A diatomaceous origin for long-chain diols and mid-chain hydroxy methyl alkanoates widely occurring in quaternary marine sediments: Indicators for high nutrient conditions

[1]  U. Riebesell,et al.  Light‐dependent carbon isotope fractionation in the coccolithophorid Emiliania huxleyi , 2002 .

[2]  W. Helder,et al.  Selective preservation of upwelling-indicating diatoms in sediments off Somalia, NW Indian Ocean , 2001 .

[3]  A. Aksu,et al.  The last occurrence of Proboscia curvirostris in the North Atlantic marine isotope stages 9-8 , 2001 .

[4]  J. Damsté,et al.  Formation of mid-chain alkane keto-ols by post-depositional oxidation of mid-chain diols in Mediterranean sapropels , 2001 .

[5]  Stefan Schouten,et al.  A molecular and stable carbon isotopic study of lipids in late Quaternary sediments from the Arabian Sea , 2000 .

[6]  R. Schneider,et al.  Mid-chain diols and keto-ols in se atlantic sediments: a new tool for tracing past sea surface water masses? , 2000 .

[7]  D. Slezak,et al.  Nutrient uptake and alkaline phosphatase (ec 3:1:3:1) activity of emiliania huxleyi (PRYMNESIOPHYCEAE) during growth under n and p limitation in continuous cultures , 2000 .

[8]  S. M. Barrett,et al.  FATTY ACIDS AND HYDROXY FATTY ACIDS IN THREE SPECIES OF FRESHWATER EUSTIGMATOPHYTES , 1999 .

[9]  M. Gosselin,et al.  Nitrate, phosphate, and iron limitation of the phytoplankton assemblage in the lagoon of Takapoto Atoll (Tuamotu Archipelago, French Polynesia) , 1999 .

[10]  R. B. Pearce,et al.  The role of mat-forming diatoms in the formation of Mediterranean sapropels , 1999, Nature.

[11]  S. Derenne,et al.  Distribution of aliphatic, nonhydrolyzable biopolymers in marine microalgae , 1999 .

[12]  G. B. Gardner,et al.  Upward transport of oceanic nitrate by migrating diatom mats , 1999, Nature.

[13]  S. M. Barrett,et al.  Microalgal biomarkers: A review of recent research developments , 1998 .

[14]  K. Grice,et al.  Biosynthetic effects on the stable carbon isotopic compositions of algal lipids: implications for deciphering the carbon isotopic biomarker record , 1998 .

[15]  J. D. Leeuw,et al.  Potential palaeoenvironmental information of C24 to C36 mid-chain diols, keto-ols and mid-chain hydroxy fatty acids; a critical review , 1997 .

[16]  J. Damsté,et al.  Resistant biomacromolecules in marine microalgae of the classes Eustigmatophyceae and Chlorophyceae: Geochemical implications , 1997 .

[17]  J. Damsté,et al.  Mid-chain hydroxy long-chain fatty acids in microalgae from the genus Nannochloropsis , 1997 .

[18]  L. N. D. S. Domis,et al.  Growth of harmful marine algae in multispecies cultures , 1996 .

[19]  D. Hernández-Becerril.  PLANKTONIC DIATOMS FROM THE GULF OF CALIFORNIA AND COASTS OFF BAJA CALIFORNIA: THE GENERA RHIZOSOLENIA, PROBOSCIA, PSEUDOSOLENIA, AND FORMER RHIZOSOLENIA SPECIES , 1995 .

[20]  Graeme A. Dunstan,et al.  C25 and C30 highly branched isoprenoid alkenes in laboratory cultures of two marine diatoms , 1994 .

[21]  R. Guillard,et al.  Stichochrysis immobilis is a diatom, not a chrysophyte , 1993 .

[22]  C. Lange,et al.  Seasonal cycle of diatoms in the Skagerrak, North Atlantic, with emphasis on the period 1980–1990 , 1992 .

[23]  R. Jordan,et al.  Fossil members of the diatom genus Proboscia , 1991 .

[24]  M. Sogin,et al.  The characterization of enzymatically amplified eukaryotic 16S-like rRNA-coding regions. , 1988, Gene.

[25]  R. E. McDuff,et al.  Interstitial water studies of Late Quaternary Eastern Mediterranean sediments with emphasis on early diagenetic reactions and evaporitic salt influences , 1987 .

[26]  H. Buser,et al.  Determination of double bond position in mono-unsaturated acetates by mass spectrometry of dimethyl disulfide adducts , 1983 .

[27]  J. W. Leeuw,et al.  The occurrence and identification of C30, C31 and C32 alkan-1, 15-diols and alkan-15-one-1-ols in Unit I and Unit II Black Sea sediments , 1981 .

[28]  V. P. Skipski,et al.  Separation of lipid classes by thin-layer chromatography. , 1965, Biochimica et biophysica acta.

[29]  S. Wakeham,et al.  Lipid biomarker fluxes in the Arabian Sea, with a comparison to the equatorial Pacific Ocean , 2002 .

[30]  J. Robert,et al.  Effects of auxosporulation on distributions of C(25) and C(30) isoprenoid alkenes in Rhizosolenia setigera. , 2002, Phytochemistry.

[31]  Sharon L. Smith.  Understanding the Arabian Sea: Reflections on the 1994-1996 Arabian Sea Expedition , 2001 .

[32]  G. Muyzer,et al.  Denaturing gradient gel electrophoresis in marine microbial ecology , 2001 .

[33]  J. Damsté,et al.  Marine and terrigenous lipids in southeast atlantic sediments (leg 175) as paleoenvironmental indicators: initial results , 2001 .

[34]  F. Prahl,et al.  Annual biomarker record for export production in the central Arabian Sea , 2000 .

[35]  G. Wefer,et al.  Offshore influence of coastal upwelling off Mauritania, NW Africa, as recorded by diatoms in sediment traps at 2195 m water depth , 1998 .

[36]  K. L. Hanson,et al.  Effect of Phytoplankton Cell Geometry on Carbon Isotopic Fractionation , 1998 .

[37]  S. M. Barrett,et al.  C30C32 alkyl diols and unsaturated alcohols in microalgae of the class Eustigmatophyceae , 1992 .

[38]  S. Casper.  The marine diatom genus Rhizosolenia, Sundström Bo G., in: A new approach to the taxonomy. (1986), 117 S., 2 Fig. im Text, 39 pls. mit 291 Fig. , 1988 .

[39]  S. Brassell,et al.  Long chain unsaturated ketones and esters in living algae and marine sediments , 1984 .

[40]  C. L. Davies,et al.  Distribution of chlorosulpholipids in algae , 1979 .