Chemical and isotopic properties of kukersites from Iowa and Estonia
- 31 October 2003
- journal article
- Published by Elsevier in Organic Geochemistry
- Vol. 34 (10) , 1419-1427
- https://doi.org/10.1016/s0146-6380(03)00138-4
Abstract
No abstract availableThis publication has 32 references indexed in Scilit:
- The chemical structure of Gloeocapsomorpha prisca microfossils: implications for their originGeochimica et Cosmochimica Acta, 2001
- Evidence for a widespread carbon isotopic event associated with late Middle Ordovician sedimentological and faunal changes in EstoniaGeological Magazine, 1999
- New guidelines for reporting stable hydrogen, carbon, and oxygen isotope-ratio dataGeochimica et Cosmochimica Acta, 1996
- Carbon isotopic evidence for the origin of macromolecular aliphatic structures in kerogenOrganic Geochemistry, 1994
- Spectroscopic features of Gloeocapsomorpha prisca colonies and of interstitial matrix in kukersite as revealed by transmission micro-FT-i.r.: location of phenolic moietiesFuel, 1994
- Similar morphological and chemical variations of Gloeocapsomorpha prisca in Ordovician sediments and cultured Botryococcus braunii as a response to changes in salinityOrganic Geochemistry, 1992
- Unique distributions of hydrocarbons and sulphur compounds released by flash pyrolysis from the fossilised alga Gloeocapsomorpha prisca, a major constituent in one of four Ordovician kerogensGeochimica et Cosmochimica Acta, 1991
- Characterization of Estonian Kukersite by spectroscopy and pyrolysis: Evidence for abundant alkyl phenolic moieties in an Ordovician, marine, type II/I kerogenOrganic Geochemistry, 1990
- Fluorescence of sedimentary organic matter in relation to its chemical compositionOrganic Geochemistry, 1986
- Carbon isotope composition of lower palaeozoic kerogen: Effects of maturationOrganic Geochemistry, 1986