring isotope ratios. Isotopes of an element have slightly different chemical properties, and life prefers to use the lighter isotopes. A chemical called deuterium is a heavier version of hydrogen. Methane and water released on Mars should show distinctive ratios for isotopes of hydrogen and carbon if life was responsible for methane production. It will take future missions, like NASA's Mars Science Laboratory, to discover the origin of the Martian methane.
References:
Strong Release of Methane on Mars in Northern Summer 2003
Michael J. Mumma, Geronimo L. Villaneuva, Robert E. Novak, Tilak Hewagama, Boncho P. Bonev, Michael A. DiSanti, Avi M. Mandell, and Michael D. Smith
Science, Published Online January 15, 2009, DOI: 10.1126/science.1165243
Martian Methane Reveals the Red Planet is not a Dead Planet
Bill Steigerwald
NASA - 15 January 2009
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ZenMaster
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Thursday, 15 January 2009
Bone Marrow Stem Cells Regenerate Skin
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Saturday, 10 January 2009
GM Goats Make Anti-clotting Drug in Their Milk

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Friday, 9 January 2009
Growth of New Brain Cells Requires ‘Epigenetic’ Switch
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Thursday, 8 January 2009
Extra Stem Cells to Repair the Body
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Making Perfect Protein: Lost in Translation

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Converting Adult Somatic Cells to Pluripotent Stem Cells Using a Single Virus
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Wednesday, 7 January 2009
Human Genomics in China

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