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isorenieratene

 
National Institutes of Health

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2014
2014
Abstract. The Paleocene–Eocene Thermal Maximum (PETM, ~ 56 Ma) was a ~ 200 kyr episode of global warming, associated with massive… Expand
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2011
2011
Organic biomarkers in marine sedimentary rocks hold important clues about the early history of Earth's surface environment. The… Expand
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Highly Cited
2008
Highly Cited
2008
Euxinic ocean conditions accompanied significant events in Earth history, including several Phanerozoic biotic crises. By… Expand
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2008
2008
The cyclization of lycopene to gamma- or beta-carotene is a major branch point in the biosynthesis of carotenoids in… Expand
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Highly Cited
2007
Highly Cited
2007
Deep-sea sediments of the eastern Mediterranean harbour a series of dark, organic carbon-rich layers, so-called sapropels. Within… Expand
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2006
2006
Abstract Soluble and insoluble fractions of the Jet Rock sedimentary organic matter have been subjected to hydropyrolysis to… Expand
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Highly Cited
2005
Highly Cited
2005
Carotenoids are produced by a variety of organisms, but the mechanisms that regulate gene expression leading to carotenoid… Expand
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2003
2003
Abstract In sediments, the diaromatic carotenoid isorenieratene can undergo a wide range of molecular transformations, including… Expand
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Highly Cited
2000
Highly Cited
2000
Abstract The carotenogenic (crt) gene cluster from Brevibacterium linens, a member of the commercially important group of… Expand
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Highly Cited
1999
Highly Cited
1999
The biosynthesis of the aromatic carotene isorenieratene is restricted to green photosynthetic bacteria and a few actinomycetes… Expand
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