Micron-scale intrashell oxygen isotope variation in cultured planktic foraminifers
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[1] M. Bar-Matthews,et al. Seasonal resolution of Eastern Mediterranean climate change since 34 ka from a Soreq Cave speleothem , 2012 .
[2] J. Valley,et al. Mollusk shell nacre ultrastructure correlates with environmental temperature and pressure. , 2012, Journal of the American Chemical Society.
[3] J. Valley,et al. Planktonic foraminiferal oxygen isotope analysis by ion microprobe technique suggests warm tropical sea surface temperatures during the Early Paleogene , 2011 .
[4] S. Eggins,et al. Planktic foraminifers as recorders of seawater Ba/Ca , 2011 .
[5] D. Kroon,et al. Quantifying sea surface temperature ranges of the Arabian Sea for the past 20 000 years , 2010 .
[6] Stefan Schouten,et al. Coherent pattern and timing of the carbon isotope excursion and warming during Eocene Thermal Maximum 2 as recorded in planktic and benthic foraminifera , 2010 .
[7] S. Eggins,et al. Effects of seafloor and laboratory dissolution on the Mg/Ca composition of Globigerinoides sacculifer and Orbulina universa tests — A laser ablation ICPMS microanalysis perspective , 2010 .
[8] J. Erez,et al. Intra-shell boron isotope ratios in the symbiont-bearing benthic foraminiferan Amphistegina lobifera: implications for δ11B vital effects and paleo-pH reconstructions. , 2010 .
[9] R. James,et al. Environmental versus biomineralization controls on the intratest variation in the trace element composition of the planktonic foraminifera G. inflata and G. scitula , 2009 .
[10] S. Eggins,et al. Surface and subsurface seawater temperature reconstruction using Mg/Ca microanalysis of planktonic foraminifera Globigerinoides ruber, Globigerinoides sacculifer, and Pulleniatina obliquiloculata , 2009 .
[11] G. Leduc,et al. Modes of eastern equatorial Pacific thermocline variability: Implications for ENSO dynamics over the last glacial period , 2009 .
[12] J. Valley,et al. Intratest oxygen isotope variability in the planktonic foraminifer N. pachyderma: Real vs. apparent vital effects by ion microprobe , 2009 .
[13] M. Bar-Matthews,et al. Climate deterioration in the Eastern Mediterranean as revealed by ion microprobe analysis of a speleothem that grew from 2.2 to 0.9 ka in Soreq Cave, Israel , 2009, Quaternary Research.
[14] J. Erez,et al. Intra-shell oxygen isotope ratios in the benthic foraminifera genus Amphistegina and the influence of seawater carbonate chemistry and temperature on this ratio , 2008 .
[15] D. Lea,et al. Geochemical investigation of gametogenic calcite addition in the planktonic foraminifera Orbulina universa , 2008 .
[16] C. Pelejero,et al. Characterization of contaminant phases in foraminifera carbonates by electron microprobe mapping , 2008 .
[17] T. Marchitto,et al. A secondary ionization mass spectrometry calibration of Cibicidoides pachyderma Mg/Ca with temperature , 2008 .
[18] D. Kroon,et al. Uncertainties in seawater thermometry deriving from intratest and intertest Mg/Ca variability in Globigerinoides ruber , 2008 .
[19] L. Riciputi,et al. Letter: High-precision oxygen isotope analysis of picogram samples reveals 2 μm gradients and slow diffusion in zircon , 2007 .
[20] S. Carpenter,et al. Diary of a bluegill (Lepomis macrochirus): daily δ 13 C and δ 18 O records in otoliths by ion microprobe , 2007 .
[21] R. Schneider,et al. 155,000 Years of West African Monsoon and Ocean Thermal Evolution , 2007, Science.
[22] P. deMenocal,et al. Mid-Holocene El Niño Southern Oscillation (ENSO) attenuation revealed by individual foraminifera in eastern tropical Pacific sediments , 2006 .
[23] K. Shirai,et al. Microdistribution of Mg/Ca, Sr/Ca, and Ba/Ca ratios in Pulleniatina obliquiloculata test by using a NanoSIMS: Implication for the vital effect mechanism , 2006 .
[24] G. Layne,et al. Application of secondary ion mass spectrometry to the determination of Mg/Ca in rare, delicate, or altered planktonic foraminifera: Examples from the Holocene, Paleogene, and Cretaceous , 2005 .
[25] S. Eggins,et al. Characterization of Mg/Ca distributions in planktonic foraminifera species by electron microprobe mapping , 2005 .
[26] H. Elderfield,et al. Variability of Mg/Ca and Sr/Ca between and within the planktonic foraminifers Globigerina bulloides and Globorotalia truncatulinoides , 2005 .
[27] T. Guilderson,et al. Laurentide Ice Sheet meltwater and abrupt climate change during the last glaciation , 2005 .
[28] C. Pelejero,et al. Identification and removal of Mn‐Mg‐rich contaminant phases on foraminiferal tests: Implications for Mg/Ca past temperature reconstructions , 2005 .
[29] B. Hönisch,et al. Effects of seawater carbonate ion concentration and temperature on shell U, Mg, and Sr in cultured planktonic foraminifera , 2004 .
[30] S. Eggins,et al. Modulation and daily banding of Mg/Ca in Orbulina universa tests by symbiont photosynthesis and respiration: A complication for seawater thermometry? , 2004 .
[31] B. Flower,et al. Phasing of deglacial warming and Laurentide Ice Sheet meltwater in the Gulf of Mexico , 2004 .
[32] N. Rogers,et al. Determination of intratest variability of trace elements in foraminifera by laser ablation inductively coupled plasma‐mass spectrometry , 2003 .
[33] S. Eggins,et al. Mg/Ca variation in planktonic foraminifera tests: implications for reconstructing palaeo-seawater temperature and habitat migration , 2003 .
[34] F. Jorissen,et al. Single foraminiferal test chemistry records the marine environment , 2003 .
[35] W. Austin,et al. The potential of ion microprobe analysis in detecting geochemical variations across individual foraminifera tests , 2003 .
[36] D. Lea,et al. Climate impact of late quaternary equatorial pacific sea surface temperature variations , 2000, Science.
[37] D. Lea,et al. Controls on magnesium and strontium uptake in planktonic foraminifera determined by live culturing , 1999 .
[38] M. Kühl,et al. Microsensor studies of photosynthesis and respiration in the symbiotic foraminifer Orbulina universa , 1998 .
[39] Jelle Bijma,et al. Reevaluation of the oxygen isotopic composition of planktonic foraminifera: Experimental results and revised paleotemperature equations , 1998 .
[40] Jelle Bijma,et al. Effect of seawater carbonate concentration on foraminiferal carbon and oxygen isotopes , 1997, Nature.
[41] K. Kohfeld,et al. Neogloboquadrina pachyderma (sinistral coiling) as paleoceanographic tracers in polar oceans: Evidence from northeast water polynya plankton tows, sediment traps, and surface sediments , 1996 .
[42] K. Billups,et al. Reconstructing the stable isotope geochemistry and paleotemperatures of the equatorial Atlantic during the last 150,000 years: Results from individual foraminifera , 1996 .
[43] R. Schiebel,et al. Impacts of storms on Recent planktic foraminiferal test production and CaCO3 flux in the North Atlantic at 47 °N, 20 °W (JGOFS) , 1995 .
[44] N. Slowey,et al. Glacial‐interglacial differences in circulation and carbon cycling within the upper western North Atlantic , 1995 .
[45] D. Lea,et al. Assessing the reliability of paleochemical tracers: barium uptake in the shells of planktonic foraminifera , 1994 .
[46] D. Lea,et al. Experimental determination of barium uptake in shells of the planktonic foraminifera Orbulina universa at 22°C , 1992 .
[47] DOUGLAS F. Williams,et al. Evidence for seasonal low‐salinity surface waters in the Gulf of Mexico over the last 16,000 years , 1990 .
[48] Peter N. Schweitzer,et al. Globorotalia truncatulinoides' Growth and chemistry as probes of the past thermocline: 1. Shell size , 1990 .
[49] W. G. Deuser,et al. Seasonally abundant planktonic Foraminifera of the Sargasso Sea: succession, deep water fluxes, isotopic compositions, and paleoceanographic implications , 1989 .
[50] DOUGLAS F. Williams,et al. Extracting environmental information from planktonic foraminiferal δ13C data , 1988, Nature.
[51] H. Spero. Ultrastructural examination of chamber morphogenesis and biomineralization in the planktonic foraminiferOrbulina universa , 1988 .
[52] D. Caron,et al. Growth of the spinose planktonic foraminifer Orbulina universa in laboratory culture and the effect of temperature on life processes , 1987, Journal of the Marine Biological Association of the United Kingdom.
[53] Steven L. Parker,et al. Photosynthesis in the symbiotic planktonic foraminifer Orbulina universa, and its potential contribution to oceanic primary productivity , 1985 .
[54] P. Schiffelbein,et al. Direct assessment of stable isotope variability in planktonic foraminifera populations , 1984 .
[55] C. Kendall,et al. Comparison of stable isotope reference samples , 1983, Nature.
[56] P. Wiebe,et al. Vertical distribution and isotopic fractionation of living planktonic foraminifera from the Panama Basin , 1982, Nature.
[57] P. Blanc,et al. Oxygen-18 Enrichment of Planktonic Foraminifera Due to Gametogenic Calcification Below the Euphotic Zone , 1981, Science.
[58] W. Berger,et al. Oxygen and carbon isotopes of individual shells of planktonic foraminifera from Ontong-Java plateau, equatorial pacific , 1981 .
[59] J. Erez,et al. Comparison of isotopic composition of planktonic foraminifera in plankton tows, sediment traps and sediments , 1981 .
[60] C. Hemleben,et al. Seasonal changes in species composition, numbers, mass, size, and isotopic composition of planktonic foraminifera settling into the deep sargasso sea☆ , 1981 .
[61] P. Wiebe,et al. Vertical Distribution and Isotopic Composition of Living Planktonic Foraminifera in the Western North Atlantic , 1980, Science.
[62] W. N. Orr. Secondary Calcification in the Foraminiferal Genus Globorotalia , 1967, Science.
[63] C. Emiliani,et al. Pleistocene Temperatures , 1955, The Journal of Geology.
[64] Samuel Epstein,et al. REVISED CARBONATE-WATER ISOTOPIC TEMPERATURE SCALE , 1953 .
[65] S. Eggins,et al. Timing and mechanism for intratest Mg/Ca variability in a living planktic foraminifer , 2015 .
[66] A. Mix,et al. Pleistocene megafloods in the northeast Pacific , 2009 .
[67] J. Valley. Oxygen Isotopes in Zircon 345 element content , 2004 .
[68] P. Martin,et al. Calcium uptake and calcification rate in the planktonic foraminifer Orbulina universa , 1995 .
[69] A. Bé. Gametogenic calcification in a spinose planktonic foraminifer, Globigerinoides sacculifer (Brady) , 1980 .
[70] A. Gregoriades,et al. Assessing the reliability of socio‐technical systems , 2002 .