A study of the optical rotation of lipids extracted from soils, sediments, and the orgueil carbonaceous meteorite.
نویسنده
چکیده
During the past few years a considerable amount of information has been accumulated on the optical rotatory dispersion of biologically significant compounds. Optical rotatory dispersion data has, in several instances, been useful in elucidating structural details of molecules, such as those of certain proteins. The optical rotations of several lipid and hydrocarbon compounds are also known. On the other hand, there is very little information available on the optical rotation of lipids which occur in soils, marine sediments, and sedimentary rocks. There are some exceptions, such as petroleum and coal. The optical rotations of petroleum distillate fractions and of coal have been studied.'-4 It was found that most petroleum fractions are dextrorotatory but a few show levorotation.2 The chemical composition of lipids in soils and sediments has also been studied,5-7 and fatty acids, saturated and aromatic hydrocarbons, and so on have been described. An investigation of the optical rotations of soil and sediment lipids may eventually be helpful to elucidate some of the transformation processes that the decayed biological matter is subjected to in the geological habitat. A study of the optical activity of soil and sediment lipids may also be of value in explaining the true nature of the optical activity reported in lipid fractions extracted from carbonaceous meteorites.8-"1 The following three topics are discussed in this report: (1) control experiments performed in order to evaluate various factors that may cause false optical activity readings, (2) optical activity measurements made on soil and sediment, and (3) optical activity measurements on carbonaceous meteorite lipids. Necessary Precautions for the Measurement of the Optical Rotation of Soil, Sediment, and Meteorite Lipids.-The measurement of the optical rotation of soil, sediment, and meteorite lipids is a most difficult task which can be successfully accomplished only if utmost care is exercised. The lipids are usually extracted from the sediment samples with a solution of benzene and methanol in a Soxhlet apparatus. The extracts are usually yellow to dark brown in color. They may contain suspended particulate matter and they usually show only a few millidegrees of optical rotation. Investigators working on problems of optical rotatory dispersion will, of course, realize that such samples could easily give spurious readings in all commercially available polarimeters unless the necessary precautions are taken. The major part of this study consisted of control experiments in order to define the factors that may lead to spurious rotations and to establish precisely the precautional procedures which one has to follow to avoid artifacts. In this study, a modified Bendix model 460-C Polarmatic Recording Spectropolarimeter was used. A series of control experiments were performed to evaluate the instrument in order to find out if it was indeed suitable for this study. The effects of the optical density of the solutions, suspended particulate matter, and the fluorescence of the solutions were studied in detail, together with such possible sources of
منابع مشابه
Optical ActivitY in the Orgueil Meteorite.
Nagy's report of an optical rotation of-0.023 degrees to -0.084 degrees in the Orgueil meteorite has not been confirmed. The highest rotation found in several fatty-acid and hydrocarbon fractions isolated from the meteorite was -0.002 degrees , less than that of optically inactive controls. The "rotations" observed by Nagy may have been caused by scattered depolarized light from colloidal parti...
متن کاملA contamination assessment of the CI carbonaceous meteorite Orgueil using a DNAdirected approach
The Orgueil meteorite has become one of the most well-studied carbonaceous meteorites, after it fell in France 150 yr ago. Extraterrestrial organic compounds such as amino acids and nucleobases in the parts per billion ranges were identified in Orgueil samples with supporting isotopic analyses. However, speculations of terrestrial contamination such as organic inclusions in the form of microbes...
متن کاملEnrichment of the amino acid L-isovaline by aqueous alteration on CI and CM meteorite parent bodies.
The distribution and enantiomeric composition of the 5-carbon (C(5)) amino acids found in CI-, CM-, and CR-type carbonaceous meteorites were investigated by using liquid chromatography fluorescence detection/TOF-MS coupled with o-phthaldialdehyde/N-acetyl-L-cysteine derivatization. A large L-enantiomeric excess (ee) of the alpha-methyl amino acid isovaline was found in the CM meteorite Murchiso...
متن کاملSpatial Relations between D/h and N Isotopic Anomalies in Orgueil and Murchison Insoluble Organic Matter: a Nanosims Study
Introduction: Most of the organic carbon in Carbonaceous Chondrites (CC) is in the form of Insoluble Organic Matter (IOM). Isotopically, the IOM in CC appears to be highly un-equilibrated: discrete H and N isotopic anomalies-the so-called hotspots-with δ values up to +19400‰ and +1770‰, respectively, are embedded in the bulk IOM, which has average compositions that are lower by a maximum one or...
متن کاملOrigin and Distribution of Clay Minerals in Calcareous, Gypsiferous, Saline Soils and Sediments of Bakhtegan Lake Bank, Southern Iran
Pedogenesis and clay mineralogy of soils and rock samples were studied in a transect of calcareous, gypsiferous, saline soils and sediments of Bakhtegan lake bank in southern Iran. The main objectives of study were to determine the occurrence of clay minerals and factors controlling their distribution pattern and relative abundance in soils and parent materials. The soil parent material is high...
متن کاملذخیره در منابع من
با ذخیره ی این منبع در منابع من، دسترسی به آن را برای استفاده های بعدی آسان تر کنید
برای دانلود متن کامل این مقاله و بیش از 32 میلیون مقاله دیگر ابتدا ثبت نام کنید
ثبت ناماگر عضو سایت هستید لطفا وارد حساب کاربری خود شوید
ورودعنوان ژورنال:
- Proceedings of the National Academy of Sciences of the United States of America
دوره 56 2 شماره
صفحات -
تاریخ انتشار 1966