Nature Search

Abrupt changes in early Holocene tropical sea surface temperature derived from coral records

J. Warren Beck
Jacques Récy
Guy Cabioch
Research20 Feb 1997
Nature

Volume: 385, P: 705-707
Measurement of Histone Methylation Dynamics by One-Carbon Metabolic Isotope Labeling and High-energy Collisional Dissociation Methylation Signature Ion Detection

Hui Tang
Bing Tian
Kangling Zhang
ResearchOpen Access17 Aug 2016
Scientific Reports

Volume: 6, P: 1-7
Use of Opioids in Asphyxiated Term Neonates: Effects on Neuroimaging and Clinical Outcome

Danilyn M Angeles
Nathaniel Wycliffe
Stephen Ashwal
Research01 Jun 2005
Pediatric Research

Volume: 57, P: 873-878
Eemian interglacial reconstructed from a Greenland folded ice core

Reconstruction of the Eemian interglacial from the new NEEM ice core shows that in spite of a climate warmer by eight degrees Celsius in Northern Greenland than that of the past millennium, the ice here was only a few hundred metres lower than its present level.

D. Dahl-Jensen
M. R. Albert
J. Zheng
Research23 Jan 2013
Nature

Volume: 493, P: 489-494
Role of Tet proteins in 5mC to 5hmC conversion, ES-cell self-renewal and inner cell mass specification

TET1 is an enzyme that catalyses the conversion of 5-methylcytosine of DNA to 5-hydroxymethylcytosine, raising the possibility that it is involved in mediating DNA demethylation. These authors show that Tet1 is involved in mouse embryonic stem cell maintenance and specification of the inner cell mass. It is required to maintain both the expression of Nanog in embryonic stem cells and the Nanog promoter in a hypomethylated state, supporting a role for Tet1 in regulating DNA methylation.

Shinsuke Ito
Ana C. D’Alessio
Yi Zhang
Research26 Aug 2010
Nature

Volume: 466, P: 1129-1133
Relationship Between Opioid Therapy, Tissue-Damaging Procedures, and Brain Metabolites as Measured by Proton MRS in Asphyxiated Term Neonates

Danilyn M Angeles
Stephen Ashwal
Barbara A Holshouser
Research01 May 2007
Pediatric Research

Volume: 61, P: 614-621
Onset of deglacial warming in West Antarctica driven by local orbital forcing

An annually resolved ice-core record from West Antarctica indicates that warming driven by local insolation resulting from sea-ice decline began in that region about 2,000 years before warming in East Antarctica, reconciling two alternative explanations for deglacial warming in the Southern Hemisphere.

T. J. Fudge
Eric J. Steig
Gifford J. Wong
Research14 Aug 2013
Nature

Volume: 500, P: 440-444

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Abrupt changes in early Holocene tropical sea surface temperature derived from coral records

Measurement of Histone Methylation Dynamics by One-Carbon Metabolic Isotope Labeling and High-energy Collisional Dissociation Methylation Signature Ion Detection

Use of Opioids in Asphyxiated Term Neonates: Effects on Neuroimaging and Clinical Outcome

Eemian interglacial reconstructed from a Greenland folded ice core

Role of Tet proteins in 5mC to 5hmC conversion, ES-cell self-renewal and inner cell mass specification

Relationship Between Opioid Therapy, Tissue-Damaging Procedures, and Brain Metabolites as Measured by Proton MRS in Asphyxiated Term Neonates

Onset of deglacial warming in West Antarctica driven by local orbital forcing

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