Resistant biomacromolecules in marine microalgae of the classes eustigmatophyceae and chlorophyceae: Geochemical implications

被引:130
作者
Gelin, F
Boogers, I
Noordeloos, AAM
Damste, JSS
Riegman, R
De Leeuw, JW
机构
[1] Netherlands Inst Sea Res NIOZ, Dept Marine Biogeochem & Toxicol, NL-1790 AB Den Burg, Netherlands
[2] Netherlands Inst Sea Res NIOZ, Dept Biol Oceanog, NL-1790 AB Den Burg, Netherlands
关键词
marine microalgae; Eustigmatophyceae; Chlorophyceae; algaenan; long-chain diols; selective preservation; kerogen; flash pyrolysis;
D O I
10.1016/S0146-6380(97)00035-1
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Non-hydrolysable macromolecular constituents (i.e. algaenans) were isolated from two out of seven marine microalgae investigated. Nannochloropsis salina and Nannochloropsis sp. from the class of Eustigmatophyceae produce highly aliphatic algaenans. Flash pyrolysis and chemical degradations with HI and RuO4 allowed for the identification of their chemical structure, which is mainly composed of polyether-linked long-chain (up to C-36) n-alkyl units. The building blocks of this polymer were also recognized in lipid fractions. The green microalgae (Chlorophyceae) Chlorella spaerckii, Chlorococcum sp. and Nannochloris sp. were earlier thought to biosynthesize algaenans comprising aliphatic and/or aromatic moieties. However, a new isolation method utilizing trifluoroacetic acid (TFA) prior to the other hydrolyses revealed that the macromolecular material isolated from these three chlorophytes was either hydrolysable with TFA or artefacts from the former method. Similar to algaenans from fresh water green microalgae, the aliphatic eustigmatophyte algaenans are likely to be selectively preserved in depositional environments and might ultimately serve as source rock organic matter of marine crude oils. Furthermore, they may play an important role in the cycling of carbon. (C) 1997 Elsevier Science Ltd.
引用
收藏
页码:659 / 675
页数:17
相关论文
共 65 条
  • [1] ALLARD B, 1997, IN PRESS ORG GEOCHEM
  • [2] [Anonymous], ORG GEOCHEM
  • [3] CLOSED PYROLYSES OF THE ISOPRENOID ALGAENAN OF BOTRYOCOCCUS-BRAUNII, L RACE - GEOCHEMICAL IMPLICATIONS FOR DERIVED KEROGENS
    BEHAR, F
    DERENNE, S
    LARGEAU, C
    [J]. GEOCHIMICA ET COSMOCHIMICA ACTA, 1995, 59 (14) : 2983 - 2997
  • [4] CLEAVAGE OF ETHERS
    BHATT, MV
    KULKARNI, SU
    [J]. SYNTHESIS-STUTTGART, 1983, (04): : 249 - 282
  • [5] CHEMICAL, MOLECULAR AND ISOTOPIC DIFFERENTIATION OF ORGANIC FACIES IN THE TERTIARY LACUSTRINE DUARINGA OIL-SHALE DEPOSIT, QUEENSLAND, AUSTRALIA
    BOREHAM, CJ
    SUMMONS, RE
    ROKSANDIC, Z
    DOWLING, LM
    HUTTON, AC
    [J]. ORGANIC GEOCHEMISTRY, 1994, 21 (6-7) : 685 - 712
  • [6] MOLECULAR CHARACTERIZATION OF KEROGEN FROM THE KIMMERIDGE CLAY FORMATION BY MILD SELECTIVE CHEMICAL DEGRADATION AND SOLID-STATE C-13-NMR
    BOUCHER, RJ
    STANDEN, G
    PATIENCE, RL
    EGLINTON, G
    [J]. ORGANIC GEOCHEMISTRY, 1990, 16 (4-6) : 951 - 958
  • [7] ELECTRON-MICROSCOPY AND PYROLYSIS OF KEROGENS FROM THE KIMMERIDGE CLAY FORMATION, UK - SOURCE ORGANISMS, PRESERVATION PROCESSES, AND ORIGIN OF MICROCYCLES
    BOUSSAFIR, M
    GELIN, F
    LALLIERVERGES, E
    DERENNE, S
    BERTRAND, P
    LARGEAU, C
    [J]. GEOCHIMICA ET COSMOCHIMICA ACTA, 1995, 59 (18) : 3731 - 3747
  • [8] CHRETIENNOTDINE.MJ, 1990, ATLAS PHYTOPLANCTON, V3, P18
  • [9] PARTIAL RESOLUTION OF SOURCES OF N-ALKANES IN THE SALINE PORTION OF THE PARACHUTE CREEK MEMBER, GREEN RIVER FORMATION (PICEANCE CREEK BASIN, COLORADO)
    COLLISTER, JW
    LICHTFOUSE, E
    HIESHIMA, G
    HAYES, JM
    [J]. ORGANIC GEOCHEMISTRY, 1994, 21 (6-7) : 645 - 659
  • [10] LIPIDS OF AQUATIC ORGANISMS AS POTENTIAL CONTRIBUTORS TO LACUSTRINE SEDIMENTS .2.
    CRANWELL, PA
    EGLINTON, G
    ROBINSON, N
    [J]. ORGANIC GEOCHEMISTRY, 1987, 11 (06) : 513 - 527