Stable carbon isotope fractionation of organic cyst-forming dinoflagellates: Evaluating the potential for a CO2 proxy

[1]  S. Kranz,et al.  Cellular inorganic carbon fluxes in Trichodesmium: a combined approach using measurements and modelling , 2014, Journal of experimental botany.

[2]  Dedmer B. Van de Waal,et al.  Differential effects of ocean acidification on carbon acquisition in two bloom-forming dinoflagellate species , 2014, Physiologia plantarum.

[3]  R. DeConto,et al.  A 40-million-year history of atmospheric CO2 , 2013, Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences.

[4]  Uwe John,et al.  Ocean Acidification Reduces Growth and Calcification in a Marine Dinoflagellate , 2013, PloS one.

[5]  A. Vernal,et al.  Atlas of modern dinoflagellate cyst distribution based on 2405 data points , 2013 .

[6]  C. Cavanaugh,et al.  Low stable carbon isotope fractionation by coccolithophore RubisCO , 2011 .

[7]  G. Lange,et al.  Selective aerobic and anaerobic degradation of lipids and palynomorphs in the Eastern Mediterranean since the onset of sapropel S1 deposition , 2010 .

[8]  F. Morel,et al.  Revelle revisited: Buffer factors that quantify the response of ocean chemistry to changes in DIC and alkalinity , 2010 .

[9]  A. Cembella,et al.  Intra-population clonal variability in allelochemical potency of the toxigenic dinoflagellate Alexandrium tamarense , 2009 .

[10]  A. Rochon,et al.  The Gonyaulax spinifera (Dinophyceae) “complex”: Perpetuating the paradox? , 2009 .

[11]  G. Versteegh,et al.  Preservation and organic chemistry of Late Cenozoic organic-walled dinoflagellate cysts: A review , 2008 .

[12]  G. Dickens,et al.  Environmental precursors to rapid light carbon injection at the Palaeocene/Eocene boundary , 2007, Nature.

[13]  G. Farquhar,et al.  Differences in Carbon Isotope Discrimination of Three Variants of D-Ribulose-1,5-bisphosphate Carboxylase/Oxygenase Reflect Differences in Their Catalytic Mechanisms*♦ , 2007, Journal of Biological Chemistry.

[14]  C. Cavanaugh,et al.  Kinetic isotope effect and biochemical characterization of form IA RubisCO from the marine cyanobacterium Prochlorococcus marinus MIT9313 , 2007 .

[15]  D. Morse,et al.  CO2‐CONCENTRATING MECHANISMS OF THE POTENTIALLY TOXIC DINOFLAGELLATE PROTOCERATIUM RETICULATUM (DINOPHYCEAE, GONYAULACALES) 1 , 2007 .

[16]  Robert A. Berner,et al.  GEOCARBSULF: A combined model for Phanerozoic atmospheric O2 and CO2 , 2006 .

[17]  D. Royer.  CO2-forced climate thresholds during the Phanerozoic , 2006 .

[18]  Robert V. Demicco,et al.  Elevated Eocene Atmospheric CO2 and Its Subsequent Decline , 2006, Science.

[19]  U. Riebesell,et al.  Inorganic carbon acquisition in red tide dinoflagellates. , 2006, Plant, cell & environment.

[20]  K. Caldeira,et al.  Comparison of water column [CO2aq] with sedimentary alkenone‐based estimates: A test of the alkenone‐CO2 proxy , 2002 .

[21]  M. Pagani.  The alkenone-CO2 proxy and ancient atmospheric carbon dioxide , 2002, Philosophical Transactions of the Royal Society of London. Series A: Mathematical, Physical and Engineering Sciences.

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

[23]  D. Wolf-Gladrow,et al.  CO2 in Seawater: Equilibrium, Kinetics, Isotopes , 2001 .

[24]  U. Riebesell,et al.  The effects of varying CO2 concentration on lipid composition and carbon isotope fractionation in Emiliania huxleyi , 2000 .

[25]  Susanne Menden-Deuer,et al.  Carbon to volume relationships for dinoflagellates, diatoms, and other protist plankton , 2000 .

[26]  U. Riebesell,et al.  Effects of growth rate, CO2 concentration, and cell size on the stable carbon isotope fractionation in marine phytoplankton , 1999 .

[27]  U. Riebesell,et al.  Stable carbon isotope fractionation by marine phytoplankton in response to daylength, growth rate, and CO2 availability , 1999 .

[28]  J. Jouzel,et al.  Climate and atmospheric history of the past 420,000 years from the Vostok ice core, Antarctica , 1999, Nature.

[29]  K. L. Hanson,et al.  Erratum: Consistent fractionation of13C in nature and in the laboratory: Growth-rate effects in some haptophyte algae (Global Biogeochemical Cycles (1997) 11:2 (279-292)) , 1999 .

[30]  Robert R. Bidigare,et al.  Effect of growth rate and CO2 concentration on carbon isotopic fractionation by the marine diatom Phaeodactylum tricornutum , 1997 .

[31]  R. Bidigare,et al.  Organic carbon δ13C variations in sedimentary rocks as chemostratigraphic and paleoenvironmental tools , 1997 .

[32]  K. L. Hanson,et al.  Consistent fractionation of 13C in nature and in the laboratory: Growth‐rate effects in some haptophyte algae , 1997, Global biogeochemical cycles.

[33]  R. Fensome,et al.  Fossil dinoflagellate diversity, originations, and extinctions and their significance , 1996 .

[34]  W. Broecker,et al.  Oceanic pH control on the boron isotopic composition of foraminifera: Evidence from culture experiments , 1996 .

[35]  D. Wolf-Gladrow,et al.  A model of photosynthetic 13C fractionation by marine phytoplankton based on diffusive molecular CO2 uptake , 1996 .

[36]  D. Anderson,et al.  Morphological development of resting cysts in cultures of the marine dinoflagellate Lingulodinium polyedrum (= L. Machaerophorum) , 1995 .

[37]  Stephen A. Macko,et al.  Dependence of phytoplankton carbon isotopic composition on growth rate and [CO2)aq: Theoretical considerations and experimental results , 1995 .

[38]  J. Hayes,et al.  Photosynthetic fractionation of 13C and concentrations of dissolved CO2 in the central equatorial Pacific during the last 255,000 years. , 1994, Paleoceanography.

[39]  M. Pilson,et al.  Carbon isotope fractionation by marine phytoplankton in culture: The effects of CO2 concentration, pH, temperature, and species , 1994 .

[40]  R. Goericke,et al.  Changes in the δ13C of surface water particulate organic matter across the subtropical convergence in the SW Indian Ocean , 1993 .

[41]  D. Dilcher,et al.  Paleoatmospheric Signatures in Neogene Fossil Leaves , 1993, Science.

[42]  J. Berry,et al.  Photosynthetic Fractionation of the Stable Isotopes of Oxygen and Carbon , 1993, Plant physiology.

[43]  J. Hayes,et al.  Fractionation of carbon isotopes by phytoplankton and estimates of ancient CO2 levels. , 1992, Global biogeochemical cycles.

[44]  A. M. Johnston,et al.  Mechanisms of inorganic-carbon acquisition in marine phytoplankton and their implications for the use of other resources , 1991 .

[45]  A. Dickson.  Standard potential of the reaction: , and and the standard acidity constant of the ion HSO4− in synthetic sea water from 273.15 to 318.15 K , 1990 .

[46]  M. D. Keller,et al.  MEDIA FOR THE CULTURE OF OCEANIC ULTRAPHYTOPLANKTON 1,2 , 1987 .

[47]  F. Millero,et al.  A comparison of the equilibrium constants for the dissociation of carbonic acid in seawater media , 1987 .

[48]  M. O'Leary,et al.  Carbon isotope effect on carboxylation of ribulose bisphosphate catalyzed by ribulosebisphosphate carboxylase from Rhodospirillum rubrum. , 1985, Biochemistry.

[49]  M. O'Leary,et al.  Carbon isotope effects on enzyme-catalyzed carboxylation of ribulose bisphosphate , 1984 .

[50]  J. Christeller,et al.  Isotope Discrimination by Ribulose 1,5-Diphosphate Carboxylase: No Effect of Temperature or HCO(3) Concentration. , 1976, Plant physiology.

[51]  W. G. Mook,et al.  CARBON ISOTOPE FRACTIONATION BETWEEN DISSOLVED BICARBONATE AND GASEOUS CARBON-DIOXIDE , 1974 .

[52]  C. Culberson,et al.  MEASUREMENT OF THE APPARENT DISSOCIATION CONSTANTS OF CARBONIC ACID IN SEAWATER AT ATMOSPHERIC PRESSURE1 , 1973 .

[53]  E. Degens,et al.  Metabolic fractionation of carbon isotopes in marine plankton—II. Data on samples collected off the coasts of Peru and Ecuador , 1968 .

[54]  H. Eugster.  Sodium carbonate‐bicarbonate minerals as indicators of Pco2 , 1966 .

[55]  R. Guillard,et al.  Studies of marine planktonic diatoms. I. Cyclotella nana Hustedt, and Detonula confervacea (cleve) Gran. , 1962, Canadian journal of microbiology.

[56]  M. Pagani.  12.13 – Biomarker-Based Inferences of Past Climate: The Alkenone pCO2 Proxy , 2014 .

[57]  A. Sluijs,et al.  From greenhouse to icehouse; organic-walled dinoflagellate cysts as paleoenvironmental indicators in the Paleogene , 2005 .

[58]  D. Anderson,et al.  Cysts of Danish Gymnodinium nolleri Ellegaard et Moestrup sp. ined. (Dinophyceae): studies on encystment, excystment and toxicity , 1998 .

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

[60]  D. Wilbur,et al.  CARBON ISOTOPE FRACTIONATION DURING GAS-WATER EXCHANGE AND DISSOLUTION OF CO2 , 1995 .

[61]  S. Wainright,et al.  Diatom sources of 13C-rich carbon in marine food webs , 1991 .

[62]  Roger Barlow,et al.  Statistics : a guide to the use of statistical methods in thephysical sciences , 1989 .

[63]  W. Richard,et al.  TEMPERATURE AND PHYTOPLANKTON GROWTH IN THE SEA , 1972 .