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== Natural preservation in fossils == |
== Natural preservation in fossils == |
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[[File:CholestaneDiagenesis3.png|thumb|''Cholesterol degrades to cholestane by loss of OH functional group and saturation of double bond (indicated in pink). Stereochemistry of the molecule is maintained in this degradation.'']] |
[[File:CholestaneDiagenesis3.png|thumb|''Cholesterol degrades to cholestane by loss of OH functional group and saturation of double bond (indicated in pink). Stereochemistry of the molecule is maintained in this degradation.'']] |
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Cholesterol has 256 [[Stereoisomerism|stereoisomers]], but only one of them is formed naturally in production of cholesterol (3β-ol, 5α (H), 14α (H), 17α (H), 20R) and is therefore the primary stereoisomer of interest for cholestane measurements. Deviations from this stereochemistry often reflects [[diagenesis]], thermal maturation and [[preservation bias]]. |
Cholesterol has 256 [[Stereoisomerism|stereoisomers]], but only one of them is formed naturally in production of cholesterol (3β-ol, 5α (H), 14α (H), 17α (H), 20R) and is therefore the primary stereoisomer of interest for cholestane measurements. Deviations from this stereochemistry often reflects [[diagenesis]], thermal maturation and [[Taphonomy|preservation bias]]. |
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[[Diagenesis]] typically leads to the loss of functional groups and double bonds in organic molecules. For cholestane specifically, diagenesis of cholesterol to cholestane produces a molecule that is fully saturated compared to its [[steroid]] counterpart. This process occurs without the loss or gain of carbon atoms and therefore can serve as an indicator of the original steroid produced by the organism in the environment.<ref>{{Cite journal|last1=Grantham|first1=P.J.|last2=Wakefield|first2=L.L.|date=January 1988|title=Variations in the sterane carbon number distributions of marine source rock derived crude oils through geological time|journal=Organic Geochemistry|volume=12|issue=1|pages=61–73|doi=10.1016/0146-6380(88)90115-5|bibcode=1988OrGeo..12...61G |issn=0146-6380}}</ref> |
[[Diagenesis]] typically leads to the loss of functional groups and double bonds in organic molecules. For cholestane specifically, diagenesis of cholesterol to cholestane produces a molecule that is fully saturated compared to its [[steroid]] counterpart. This process occurs without the loss or gain of carbon atoms and therefore can serve as an indicator of the original steroid produced by the organism in the environment.<ref>{{Cite journal|last1=Grantham|first1=P.J.|last2=Wakefield|first2=L.L.|date=January 1988|title=Variations in the sterane carbon number distributions of marine source rock derived crude oils through geological time|journal=Organic Geochemistry|volume=12|issue=1|pages=61–73|doi=10.1016/0146-6380(88)90115-5|bibcode=1988OrGeo..12...61G |issn=0146-6380}}</ref> |
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Latin: A a Á á À à  â Ä ä Ǎ ǎ Ă ă Ā ā à ã Å å Ą ą Æ æ Ǣ ǣ B b C c Ć ć Ċ ċ Ĉ ĉ Č č Ç ç D d Ď ď Đ đ Ḍ ḍ Ð ð E e É é È è Ė ė Ê ê Ë ë Ě ě Ĕ ĕ Ē ē Ẽ ẽ Ę ę Ẹ ẹ Ɛ ɛ Ǝ ǝ Ə ə F f G g Ġ ġ Ĝ ĝ Ğ ğ Ģ ģ H h Ĥ ĥ Ħ ħ Ḥ ḥ I i İ ı Í í Ì ì Î î Ï ï Ǐ ǐ Ĭ ĭ Ī ī Ĩ ĩ Į į Ị ị J j Ĵ ĵ K k Ķ ķ L l Ĺ ĺ Ŀ ŀ Ľ ľ Ļ ļ Ł ł Ḷ ḷ Ḹ ḹ M m Ṃ ṃ N n Ń ń Ň ň Ñ ñ Ņ ņ Ṇ ṇ Ŋ ŋ O o Ó ó Ò ò Ô ô Ö ö Ǒ ǒ Ŏ ŏ Ō ō Õ õ Ǫ ǫ Ọ ọ Ő ő Ø ø Œ œ Ɔ ɔ P p Q q R r Ŕ ŕ Ř ř Ŗ ŗ Ṛ ṛ Ṝ ṝ S s Ś ś Ŝ ŝ Š š Ş ş Ș ș Ṣ ṣ ß T t Ť ť Ţ ţ Ț ț Ṭ ṭ Þ þ U u Ú ú Ù ù Û û Ü ü Ǔ ǔ Ŭ ŭ Ū ū Ũ ũ Ů ů Ų ų Ụ ụ Ű ű Ǘ ǘ Ǜ ǜ Ǚ ǚ Ǖ ǖ V v W w Ŵ ŵ X x Y y Ý ý Ŷ ŷ Ÿ ÿ Ỹ ỹ Ȳ ȳ Z z Ź ź Ż ż Ž ž ß Ð ð Þ þ Ŋ ŋ Ə ə
Greek: Ά ά Έ έ Ή ή Ί ί Ό ό Ύ ύ Ώ ώ Α α Β β Γ γ Δ δ Ε ε Ζ ζ Η η Θ θ Ι ι Κ κ Λ λ Μ μ Ν ν Ξ ξ Ο ο Π π Ρ ρ Σ σ ς Τ τ Υ υ Φ φ Χ χ Ψ ψ Ω ω {{Polytonic|}}
Cyrillic: А а Б б В в Г г Ґ ґ Ѓ ѓ Д д Ђ ђ Е е Ё ё Є є Ж ж З з Ѕ ѕ И и І і Ї ї Й й Ј ј К к Ќ ќ Л л Љ љ М м Н н Њ њ О о П п Р р С с Т т Ћ ћ У у Ў ў Ф ф Х х Ц ц Ч ч Џ џ Ш ш Щ щ Ъ ъ Ы ы Ь ь Э э Ю ю Я я ́
IPA: t̪ d̪ ʈ ɖ ɟ ɡ ɢ ʡ ʔ ɸ β θ ð ʃ ʒ ɕ ʑ ʂ ʐ ç ʝ ɣ χ ʁ ħ ʕ ʜ ʢ ɦ ɱ ɳ ɲ ŋ ɴ ʋ ɹ ɻ ɰ ʙ ⱱ ʀ ɾ ɽ ɫ ɬ ɮ ɺ ɭ ʎ ʟ ɥ ʍ ɧ ʼ ɓ ɗ ʄ ɠ ʛ ʘ ǀ ǃ ǂ ǁ ɨ ʉ ɯ ɪ ʏ ʊ ø ɘ ɵ ɤ ə ɚ ɛ œ ɜ ɝ ɞ ʌ ɔ æ ɐ ɶ ɑ ɒ ʰ ʱ ʷ ʲ ˠ ˤ ⁿ ˡ ˈ ˌ ː ˑ ̪ {{IPA|}}
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