Abietane Diterpenoids As Potential Drugs

Total Page:16

File Type:pdf, Size:1020Kb

Abietane Diterpenoids As Potential Drugs 5 CATALYZER THE FIFTH ISSUE OF CATALYZER MAGAZINE 19/07/2020 ABIETANE DITERPENOIDS AS POTENTIAL DRUGS Abietanes are naturally word “turpentine”. Each isoprene occurring diterpenoids that unit also called a “C5 building haveAbietane been isolated Diterpenoids from several as Potentialblock” or Drugs hemi-terpene; they terrestrial plant families are linked to form terpenes in includingGülaçtı Topçu Lamiaceae (Labiatae), “head-to-tail” fashion, in general. Asteraceae, Celastraceae, Therefore, monoterpenes are and Boraginaceae, and resins formed from 2 isoprene units (10 Abietanes are naturally occurring diterpenoids that have been isolated from several terrestrial Sildi: which from conifers belonging to the C’s), sesquiterpenes from 3 units familiesplant families Cupressaceae, including Lamiaceae Pinaceae, (Labiatae), (15Asteraceae, C’s), diterpenes Celastraceae, fromand Boraginaceae 4 units , Podocarpaceae,and resins from conifers Phyllocladaceae, belonging to the families(20 Cupressaceae,C’s), and sesterterpenes Pinaceae, Podocarpaceae, from andPhylloclad Araucariaceae.aceae, and Araucariaceae. 5 units (25 C’s), while triterpenes Sildi: e are from 6 units (30 C’s) and Secondary metabolites metabolites of plants of can be classifiedtetraterpenes, namely as fromterpenoids 8 units and (40 steroids, Sildi: ; plantsflavonoids can and be other classified, phenolics, namelyand alkaloids, C’s). which all play an important role in their asdefense terpenoids mechanisms, and such steroids, as fighting with herbivores, pests, and pathogens as well as other Sildi: to flavonoidstypes of external and damage other. Asphenolics, one of the secondaryMono- metabolites and sesquiterpenoids of plants, terpenoids are Sildi: s and alkaloids, which all play an are the main constituents composed of isoprene (2-methyl-1,3-butadiene) units. The name "terpene" is derived from the Sildi: formed important role in their defense of the essential oils of all mechanisms,word “turpentine”. such Each isopreneas fighting unit also calledplants a “C5 building and flowers block” or and hemi they-terpene ; they Sildi: , withare linked herbivores, to form terpenes pests, in and“head -to-tail” fashion,give in them general. their Therefore, special monoterpenes smell are pathogensformed from 2 as isoprene well asunits other (10 C’s), types sesquiterpenes and taste. Diterpenoids from 3 units (15 C’s), diterpenes are from of4 units external (20 C’s), damage. and sesterterpenes As one offrom 5 unitscomposed (25 C’s), wh ofile fourtriterpenes isoprene are from units 6 units the(30 C’s) secondary and tetraterpenes metabolites from 8 unit ofs (40 C’s). with a core molecular formula Sildi: e plants, terpenoids are composed C20H32to form different skeletons, ofMono isoprene- and sesquiterpenoids (2-methyl-1,3- are the main constituentssuch as of abietane,the essential kaurane,oils of all plants and butadieneflowers and )they units. give The them name their special smell andatisane, taste. Diterpenoids labdane, jatrophane,are composed of four Sildi: which occur “terpene” is derived from the tigliane, lathyrane, or taxane. isoprene units with a core molecular formula C20H32 to form different skeletons, such as abietane, kaurane, atisane, labdane, jatrophane, tigliane, lathyrane, or taxane. Sildi: h Sildi: , etc Abietane skeleton Abietic acid Dehydroabietic acid Ferruginol Abietane diterpenoids have three 6-membered cyclic rings (trans-fused A-B, and trans-fused B-C rings) with an isopropyl side chain attached to C-13 on ring C. A simple example of them Sildi: is abietic acid (7,13-abietadien-18-oic acid), and dehydroabietic acid, which has an aromatic Sildi: The Sildi: for INTERNATIONAL CHEMISTRY OLYMPIAD MAGAZINE / ISTANBUL - TURKEY 2020 Taxodione Salvinolone 6-Hydroxysalvinolone Abietane diterpenoids have three six-membered cyclic rings (trans- Some Salvia species afforded abietane diterpenoids that have opened Taxodione Salvinolone 6-Hydroxysalvinolone fused A-B, and trans-fused B-C rings) with an isopropyl side chain ring A, which are called seco-abietanes, such as aethiopinone and Some Salvia species afforded abietane diterpenoids that have opened ring A, which are called Sildi: which attached to C-13 on ring C. A simple example of them is abietic acid salvipisone [2,8]. (7,13-abietadien-18-oic acid), and dehydroabietic acid, which has seco-abietanes, such as aethiopinone and salvipisone [2,8]. Some Salvia species afforded abietane diterpenoids that have opened ring A, which are called Sildi: which an aromatic ring C, previously obtained during chemical studies starting from abietic acid. Another simple abietane diterpene withseco the -abietanes, such as aethiopinone and salvipisone [2,8]. aromatic ring C is ferruginol, first isolated in 1939 from the resin of thering miro C, previouslytree (Podocarpus obtained ferrugineus during chemical) endemic studies to starting New Zealandfrom abietic [1]. acid. Another simple abietane diterpene with the aromatic ring C is ferruginol, first isolated in 1939 from the resin Aromatic abietanes comprise the largest group of naturally occurring abietanesof the miro [1] t reeand (Podocarpus are the main ferr secondaryugineus) endemic metabolites to New ofZealand the Salvia [1]. Sildi: M Sildi: h L. (sage) plants belonging to the family Lamiaceae. The genus Salvia Aethiopinone Salvipisone Aromatic abietanes comprise the largest group of naturally occurring abietanes [1] and are the Sildi: species is represented by over 900 species throughout the world, and the bestmain known secondary Salvia metabolites species are of the S. miltiorrhizaSalvia L. (sage) (Danshen plants belonging or Tanshen) to the in family Lamiaceae. Sildi:Aethiopinone the Salvipisone China and other Asian countries, S. officinalis L. in Europe (sage), and Sildi: The genus Salvia is represented by over 900 species throughout the worldThe, and most theThe bestinteresting most known interesting re-arranged re-arranged abietanes abietanes were obtained were obtainedfrom endemic from Anatolian Salvia Sildi: M S. fruticosa Mill. (syn: S. triloba L.) in Mediterranean countries, and S. Sildi: d endemic Anatolian Salvia species, such as S. microstegia Boiss. et M divinorumSalvia species L., a hallucinogenicare S. miltiorrhiza species, (Dansh enwhose or Tanshen) origin indates China back and tootherspecies Thethe Asian m,ost such couinteresting ntriesas S., S.microstegia re-arrangedSildi: (BrandtBoiss. abietanes ve etNeubauer Bal were. 1939)grow obtaineding in fromthe Binboğaendemic MountainsAnatolian Salvia(Turkey) , Sildi: Sildi: n Bal. growing in the Binboğa Mountains (Turkey), which afforded a Mazatecofficinalis hallucinogenic L. in Europe sage.(sage), Most and SalviaS. fruticosa species Mill. are (syn: rich S. in triloba abietanespecies L.) in , Mediterraneansuch as S. microstegia Sildi: Boiss. family et Bal. growing in the Binboğa Mountains (Turkey), Sildi: n which affordedrearranged a rearranged tricyclic abietanetricyclic diterpene.abietane diterpene. Its structure Its structurewas elucidated was elucidated by a diterpenoids, while S. divinorum is rich in neo-clerodane diterpenoids. Sildi: most countries, and S. divinorum L., a hallucinogenic species, whose originwhich dates affordedby back a series toa rearrangedthe of NMR techniques,tricyclic 1abietane such 13asditerpene. 1H and 13ItsC NMR,structure COSY was elucidated by a In Turkey, Salvia species are represented by over 100 species (114series of NMR techniques, Sildi:such h as H and C NMR, COSY and 1D-NOE and SINEPT taxa),Mazatec and hallucinogenichalf of them are sage endemic. Most Salvia to Anatolia species (Asian are rich part in abietane of Turkey). seriesditerpenoids ofand NMR ,1D-NOE while techniques, S. and SINEPT such a experimentss 1H and 13C asNMR, well COSYas HRMS and analysis. 1D-NOE and SINEPT experimentsExamination as well as of HRMS its unusualSildi: analysis. Mediterra carbonnian Examination skeleton ofsuggested its unusual that carbon this skeleton suggested divinorum is rich in neo-clerodane diterpenoids. In Turkey, Salvia speciesexperiments are represented as well by as HRMSSildi: analysis. hallusinogenic Examination of its unusual carbon skeleton suggested During our group studies on Salvia species by Prof. Ulubelen and that this compound might be derived biogenetically fromfrom regularregular abietane abietane diterpene having a Sildi: its byover Prof. 100 Topcu, species over (114 140 taxa) abietane, and half diterpenoids of them are endemic were isolated to Anatolia (Asianthat this part diterpenecompound of Turkey ).havingmight be a threederived six-membered biogenetically Cfrom skeleton regular by abietane ring A diterpene having a three–six-membered C skeletonSildi: of theby ring A cleavage between C-4 and C-5, followed by Sildi: [2,7], at least half of them being new, and most ofring them C, previouslyhave an obtainedcleavage during chemical between studies C-4 and starting C-5, followed from abietic by recyclization acid. Another of sim C-4ple three–six-membered C skeletonSildi: beingby ring A cleavage between C-4 and C-5, followed by Sildi: Sildi: aromaticDuring ourring group C. Their studies structures on Salvia were species elucidated by Prof. basedUlubelen on and 1D- by and recyclizationProf. Topcu,to C-11. overof C Therefore, -1440 to C-11. the Th finalerefore, product, the final named product microstegiol,, named microstegiol with a , with a seven- abietane diterpene with the aromatic ring C is ferruginol, first isolated in 1939 from the resin Sildi: 2D-NMRabietane and diterpenoids
Recommended publications
  • G. Staccioli, G. Menchi, U. Matteoli, R. Seraglia & P. Traldi
    Flora Mediterranea 6 - 1996 113 G. Staccioli, G. Menchi, U. Matteoli, R. Seraglia & P. Traldi Chemotaxonomic observations on some pliocenic woods from Arno Basin and fossil forest ofDunarobba (ltaly) Abstract Staccioli, G., Menchi, G., Matteoli, U., Seraglia, R. & Traldi, P.: Chemotaxonomic observations on some pliocenic woods from Amo Basin and fossil forest of Dunarobba (ltaiy). - Fl. Medit. 6: 113-117. 1996 - ISSN I 120-4052. A new fossil wood from a lignite quarry in the Amo basin was examined for its terpene contenI. It was characterised by the lack of smell on comparison with two previous samplcs. Analysis has shown several components of diterpenes (abietanc, abietatriene, a-phyllocladanc and simonellite) and only traces of sesquiterpenes in common with thc previous samples. Comparison of ali analysed samples with others from thc fossil forest of Dunarobba shows the occurrence of many shared components especially diterpenes. It is conc!udcd that Taxodioxy/on I?ypsaceum, the first species described from Dunarobba's forest, is probably the species which has given rise to the lignite of the Amo basino Introduction The first step in naming a living trec, as well as its geological remains, namely fossil woods, is givcn by botanical identification. This operation is carried out utilising several anatomical features characteristic for the species. However, in some cascs these features are lacking, so that the use of chemotaxonomy is required. Chemical compounds of taxonomic value include secondary componcnts of wood such as Iignans, tcrpcnes, phenols, etc. (Erdtman 1952). Recently, some fossil softwoods werc cxamincd for their terpene components. The first fossil wood was from the fossil forest of Dunarobba and was identified as Taxodioxylon gypsaceum by Biondi & Brugiapaglia (1991).
    [Show full text]
  • Title the Chemistry on Diterpenoids in 1965 Author(S)
    View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Kyoto University Research Information Repository Title The Chemistry on Diterpenoids in 1965 Author(s) Fujita, Eiichi Bulletin of the Institute for Chemical Research, Kyoto Citation University (1966), 44(3): 239-272 Issue Date 1966-10-31 URL http://hdl.handle.net/2433/76121 Right Type Departmental Bulletin Paper Textversion publisher Kyoto University The Chemistry on Diterpenoids in 1965 Eiichi FuJITA* (FujitaLaboratory) ReceivedJune 20, 1966 I. INTRODUCTION Several reviews on diterpenoids have been published.*2 Last year, the author described the chemistry on diterpenoids in 1964 in outline.'7 The present review is concerned with the chemical works on diterpenoids in 1965. The classification consists of abietanes, pimaranes, labdanes, phyllocladanes, gibbanes, diterpene alkaloids, and the others. 1617 151613 2016 2©' 10gII 14 56.7 4®20 I20ei317115118 191 1819 14]5 18 19 AbietanePimaraneLabdane 20its1744a 13 4U15 36 15, 2.®7 110 ®® 18 199 8 PhyllocladaneGibbane II. ABIETANE AND ITS REOATED SKELETONS Lawrence et al.27 isolated palustric acid (2) from gum rosin. The selective crystallization of its 2,6-dimethylpiperidine salt, which precipitated from acetone solution of the rosin, from methanolacetone (1:1) was effective for isolation. The four conjugated dienic resin acids, namely, levopimaric (1), palustric (2), neoabietic (3), and abietic acid (4) were treated with an excess of potassium t- butoxide in dimethyl slufoxide solution at reflux temperature (189°) for 2 minutes.37 All four solutions then exhibited a single major peak in their U.V. spectra charac- teristic of abietic acid.
    [Show full text]
  • Hydrotreating of Tall Oils on a Sulfided Nimo Catalyst for the Production Of
    IENCE SC • VTT SCIENCE • T S E Hydrotreating of tall oils on a sulfided NiMo catalyst N C O H I N for the production of base-chemicals in steam S O I V Dissertation L • crackers O S G T 83 Y H • R G The technology development for the production of value-added I E L S H 83 E G A I R chemicals from biomass through various thermo-chemical H C approaches is more demanding than ever. Renewable feedstocks H appear as the best starting materials to achieve these developments in an industrial perspective. Tall oil, the by-product of kraft-pulping process is already well-known as a sustainable and low cost feedstock. Hydrotreating of tall oils on a sulfided NiMo catalyst for... This research thesis validates the potential of tall oil as a renewable feedstock for the production of base-chemicals, especially olefins, as conceived in the thermo-chemical bio-refinery concept. The focus was on the use of hydrotreating and steam cracking technologies with different tall oil feedstocks. Particular advances were accomplished in terms of technology development for high yield of ethylene from a complex and challenging bio-feedstock, such as tall oil. Hydrotreating of tall oils on a sulfided NiMo catalyst for the production of base-chemicals in ISBN 978-951-38-8239-6 (Soft back ed.) ISBN 978-951-38-8240-2 (URL: http://www.vtt.fi/publications/index.jsp) steam crackers ISSN-L 2242-119X ISSN 2242-119X (Print) ISSN 2242-1203 (Online) Jinto Manjaly Anthonykutty VTT SCIENCE 83 Hydrotreating of tall oils on a sulfided NiMo catalyst for the production of base- chemicals in steam crackers Jinto Manjaly Anthonykutty VTT Technical Research Centre of Finland Ltd Thesis for the degree of Doctor of Technology to be presented with due permission of the School of Chemical Technology for public examination and criticism in Auditorium KE2 at Aalto University School of Chemical Technology (Espoo, Finland) on the 24th of April, 2015, at 12.00.
    [Show full text]
  • Determination of Molecular Signatures of Natural and Thermogenic Products in Tropospheric Aerosols - Input and Transport
    AN ABSTRACT OF THE THESIS OF Laurel J. Standley for the degree of Doctor of Philosophy in Oceanography presented on June 12, 1987. Title: Determination of Molecular Signatures of Natural and Thermogenic Products in Tropospheric Aerosols - Input and Transport Redacted for Privacy Abstract approved: Bernd R.Y. Simoneit A cheniotaxonomic study of natural compounds and their thermally altered products in rural and smoke aerosols within Oregon is pre- sented. Correlation with source vegetation provided information on the formation of aerosols and their transport. Distributions and concentrations of straight-chain homologous series such as n- alkanes, n-alkanoic acids, n-alkan-2-ones, n-alkanols and n-alkanals were analyzed in rural aerosols, aerosols produced by prescribed burning and residential wood combustion, and extracts of source vegetation. Cyclic di- and triterpenoids were also examined. The latter components provided more definitive correlations between source vegetation and aerosols. Results included: (1) an increase in Cmax in regions of warmer climate; (2) possible correlation of aerosols with source vegetation 100 km to the east; (3) the tracing of input from combustion of various fuels such as pine, oak and alder in aerosols produced by residential wood combustion; and (4) preliminary results that demonstrate a potentially large input of thermally altered diterpenoids via direct deposition rather than diagenesis of unaltered sedimentary diterpenoids. CCopyright by Laurel J. Standley June 12, 1987 All rights reserved DETERMINATION OF MOLECULAR SIGNATURES OF NATURAL AND THERMOGENIC PRODUCTS IN TROPOSPHERIC AEROSOLS - INPUT AND TRANSPORT by Laurel 3. Standley A THESIS submitted to Oregon State University in partial fulfillment of the requirements for the degree of Doctor of Philosophy Completed June 12, 1987 Commencement June, 1988 APPROVED: Redacted for Privacy Dr.
    [Show full text]
  • Geochemical Characterization of the Eocene Coal-Bearing Source
    minerals Article Geochemical Characterization of the Eocene Coal-Bearing Source Rocks, Xihu Sag, East China Sea Shelf Basin, China: Implications for Origin and Depositional Environment of Organic Matter and Hydrocarbon Potential Xiong Cheng 1,2,* , Dujie Hou 1,2,*, Xinhuai Zhou 3, Jinshui Liu 4, Hui Diao 4 and Lin Wei 1,2 1 School of Energy Resources, China University of Geosciences, Beijing 100083, China; [email protected] 2 Key Laboratory of Marine Reservoir Evolution and Hydrocarbon Accumulation Mechanism, Ministry of Education, Beijing 100083, China 3 Hainan Branch of China National Offshore Oil Corporation, Haikou 570100, China; [email protected] 4 Shanghai Branch of China National Offshore Oil Corporation, Shanghai 200050, China; [email protected] (J.L.); [email protected] (H.D.) * Correspondence: [email protected] (X.C.); [email protected] (D.H.) Abstract: Eocene coal-bearing source rocks of the Pinghu Formation from the W-3 well in the western margin of the Xihu Sag, East China Sea Shelf Basin were analyzed using Rock-Eval pyrolysis and gas Citation: Cheng, X.; Hou, D.; Zhou, chromatography–mass spectrometry to investigate the samples’ source of organic matter, depositional X.; Liu, J.; Diao, H.; Wei, L. environment, thermal maturity, and hydrocarbon generative potential. The distribution patterns of Geochemical Characterization of the n-alkanes, isoprenoids and steranes, high Pr/Ph ratios, abundant diterpanes, and the presence of non- Eocene Coal-Bearing Source Rocks, hopanoid triterpanes indicate predominant source input from higher land plants. The contribution of Xihu Sag, East China Sea Shelf Basin, aquatic organic matter was occasionally slightly elevated probably due to a raised water table.
    [Show full text]
  • Chemical Composition of Lipophilic Bark Extracts from Pinus Pinaster and Pinus Pinea Cultivated in Portugal
    applied sciences Article Chemical Composition of Lipophilic Bark Extracts from Pinus pinaster and Pinus pinea Cultivated in Portugal Joana L. C. Sousa 1,2,† , Patrícia A. B. Ramos 1,2,† , Carmen S. R. Freire 1, Artur M. S. Silva 2 and Armando J. D. Silvestre 1,* 1 CICECO, Department of Chemistry, University of Aveiro, 3810-193 Aveiro, Portugal; [email protected] (J.L.C.S.); [email protected] (P.A.B.R.); [email protected] (C.S.R.F.) 2 QOPNA, Department of Chemistry, University of Aveiro, 3810-193 Aveiro, Portugal; [email protected] * Correspondence: [email protected]; Tel.: +351-234-370-711; Fax: +351-234-370-084 † Both authors contributed equally to this work. Received: 25 November 2018; Accepted: 8 December 2018; Published: 11 December 2018 Abstract: The chemical composition of lipophilic bark extracts from Pinus pinaster and Pinus pinea cultivated in Portugal was evaluated using gas chromatography-mass spectrometry. Diterpenic resin acids were found to be the main components of these lipophilic extracts, ranging from 0.96 g kg−1 dw in P. pinea bark to 2.35 g kg−1 dw in P. pinaster bark. In particular, dehydroabietic acid (DHAA) is the major constituent of both P. pinea and P. pinaster lipophilic fractions, accounting for 0.45 g kg−1 dw and 0.95 g kg−1 dw, respectively. Interestingly, many oxidized compounds were identified in the studied lipophilic extracts, including DHAA-oxidized derivatives (7-oxo-DHAA, 7α/β-hydroxy-DHAA, and 15-hydroxy-DHAA, among others) and also terpin (an oxidized monoterpene). These compounds are not naturally occurring compounds, and their formation might occur by the exposure of the bark to light and oxygen from the air, and the action of micro-organisms.
    [Show full text]
  • Stable Carbon Isotopes of C3 Plant Resins and Ambers Record Changes in Atmospheric Oxygen Since the Triassic
    Available online at www.sciencedirect.com ScienceDirect Geochimica et Cosmochimica Acta 121 (2013) 240–262 www.elsevier.com/locate/gca Stable carbon isotopes of C3 plant resins and ambers record changes in atmospheric oxygen since the Triassic Ralf Tappert a,b,⇑, Ryan C. McKellar a,c, Alexander P. Wolfe a, Michelle C. Tappert a, Jaime Ortega-Blanco c,d, Karlis Muehlenbachs a a Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, Alberta, Canada b Institute of Mineralogy and Petrography, University of Innsbruck, Innsbruck, Austria c Division of Entomology (Paleoentomology), Natural History Museum, University of Kansas, Lawrence, KS, USA d Departament d’Estratigrafia, Paleontologia i Geocie`ncies Marines, Facultat de Geologia, Universitat de Barcelona, Barcelona, Spain Received 28 September 2012; accepted in revised form 10 July 2013; Available online 24 July 2013 Abstract Estimating the partial pressure of atmospheric oxygen (pO2) in the geological past has been challenging because of the lack of 13 reliable proxies. Here we develop a technique to estimate paleo-pO2 using the stable carbon isotope composition (d C) of plant resins—including amber, copal, and resinite—from a wide range of localities and ages (Triassic to modern). Plant resins are par- ticularly suitable as proxies because their highly cross-linked terpenoid structures allow the preservation of pristine d13Csignatures over geological timescales. The distribution of d13C values of modern resins (n = 126) indicates that (a) resin-producing plant fam- ilies generally have a similar fractionation behavior during resin biosynthesis, and (b) the fractionation observed in resins is similar to that of bulk plant matter. Resins exhibit a natural variability in d13C of around 8& (d13Crange:À31& to À23&,mean: À27&), which is caused by local environmental and ecological factors (e.g., water availability, water composition, light exposure, temperature, nutrient availability).
    [Show full text]
  • Aromatic Hydrocarbons from the Middle Jurassic Fossil Wood of the Polish Jura
    82 Contemporary Trends in Geoscience vol . 2 DOI: 10.2478/ctg-2014-0012 Justyna Smolarek1, Leszek Marynowski1 Aromatic hydrocarbons from the Middle Jurassic 1Faculty of Earth Sciences, University of Silesia, fossil wood of the Polish Jura Bedzinska 60, 41-200 Sosnowiec. E-mail: [email protected], [email protected] Key words: Abstract fossil wood, Middle Jurassic, organic Aromatic hydrocarbons are present in the for the majority of the samples are in the matter, biomarkers, aromatic fossil wood samples in relatively small range of 0.1 to 0.5, which results in the high- hydrocarbons, GC-MS amounts. In almost all of the tested sam- ly variable values of Rc (converted value of ples the dominating aromatic hydrocarbon vitrinite reflectance) ranging from 0.45 to is perylene and its methyl and dimethyl de- 0.70%. Such values suggest that MPI1 param- rivatives. The most important biomarkers eter is not useful as maturity parameter in present in the aromatic fraction are dehy- case of Middle Jurassic ore-bearing clays, droabietane, siomonellite and retene, com- even if measured strictly on terrestrial or- pounds characteristic for conifers. The dis- ganic matter (OM). As a result of weather- tribution of discussed compounds is highly ing processes (oxidation) the distribution of variable due to such early diagenetic pro- aromatic hydrocarbons changes. In the ox- cesses affecting the wood as oxidation and idized samples the amount of aromatic hy- the activity of microorganisms. MPI1 pa- drocarbons, both polycyclic as well as aro- rameter values (methylphenanthrene index) matic biomarkers decreases. Contemporary trends in Geoscience vol .
    [Show full text]
  • Hydrotreating of Tall Oils on a Sulfided Nimo Catalyst for The
    IENCE SC • VTT SCIENCE • T S E Hydrotreating of tall oils on a sulfided NiMo catalyst N C O H I N for the production of base-chemicals in steam S O I V Dissertation L • crackers O S G T 83 Y H • R G The technology development for the production of value-added I E L S H 83 E G A I R chemicals from biomass through various thermo-chemical H C approaches is more demanding than ever. Renewable feedstocks H appear as the best starting materials to achieve these developments in an industrial perspective. Tall oil, the by-product of kraft-pulping process is already well-known as a sustainable and low cost feedstock. Hydrotreating of tall oils on a sulfided NiMo catalyst for... This research thesis validates the potential of tall oil as a renewable feedstock for the production of base-chemicals, especially olefins, as conceived in the thermo-chemical bio-refinery concept. The focus was on the use of hydrotreating and steam cracking technologies with different tall oil feedstocks. Particular advances were accomplished in terms of technology development for high yield of ethylene from a complex and challenging bio-feedstock, such as tall oil. Hydrotreating of tall oils on a sulfided NiMo catalyst for the production of base-chemicals in ISBN 978-951-38-8239-6 (Soft back ed.) ISBN 978-951-38-8240-2 (URL: http://www.vtt.fi/publications/index.jsp) steam crackers ISSN-L 2242-119X ISSN 2242-119X (Print) ISSN 2242-1203 (Online) Jinto Manjaly Anthonykutty VTT SCIENCE 83 Hydrotreating of tall oils on a sulfided NiMo catalyst for the production of base- chemicals in steam crackers Jinto Manjaly Anthonykutty VTT Technical Research Centre of Finland Ltd Thesis for the degree of Doctor of Technology to be presented with due permission of the School of Chemical Technology for public examination and criticism in Auditorium KE2 at Aalto University School of Chemical Technology (Espoo, Finland) on the 24th of April, 2015, at 12.00.
    [Show full text]
  • El Soplao, Cantabria, Spain): Paleochemotaxonomic Aspects
    Organic Geochemistry xxx (2010) xxx–xxx Contents lists available at ScienceDirect Organic Geochemistry journal homepage: www.elsevier.com/locate/orggeochem Terpenoids in extracts of Lower Cretaceous ambers from the Basque-Cantabrian Basin (El Soplao, Cantabria, Spain): Paleochemotaxonomic aspects César Menor-Salván a,*, Maria Najarro b, Francisco Velasco c, Idoia Rosales b, Fernando Tornos b, Bernd R.T. Simoneit d,e a Centro de Astrobiología (CSIC-INTA), 28850 Torrejón de Ardoz, Spain b Instituto Geológico y Minero de España (IGME), Rios Rosas 23, 28003 Madrid, Spain c Universidad del País Vasco, Departamento Mineralogía y Petrología, Apdo. 644, 48080 Bilbao, Spain d COGER, King Saud University, Riyadh 11451, Saudi Arabia e Department of Chemistry, Oregon State University, Corvallis, OR 97331, USA article info abstract Article history: The composition of terpenoids from well preserved Cretaceous fossil resins and plant tissues from the Received 22 June 2010 amber bearing deposits of El Soplao and Reocín in Cantabria (northern Spain) have been analyzed using Accepted 30 June 2010 gas chromatography–mass spectrometry and the results are discussed using the terpenoid composition Available online xxxx of extant conifers as a reference. Amber is present at many horizons within two units of coastal to shallow marine siliciclastics of Albian and Cenomanian age. The fossil resins are associated with black amber (jet) and abundant, well preserved plant cuticle compressions, especially those of the extinct conifer genus Frenelopsis (Cheirolepidiaceae). We report the molecular characterization of two types of amber with different botanical origins. One of them is characterized by the significant presence of phenolic terpenoids (ferruginol, totarol and hinokiol) and pimaric/isopimaric acids, as well as their diagenetic products.
    [Show full text]
  • Determination of the Molecular Signature of Fossil Conifers By
    EGU Journal Logos (RGB) Open Access Open Access Open Access Advances in Annales Nonlinear Processes Geosciences Geophysicae in Geophysics Open Access Open Access Natural Hazards Natural Hazards and Earth System and Earth System Sciences Sciences Discussions Open Access Open Access Atmospheric Atmospheric Chemistry Chemistry and Physics and Physics Discussions Open Access Open Access Atmospheric Atmospheric Measurement Measurement Techniques Techniques Discussions Open Access Biogeosciences, 10, 1943–1962, 2013 Open Access www.biogeosciences.net/10/1943/2013/ Biogeosciences doi:10.5194/bg-10-1943-2013 Biogeosciences Discussions © Author(s) 2013. CC Attribution 3.0 License. Open Access Open Access Climate Climate of the Past of the Past Determination of the molecular signature of fossil conifers by Discussions Open Access experimental palaeochemotaxonomy – Part 1: The Araucariaceae Open Access Earth System family Earth System Dynamics Dynamics Y. Lu, Y. Hautevelle, and R. Michels Discussions UMR 7359 CNRS Georessources, University of Lorraine, BP 239, 54506 Vandœuvre-les-Nancy` cedex, France Open Access Geoscientific Geoscientific Open Access Correspondence to: Y. Hautevelle ([email protected]) Instrumentation Instrumentation Received: 11 July 2012 – Published in Biogeosciences Discuss.: 8 August 2012 Methods and Methods and Revised: 7 January 2013 – Accepted: 17 February 2013 – Published: 20 March 2013 Data Systems Data Systems Discussions Open Access Open Access Abstract. Twelve species of the conifer family Araucari- 1
    [Show full text]
  • Paleovegetational Reconstruction and Implications on Formation
    energies Article Paleovegetational Reconstruction and Implications on Formation of Oil Shale and Coal in the Lower Cretaceous Laoheishan Basin (NE China): Evidence from Palynology and Terpenoid Biomarkers Yu Song 1,*, Kai Zhu 1, Yinbo Xu 2,* , Qingtao Meng 3, Zhaojun Liu 3, Pingchang Sun 3 and Xiang Ye 1 1 Key Laboratory of Tectonics and Petroleum Resources, China University of Geosciences, Ministry of Education, Wuhan 430074, China; [email protected] (K.Z.); [email protected] (X.Y.) 2 Oil and Gas Survey, China Geological Survey, Beijing 100083, China 3 College of Earth Sciences, Key Laboratory for Oil Shale and Paragenetic Minerals of Jilin Province, Jilin University, Changchun 130061, China; [email protected] (Q.M.); [email protected] (Z.L.); [email protected] (P.S.) * Correspondence: [email protected] (Y.S.); [email protected] (Y.X.) Abstract: In some cases, the oil shale deposited in shallow lakes may be genetically associated with the coal-bearing successions. Although paleovegetation is an important controlling factor for the formation of oil shale- and coal-bearing successions, few studies have focused on their joint characterization. In this study, a total of twenty-one oil shale and coal samples were collected from the upper member of the Lower Cretaceous Muling Formation (K1ml2) in the Laoheishan Citation: Song, Y.; Zhu, K.; Xu, Y.; Basin, and investigated for their bulk geochemical, maceral, palynological, and terpenoid biomarker Meng, Q.; Liu, Z.; Sun, P.; Ye, X. characteristics, in order to reconstruct the paleovegetation and reveal its influence on the formation Paleovegetational Reconstruction and of oil shale and coal.
    [Show full text]