Non-equilibrium Isotopic Fractionation between Seawater and Planktonic Foraminiferal Tests
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Opal-based isotopic proxies of paleoenvironmental conditionsA rapid genome-scale response of the transcriptional oscillator to perturbation reveals a period-doubling path to phenotypic change.A high-performance, safer and semi-automated approach for the delta18O analysis of diatom silica and new methods for removing exchangeable oxygen.A genomewide oscillation in transcription gates DNA replication and cell cycleCell cycle Start is coupled to entry into the yeast metabolic cycle across diverse strains and growth ratesEnvironmental and biological controls on size-specific δ13 C and δ18 O in recent planktonic foraminiferaDisappearance of pink-pigmented Globigerinoides ruber at 120,000 yr BP in the Indian and Pacific OceansVital effect on stable-isotope composition seen in foraminifera and coral skeletons
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P2860
Non-equilibrium Isotopic Fractionation between Seawater and Planktonic Foraminiferal Tests
description
article publié dans la revue scientifique Nature
@fr
scientific article published in Nature
@en
wetenschappelijk artikel
@nl
наукова стаття, опублікована в Nature в березні 1973
@uk
name
Non-equilibrium Isotopic Fract ...... Planktonic Foraminiferal Tests
@en
Non-equilibrium Isotopic Fract ...... Planktonic Foraminiferal Tests
@nl
type
label
Non-equilibrium Isotopic Fract ...... Planktonic Foraminiferal Tests
@en
Non-equilibrium Isotopic Fract ...... Planktonic Foraminiferal Tests
@nl
prefLabel
Non-equilibrium Isotopic Fract ...... Planktonic Foraminiferal Tests
@en
Non-equilibrium Isotopic Fract ...... Planktonic Foraminiferal Tests
@nl
P2093
P356
P1433
P1476
Non-equilibrium Isotopic Fract ...... Planktonic Foraminiferal Tests
@en
P2093
H. A. BUCKLEY
J. D. H. WISEMAN
N. J. SHACKLETON
P2888
P304
P356
10.1038/242177A0
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P577
1973-03-01T00:00:00Z
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1037948140