Influence of surface ocean density on planktonic foraminifera calcification
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G. Kontakiotis | Stergios D. Zarkogiannis | A. Tripati | A. Antonarakou | H. Drinia | P. G. Mortyn | M. Greaves
[1] S. Eggins,et al. Planktic foraminifera form their shells via metastable carbonate phases , 2017, Nature Communications.
[2] M. Schulz,et al. Factors controlling the depth habitat of planktonic foraminifera in the subtropical eastern North Atlantic , 2016 .
[3] Matthew J. Smith,et al. Transient dynamics of terrestrial carbon storage: Mathematical foundation and numeric examples , 2016 .
[4] S. Flögel,et al. Paleoseawater density reconstruction and its implication for cold-water coral carbonate mounds in the northeast Atlantic through time , 2016 .
[5] M. Kučera,et al. Seasonal Variation in Shell Calcification of Planktonic Foraminifera in the NE Atlantic Reveals Species-Specific Response to Temperature, Productivity, and Optimum Growth Conditions , 2016, PloS one.
[6] Claire Waelbroeck,et al. Evolution of South Atlantic density and chemical stratification across the last deglaciation , 2015, Proceedings of the National Academy of Sciences.
[7] G. Kontakiotis,et al. Biotic and geochemical (δ 18 O, δ 13 C, Mg/Ca, Ba/Ca) responses of Globigerinoides ruber morphotypes to upper water column variations during the last deglaciation, Gulf of Mexico , 2015 .
[8] Y. Okazaki,et al. Observation of the dissolution process of Globigerina bulloides tests (planktic foraminifera) by X‐ray microcomputed tomography , 2015 .
[9] A. Roberts,et al. Sea-level and deep-sea-temperature variability over the past 5.3 million years , 2014, Nature.
[10] P. Bown,et al. The response of calcifying plankton to climate change in the Pliocene , 2013 .
[11] M. Kučera,et al. Calcification intensity in planktonic Foraminifera reflects ambient conditions irrespective of environmental stress , 2013 .
[12] R. Thunell,et al. Planktonic foraminiferal area density as a proxy for carbonate ion concentration: A calibration study using the Cariaco Basin ocean time series , 2013 .
[13] D. Purdie,et al. Calcification in the planktonic foraminifera Globigerina bulloides linked to phosphate concentrations in surface waters of the North Atlantic Ocean , 2011 .
[14] R. Zahn,et al. Contrasting multiproxy reconstructions of surface ocean hydrography in the Agulhas Corridor and implications for the Agulhas Leakage during the last 345,000 years , 2010 .
[15] M. Schulz,et al. Inside story: An X-ray computed tomography method for assessing dissolution in the tests of planktonic foraminifera , 2010 .
[16] P. Govil,et al. Relationship between Weights of Planktonic Foraminifer Shell and Surface Water CO3 = Concentration during the Holocene and Last Glacial Period , 2010 .
[17] R. Zeebe,et al. Glacial cycles: Atmosphere and ocean chemistry , 2010 .
[18] R. Schiebel,et al. Testing planktic foraminiferal shell weight as a surface water [CO32?] proxy using plankton net samples , 2010 .
[19] W. Howard,et al. Reduced calcification in modern Southern Ocean planktonic foraminifera , 2009 .
[20] H. Elderfield,et al. Holocene oscillations in temperature and salinity of the surface subpolar North Atlantic , 2009, Nature.
[21] C. Edwards,et al. A 5 million year comparison of Mg/Ca and alkenone paleothermometers , 2008 .
[22] F. Sierro,et al. Controls of shell calcification in planktonic foraminifers , 2008 .
[23] M. Greaves. Trace elements in marine biogenic carbonates : analysis and application to past ocean chemistry , 2008 .
[24] S. Naik,et al. Calcite dissolution along a transect in the western tropical Indian Ocean: A multiproxy approach , 2007 .
[25] D. Archer,et al. Globally increased pelagic carbonate production during the Mid-Brunhes dissolution interval and the CO2 paradox of MIS 11 , 2006 .
[26] Gavin A. Schmidt,et al. Global gridded data set of the oxygen isotopic composition in seawater , 2006 .
[27] F. Mackenzie,et al. Coastal ocean and carbonate systems in the high CO2 world of the Anthropocene , 2005 .
[28] T. Kiefer,et al. Temporal changes in North Atlantic circulation constrained by planktonic foraminiferal shell weights , 2004 .
[29] R. Zeebe,et al. History of carbonate ion concentration over the last 100 million years , 2004 .
[30] W. Prell,et al. Calibration of the Mg/Ca of Globorotalia truncatulinoides (R) for the reconstruction of marine temperature gradients , 2004 .
[31] W. Broecker,et al. Shell weights from the South Atlantic , 2004 .
[32] S. Villiers. A 425 kyr record of foraminiferal shell weight variability in the western equatorial Pacific , 2003 .
[33] C. Fisher. Planktic foraminiferal porosity: a water mass proxy for latest Cenomanian paleoceanography, Greenhorn Sea, Western Interior USA and Canada , 2003 .
[34] Henry Elderfield,et al. Calibration of Mg/Ca thermometry in planktonic foraminifera from a sediment trap time series , 2003 .
[35] M. Sarnthein,et al. Paired δ18O signals of Neogloboquadrina pachyderma (s) and Turborotalita quinqueloba show thermal stratification structure in Nordic Seas , 2003 .
[36] B. Delille. CO2 in Seawater: Equilibrium, Kinetics, Isotopes , 2002 .
[37] S. Barker,et al. Foraminiferal Calcification Response to Glacial-Interglacial Changes in Atmospheric CO2 , 2002, Science.
[38] R. Henrich,et al. Present water mass calcium carbonate corrosiveness in the eastern South Atlantic inferred from ultrastructural breakdown of Globigerina bulloides in surface sediments , 2002 .
[39] W. Broecker,et al. Carbonate ion concentration in glacial‐age deep waters of the Caribbean Sea , 2002 .
[40] W. Broecker,et al. Glacial-to-Holocene Redistribution of Carbonate Ion in the Deep Sea , 2001, Science.
[41] D. Wolf-Gladrow,et al. CO2 in Seawater: Equilibrium, Kinetics, Isotopes , 2001 .
[42] W. Broecker,et al. An evaluation of Lohmann's foraminifera weight dissolution index , 2001 .
[43] W. Broecker,et al. Distribution of carbonate ion in the deep ocean: Support for a post‐Little Ice Age change in Southern Ocean ventilation? , 2000 .
[44] R. Henrich,et al. Carbonate dissolution in the South Atlantic Ocean: evidence from ultrastructure breakdown in Globigerina bulloides , 2000 .
[45] D. Schrag,et al. Surface ocean density gradients during the Last Glacial Maximum , 2000 .
[46] William B. Curry,et al. Weaker Gulf Stream in the Florida Straits during the Last Glacial Maximum , 1999, Nature.
[47] D. Lea,et al. Glacial–interglacial changes in Subantarctic sea surface temperature and δ18O-water using foraminiferal Mg , 1999 .
[48] D. Hodell,et al. A 1.0 Myr Record of Glacial North Atlantic Intermediate Water Variability from ODP Site 982 in the Northeast Atlantic , 1999 .
[49] Jelle Bijma,et al. Reevaluation of the oxygen isotopic composition of planktonic foraminifera: Experimental results and revised paleotemperature equations , 1998 .
[50] Jelle Bijma,et al. Effect of seawater carbonate concentration on foraminiferal carbon and oxygen isotopes , 1997, Nature.
[51] Sang-Tae Kim,et al. Equilibrium and nonequilibrium oxygen isotope effects in synthetic carbonates , 1997 .
[52] D. Furbish,et al. Hydrodynamic strategies in the morphological evolution of spinose planktonic foraminifera , 1997 .
[53] J. Milliman. Production and accumulation of calcium carbonate in the ocean: Budget of a nonsteady state , 1993 .
[54] C. Hemleben,et al. Temperature and salinity limits for growth and survival of some planktonic foraminifers in laboratory cultures , 1990 .
[55] R. Fairbanks. A 17,000-year glacio-eustatic sea level record: influence of glacial melting rates on the Younger Dryas event and deep-ocean circulation , 1989, Nature.
[56] Christoph Hemleben,et al. Modern Planktonic Foraminifera , 1988, Springer New York.
[57] L. Feldkamp,et al. Practical cone-beam algorithm , 1984 .
[58] W. Balsam. Carbonate Dissolution on the Muir Seamount (Western North Atlantic): Interglacial/Glacial Changes , 1983 .
[59] D. Caron,et al. Sequence of morphological and cytoplasmic changes during gametogenesis in the planktonic foraminifer Globigerinoides sacculifer (Brady) , 1983 .
[60] D. S. Marszalek. The role of heavy skeletons in vertical movements of non‐motile zooplankton , 1982 .
[61] A. Bé,et al. Orbulina universa d'Orbigny in the Indian Ocean , 1973 .
[62] C. Emiliani. Depth Habitats of Growth Stages of Pelagic Foraminifera , 1971, Science.
[63] W. Broecker,et al. Degree of saturation of CaCO3 in the oceans , 1969 .
[64] Allan W. H. B�. Shell Porosity of Recent Planktonic Foraminifera as a Climatic Index , 1968, Science.
[65] Will Wiles. Pleistocene changes in the pore concentration of a planktonic foraminiferal species from the Pacific Ocean , 1965 .
[66] R. Schiebel,et al. Planktic Foraminifers in the Modern Ocean , 2017 .
[67] J. Singarayer,et al. Reconstructing paleosalinity from δ18O: Coupled model simulations of the Last Glacial Maximum, Last Interglacial and Late Holocene , 2016 .
[68] D. Wolf-Gladrow,et al. Equilibrium, Kinetics, Isotopes , 2010 .
[69] Rainer Feistel,et al. The International Thermodynamic Equation Of Seawater 2010 (TEOS-10): Calculation and Use of Thermodynamic Properties , 2010 .
[70] S. Villiers. Optimum growth conditions as opposed to calcite saturation as a control on the calcification rate and shell-weight of marine foraminifera , 2004 .
[71] R. Schiebel,et al. Interannual variability of planktic foraminiferal populations and test flux in the eastern North Atlantic Ocean (JGOFS) , 2000 .
[72] E. Maier‐Reimer,et al. Effect of deep-sea sedimentary calcite preservation on atmospheric CO2 concentration , 1994, Nature.
[73] P. Haenel. Intérêt paléoocéanographique d'Orbulina universa d'Orbigny (Foraminifère) , 1987 .
[74] S. Vogel. Life in Moving Fluids: The Physical Biology of Flow , 1981 .
[75] J. Kennett,et al. Biometric analysis of phenotypic variation in RecentGlobigerina bulloides d'Orbigny in the southern Indian Ocean , 1976 .
[76] L. Borgman,et al. Latitudal variations in planktonic foraminiferal test porosity; Part 1, Optical studies , 1972 .
[77] G. H. Scott. The relationship between the Miocene Foraminiferida Globorotalia miozea miozea and G. praemenardii , 1972 .